Oregon Theodore R KjibngDski, Governor NOTICE OF ADOPTED AMENDMENT Department of Land Conservation and Development 635 Capitol Street, Suite 150 Salem, OR 97301-2540 (503) 373-0050 Fax (503) 378-5518 w w w . lcd.state.or .us Mis. 11/30/2009 TO: Subscribers to Notice of Adopted Plan or Land Use Regulation Amendments FROM: Plan Amendment Program Specialist SUBJECT: City of Grants Pass Plan Amendment DLCD File Number 007-09 The Department of Land Conservation and Development (DLCD) received the attached notice of adoption. Due to the size of amended material submitted, a complete copy has not been attached. A Copy of the adopted plan amendment is available for review at the DLCD office in Salem and the local government office. Appeal Procedures* DLCD ACKNOWLEDGMENT or DEADLINE TO APPEAL: Friday, December 11, 2009 This amendment was submitted to DLCD for review prior to adoption. . Pursuant to ORS 197.830(2)(b) only persons who participated in the local government proceedings leading to adoption of the amendment are eligible to appeal this decision to the Land Use Board of Appeals (LUBA). If you wish to appeal, you must file a notice of intent to appeal with the Land Use Board of Appeals (LUBA) no later than 21 days from the date the decision was mailed to you by the local government. If you have questions, check with the local government to determine the appeal deadline. Copies of the notice of intent to appeal must be served upon the local government and others who received written notice of the final decision from the local government. The notice of intent to appeal must be served and filed in the form and manner prescribed by LUBA, (OAR Chapter 661, Division 10). Please call LUBA at 503-373-1265, if you have questions about appeal procedures. *NOTE: THE APPEAL DEADLINE IS BASED UPON THE DATE THE DECISION WAS MAILED BY LOCAL GOVERNMENT. A DECISION MAY HAVE BEEN MAILED TO YOU ON A DIFFERENT DATE THAT IT WAS MAILED TO DLCD. AS A RESULT, YOUR APPEAL DEADLINE MAY BE EARLIER THAN THE ABOVE DATE SPECIFIED. Cc: Lora Glover, City of Grants Pass Gloria Gardiner, DLCD Urban Planning Specialist Chris Shirley, FEMA Specialist John Renz, DLCD Regional Representative N 2 _J Iii ¡ am i r • electronic G ma fleti DLCD DEPTOF Notice of Adoption m im THIS FORM MUST BE MAILED TO DLCD LAND CON3E WITHIN 5 WORKING DAYS AFTER THE FINAL DECISION * AND DEVELOP WEN I PER ORS 197.610, OAR CHAPTER 660 - DIVISION 18 IwlJl ÜEUst 0p|S Jurisdiction: d /TV OP £r /WTS P 1 / ^ Local file number: £fi - QO%0000<4 Date of Adoption: Date Mailed: { [ g ^ c f ' HOSDOÖdj Was a Notice of Proposed Amendment (Form 1) mailed to DLCD? Select oneDate: 0 Comprehensive Plan Text Amendment O Comprehensive Plan Map Amendment J Land Use Regulation Amendment R^Zoning Map Amendment ^LODb KW^Hf^ • New Land Use Regulation • Other: Summarize the adopted amendment. Do not use technical terms. Do not write "See Attached". fiWPTlÖH ÖF (UM15UT CftEC-TiVe Fux>^ /WSOfcttM^ ^TUhM^Fi^ f=LCDt> /MSM.-RAWC5 WlH C f W ^ M T E b 3 , • Does the Adoption differ from proposal? Please select one "¿vM" Plan Map Changed from: ^ /A- to: "k/ f4- Zone Map Changed from: to: Location: Acres Involved: ^h. Specify Density: Previous: New: fy j f t - Applicable statewide planning goals: X 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 • • • • • • 0 • • • • • • • D • • • • Was an Exception Adopted? • YES ^ N O Did DLCD receive a Notice of Proposed Amendment... 45-days prior to first evidentiary hearing? H^Yes • No If no, do the statewide planning goals apply? • Yes • No If no, did Emergency Circumstances require immediate adoption? • Yes • No D L C D f i l e N o . 007-09 (17717) [15859] (This file also refers to D L C D Fi le Grants Pass 004-09) Please list ai( affected State or Federal Agencies, Local Governments or Special Districts: ÖDuusny b L C Ä Local Contact: L O W &)LD\J@/t Phone: {&{)cflt{- (¿ZS^Extension: Address: ( o f M U * Fax Number:5V MlU- JZtfS City: a m W i M ^ O R Zip: E-mail Address:/^ ADOPTION SUBMITTAL REQUIREMENTS This form must be mailed to DLCD within 5 working days after the final decision perORS 197.610, OAR Chapter 660 - Division 18. 1. Send this Form and TWO Complete Copies (documents and maps) of the Adopted Amendment to: ATTENTION: PLAN AMENDMENT SPECIALIST DEPARTMENT OF LAND CONSERVATION AND DEVELOPMENT 635 CAPITOL STREET NE, SUITE 150 SALEM, OREGON 97301-2540 2. Electronic Submittals: At least one hard copy must be sent by mail or in person, but you may also submit an electronic copy, by either email or FTP. You may connect to this address to FTP proposals and adoptions: webserverJcd.state.or.us. To obtain our Username and password for FTP, call Mara Ulloa at 503-373-0050 extension 238, or by emailing mara.ulloa@state.or,us. 3. Please Note: Adopted materials must be sent to DLCD not later than FIVE (5) working days following the date of the final decision on the amendment. 4. Submittal of this Notice of Adoption must include the text of the amendment plus adopted findings and supplementary information. 5. The deadline to appeal will not be extended if you submit this notice of adoption within five working days of the final decision. Appeals to LUBA may be filed within TWENTY-ONE (21) days of the date, the Notice of Adoption is sent to DLCD. 6. In addition to sending the Notice of Adoption to DLCD, you must notify persons who participated in the local hearing and requested notice of the final decision. 7. Need More Copies? You can now access these forms online at http://www.lcd.state.or.us/. Please print on 8 - l / 2 \ l l green paper only. You may also call the DLCD Office at (503) 373-0050; or Fax your request to: (503) 378-5518; or Email your request to mara.ulloa@state.or.us - ATTENTION: PLAN AMENDMENT SPECIALIST. http://www.lcd.state.or.us/LCD/forms.shtml Updated November 27,2006 November 20, 2009 City of Grants Pass Department of Land Conservation & Development Attn: Plan Amendment Specialist 635 Capitol Street NE, Suite 150 Salem OR 97301-2540 Re: Notice of Adoption ~ Flood Map Amendments File No.: 09-40500004 & 09-40500006 Dear Sir/Madam, Please find enclosed the Notice of Adoption for the above-referenced file. If you have any question, please do not hesitate to contact me. Lor a Glover Associate Planner Ext. #6427 lglover@grantspassoregon.gov Enclosure: Notice of Adoption, Ordinance No. 5498 w/record pc: Stephen Lucker, DLCD w/Ordinance No. 5498 Dennis Hunsinger, Acting Regional Administrator, FEMA Region X w/Ordinance No. 5498 C/F, tax lot file 101 Northwest "A" Streel, Grants Pass, Oregon 97526 * (541)474-6355 * FAX (541) 476-9218 * www.grantspassoregon.gov Sincerely, ORDINANCE NO. 5498 AN ORDINANCE OF THE COUNCIL OF THE CITY OF GRANTS PASS AMENDING: (1) THE SPECIAL PURPOSE DISTRICT MAP FOR THE FLOOD HAZARD DISTRICT BY ADOPTING THE CURRENT FLOOD INSURANCE STUDY (FIS) AND FLOOD INSURANCE RATE MAPS (FIRM) FOR JOSEPHINE COUNTY AND INCORPORATED AREAS EFFECTIVE DECEMBER 3, 2009; (2) SECTION 13.200 (FLOOD HAZARD DISTRICT) OF THE CITY OF GRANTS PASS DEVELOPMENT CODE; AND (3) ELEMENT 5, SECTION 5.30 ~ FLOOD HAZARD, OF THE GRANTS PASS AND URBANIZING AREA COMPREHENSIVE COMMUNITY DEVELOPMENT PLAN; AND DECLARING AN EMERGENCY. WHEREAS: 1. The Grants Pass and Urbanizing Area Comprehensive Community Development Plan was adopted December 15, 1982; and 2. The goal of the amendments is to maintain the City's eligibility to participate in National Flood Insurance Program (NFIP); and 3. The proposal is consistent with the goals and policies of the Comprehensive Plan; and 4. The applicable criteria from the Comprehensive Plan and the Development Code are satisfied, and approval of the proposal is recommended by the Urban Area Planning Commission to the City Council. NOW, THEREFORE, THE CITY OF GRANTS PASS HEREBY ORDAINS: Section 1: Adopt into the Comprehensive Plan the Flood Insurance Study (FIS) Volume 1 and 2, as set forth in Exhibit "A" attached hereto. Section 2: Adopt into the Comprehensive Plan the Flood Insurance Rate Maps (FIRM) for Josephine County, Oregon and Incorporated areas effective December 3, 2009 (amending the Special Purpose District Map for the Flood Hazard District), as set forth in Exhibit "A" attached hereto. Section 3: Revise Section 13.200 (Flood Hazard District) of the City of Grants Pass Development Code as set forth in Exhibit "A" attached hereto. Section 4: Revise Element 5, Section 5.30 ~ Flood Hazard of the Comprehensive plan, to reference the new FIS and FIRM effective December 3, 2009, as set forth in Exhibit "A" attached hereto. Section 5: Repeal Sections 9.50-9.56 (Flood Hazard Regulations), Title 9: Land Development and Public Improvements of the City of Grants Pass Municipal Code, and re-title Chapter 4 of Title 9 as "Measure 7" as set forth in Exhibit "B" attached hereto. Section 6: An emergency is hereby declared to exist and in the interest of the public peace, health and safety of the City of Grants Pass and the inhabitants thereof, this Ordinance has been introduced and read twice and placed upon its final passage at a single meeting of the Council and shall take effect immediately upon passage. ADOPTED by the Council of the City of Grants Pass, Oregon, in regular session this 4th day of November, 2009. SUBMITTED to and Ayxa/WirT? by the Mayor of the City of Grants Pass, Oregon, this ^.v^dav of November, 2009. ATTEST: Date submitted to Mayor: ^ - 9 Finance Director Approved as to Form, Mark Bartholomew, Interim City Attorney Exhibit "A" to Adopting Ordinance Exhibit A consists of the following documents which have not been reproduced in their entirety to conserve resources: 1. Flood Insurance Study (FIS) for Josephine County, Oregon and Incorporated areas, dated December 3,2009 (the full report is available in the Planning file). 2. Flood Insurance Rate Maps (FIRM) dated December 3, 2009 (the full set of maps is available in the Community Development office). 3. Revised Section 13.200 ~ Flood Hazard District of the Development Code (available in the Planning file). 4. Revised Element 5, Section 5.30 - Flood Hazard of the Comprehensive Plan (available in the Planning file). Exhibit "B" to Adopting Ordinance Exhibit B consists of the following document: 1. Revised Title 9 of the Municipal Code. E X H I B I T H n o R » i » * « e FLOOD INSURANCE STUDY JOSEPHINE COUNTY, OREGON AND INCORPORATED AREAS VOLUME 1 OF 2 COMMUNITY COMMUNITY NAME NUMBER CAVE JUNCTION, CITY OF . 4 1 0 1 0 7 GRANTS PASS, CITY OF 410108 JOSEPHINE COUNTY UNINCORPORATED AREAS 4 ] 5590 Effective: December 3, 20Q9 Flood Insurance Study Number 41033CV001A EXHIBIT JL- rtTTrtòU^WT I • 'f NOTICE TO FLOOD INSURANCE STUDY USERS Communities participating in the National Flood Insurance Program have established repositories of flood hazard data for floodplain management and flood insurance purposes. This Flood Insurance Study (FIS) report may not contain all data available within the Community Map Repository- Please contact the Community Map Repository for any additional data. Selected Flood Insurance Rate Map panels for the community contain information that was previously shown separately on the corresponding Flood Boundary and Floodway Map panels (e.g, floodways, cross sections). In addition, former flood hazard zone designations have been changed as follows: Old Zone AI through A3 0 VI through V30 B C Part or all of this may be revised and republished at any time. In addition, part of this FIS may be revised by a Letter of Map Revision process, which does not involve republication or redistribution of the FIS. It is, therefore, the responsibility of the user to consult with community officials and to check the community repository' to obtain the most current FIS report components. This FIS report was revised on December 3,2009. User should refer to Section 10.0, Revision Descriptions, for further information. Section 10.0 is intended to present the most up-to-date information for specific portions of this FIS report. Therefore, users of this FIS report should be aware that the information presented in Section 10.0 supersedes information in Sections 1,0 through 9.0 of this FIS report. New Zone AE VE X (shaded) X(unshaded) TABLE OF CONTENTS'- VOLUME 1 1.0 INTRODUCTION LI Purpose of Study 1.2 Authority and Acknowledgements 1.3 Coordination 2.0 AREA STUDIED 2.1 Scope of Study 2.2 Community Description 2.3 Principal Flood Problems 2.4 Flood Protection Measures 3.0 ENGINEERING METHODS 3.1 Hydrologic Analyses 3.2 Hydraulic Analyses 3.3 Vertical Datum 4.0 FLOODPLAIN MANAGEMENT APPLICATIONS 4.1 Floodplain Boundaries 4.2" Floodways 5.0 INSURANCE APPLICATION 6.0 FLOOD INSURANCE RATE MAP 7.0 OTHER STUDIES 8.0 LOCATION OF DATA 9.0 BIBLIOGRAPHY AND REFERENCES 1Q.0 REVISION DESCRIPTION FIGURES Figure 1 - Floodway Schematic TABLES Table.l - Initial, Intermediate, and Final CCO Meetings Table 2 - Flooding Sources Studied by Detailed Methods Table 3 - Flooding Sources Studied by Approximate Methods Table 4 - Summary of Discharges Table 5 - Range of Manning's Roughness Values Table 6 - Floodway Data Table 7 - Flood Insurance Zones Within Each Community Table 8 - Community Map History TABLES (continued! Table 9 - Revised Study Descriptions- 53 Exhibit 1 ~ Flood Profiles Applegate River Deer Creek Gilbert Creek Illinois River East Fork Illinois River West Fork Illinois River Jumpoff Joe Creek Louse Creek Muiphy Creek Rogue River Rogue River Right Overbank Slate Creek Waters Creek • TABLE OF CONTENTS - VOLUME 2 EXHIBITS Panels 01P-18P Panels 19P-23P Panels 24P-29P Panels 30P-35P Panels 36P-47P Panels 48P-59P Panels 60P-66P Panels 67P-80P Panels 81P-86P Panels 87P-100P Panel 10 IP Panels 102P.-108P Panels 109P-11 IP PUBLISHED SEPARATELY Flood Insurance Rate Map Index Flood Insurance Rate Map FLOOD INSURANCE STUDY ; JOSEPHINE COUNTY, OREGON AND INCORPORATED AREAS 1.0 INTRODUCTION 1.1 Purpose of Study This Flood Insurance Study revises and updates information on the existence and severity of flood hazards in the geographic area of Josephine County, including the Cities of Cave Junction and Grants Pass; and the unincorporated areas of Josephine County (referred to collectively herein as Josephine County), and aids in the administration of the National Flood Insurance Act of 1968 and the Flood Disaster Protection Act of 1973. This study has developed flood-risk data for various areas of the community that will be used to establish actuarial flood insurance rates and to assist the community in its efforts to promote sound floodp lain management. Minimum floodplain management requirements for participation in the National Flood Insurance Program (NFIP) are set forth in the Code of Federal Regulations at 44 CFR, 60.3. In some states or communities, floodplain management criteria or regulations may exist that are more restrictive or comprehensive than the minimum Federal requirements. In such cases, the more restrictive criteria take precedence and the State (or other jurisdictional agency) will be able to explain them. 1.2 Authority and Acknowledgments The sources of/authority for this Flood Insurance Study are the National Flood Insurance Act of 1968 and the Flood Disaster Protection Act of 1973. The hydrologic and hydraulic analyses for the studies in Grants Pass and unincorporated Josephine County were performed by the- U.S. Geological Survey (USGS) for the Federal Emergency Management Agency (FEMA) under Interagency Agreement No. IAA-H-14-78, Project Order No, 8. The analysis for the "City of Cave Junction was performed under Amendment 1-2 of the same contract. Analyses for the City of Cave Junction and unincorporated Josephine County were completed in July 1980. The original analysis for the City of Grants Pass was completed in July 1979. The restudy of the reach of the Rogue River flowing through Grants Pass was performed by OTAK, Incorporated. This additional work was completed in December .1989 for FEMA under Contract No. EMW-89-C-2847. The countywide.update was performed by WEST Consultants,. Inc. for FEMA under ContractNo. EMS-20010-0>0068.. Updated aeriál photography dated 2005 was used in the analysis. Work on the countywide update was completed in October 2008. 1.3 Coordination v The dates of the initial, intermediate, ánd final CCO meetings held for the previous FIS reports for "Josephine County and the incorporated communities within its boundaries are shown in Table 1, "Initial, Intermedíate, and Final CCO Meetings"; They were attended by •representatives of FEMA, the U.S. Geological Survey, the communities, and the study contractor. 1 Table 1. Initial, Intermediate, and Final CCO Meetings Community Initial CCO Date ftS0!?^ Final CCO Date — CCO Date(s) — ~— Cave Junction, City of January 12, 1978 May 12, 1980 June 3, 1981 Grants Pass, City o f January 1978 S e P t e m b e r l 9> 1 9 9 0 Josephine County, ; ^ m Q ^ ^ unincorporated areas Streams requiring detailed study were identified at a meeting held on January 12,1978. In attendance were representatives of the U.S. Geological Survey, FEMA, Josephine County, and the communities of Cave Junction and Grants Pass. The U.S. Army Corps of Engineers (COE) provided hydrologic data for the original Rogue River study, reflecting anticipated flood-control regulation from Lost Creek Dam, located 55.4 miles upstream from the city. Results of the hydrologic analyses were coordinated with the COE. Ending water-surface elevations at Savage Rapids Dam on the Rogue River were consistent with data furnished by the U.S. Geological Survey for the Jackson County Flood Insurance Study (Reference 1). On May 12, 1980, an intermediate meeting reviewing preliminary work done by the study contractor was attended by representatives of the study contractor, FEMA, the City of Cave Junction, and Josephine County. On May 27,1980, the results of the original study for the City of Grants Pass were reviewed at the final community coordination meeting attended by representatives of FEMA, the city, and the study contractor. No problems were raised at tlie meeting. A final coordination meeting for the City of Cave Junction and Josephine County was held on June. 3, 1981. The meeting was attended by representatives of the FEMA, the study contractor, the City of Cave Junction, and Josephine County. All problems raised at tlie meeting were resolved. Several flooding sourees within Grants Pass, including portions of the Rogue and Applegate Rivers,, and portions of Louse and Waters Creeks were selected for restudy at a meeting attended by representatives of FEMA,. Josephine County, the City of Grants Pass, and the study contractor on May 25,1988. Results of the hydrologic analyses performed by OTAK, Incorporated were coordinated with the COE, USGS, Soil Conservation Service, Oregon Department of Land Conservation and Development, and Josephine County. On September 19, 1990, the results of the restudy were reviewed at the final community coordination meeting attended by representatives of FEMA, the city, and the study contractor. Countvwide Update An initial community coordination meeting for Josephine County was held on March 6, 2006. This meeting was attended by representatives of the Cities of Grants Pass and Cave Junction, Josephine County, FEMA, and WEST Consultants, Inc. The results of the study were reviewed at the final Consultation Coordination Officer [CCO] meeting held on March 5, 2009, and attended by representatives of the Cities of Cave Junction and Grants Pass, Josephine County, The Oregon Department of Land Conservation and Development and FEMA. All problems raised at that meeting have been addressed in this study. 2 2.0 . AREA; STUDIED 2.1 Scope of Study This Flood Insurance Study covcrs the geographic area of Josephine County, Oregon, including the incorporated communities listed in Section l . l . The flooding sources studied by detailed methods in unincorporated Josephine County and the City of Cave Junction were selected with priority given to all known flood hazards and areas of projected development or proposed construction through 1985. Projected development or proposed construction were considered through 1995 within the City of Grants Pass. The limits of detailed studies in Josephine County were determined by FEMA with community and study contractor consultation at meetings in January 1978 and May 1988. Table 2 lists the flooding sources studied in detail and the included segments. River mileages used in this discussion are based on data published by the Hydrology Committee of the Columbia Basin Inter-Agency Committee (Reference 2). Table 2. Flooding Sources Studied by Detailed Methods Limits of Detailed Study From its confluence with the Rogue River to approximately 4,000 feet upstream of Wildcat Gulch near Murphy. From a point approximately one mile southwes t of Selma (RM 3.5) to Crooks Creek, From SW Rogue River Avenue to approximately 875 feet upstream from NW North Hill Drive. From the stream gaging station north ofKerby (near RM 50.0) to the confluence of the East and West Forks of the Illinois River. From its confluence with the Illinois River to approximately 500 feet downstream from Sucker Greek near Cave Junction and from Little Elder Creek (RM 65.6) to Page Creek south of Takilma. From its confluence with the Illinois River to the Redwood Highway bridge and from a point 870 feet downstream from . Hugo Road at.O'Brien (RM 7.8) to a point approximately 2.4 miles further upstream. From its confluence with the Rogue River to Monument Drive . near Merlin. From its confluence with Jumpoff Joe Creek to Granite Hill Road. From its confluence with the Applegate River to approximately 7,000 feet upstream from its mouth. Flooding Source 1. Applegate River 2. Deer Creek 3. Gilbert Creek 4. Illinois River 5. East Fork Illinois River 6. West Fork Illinois River 7. Jumpoff Joe Creek 8. Louse Creek 9. Murphy.Creek Table 2. Flooding Sources Studied by Detailed Methods (continued) From Maple Creek near Galice (RM 75.2) to the Josephine- Jackson County limits at Savage Rapids Dam.. From its confluence with the main stem of the Rogue River to its divergence from the main stem of the .Rogue River approximately 1,300 feet upstream from Lincoln Avenue. From its confluence with the Applegate River to approximately the intersection of Round Prairie Road and Redwood Highway. From its confluence with Slate Creek to approximately 6,200 feet upstream from its mouth. Flows in Skunk Creek and Blue Gulch are well contained in rectified channels or underground conduits and were not included in the original study. The consultation meetings in January 1978 and May 1988 further identified flooding sources for which the extent of floodway analysis would be limited or excluded. The Rogue River floodway was determined only from Pass Creekdownstream of Grants Pass to the Josephine- Jackson County boundary. The Louse Creek floodway analysis was terminated at a point 2,100 feet downstream from the Interstate Highway 5 bridge. The detailed analysis of Murphy Creek did not include a floodway analysis. Floodway delineations were considered unnecessary in the areas already having multiple Federal, State, and eounty permit requirements for new construction (such as the area downstream from Pass Creek on the Rogue River). Approximate analyses were used to study flooding sources in areas having a low development potential or minimal flood hazards. The scopes and methods of analysis were proposed to, and agreed upon by FEMA, Josephine County, and the Cities of Cave Junction and Grants Pass. These analyses were adopted from previously effective flood hazard boundary, maps (Reference 3), Table 3 lists the flooding sources, grouped by watershed, which were studied by approximate methods. Table 3. Flooding Sources Studied by Approximate Methods 1. Rogue River, Grave Creek, Wolf Creek,.Coyote Creek, Limpy Creek, and Dutcher Creek. 2. Jumpoff Joe Creek, Quartz Creek, Bummer Creek, Bannister Creek, Schoolhouse Creek, and Haints Creek. 3. Slate Creek, Cheney Creek, Murphy Creek, Williams Creek, Banning Creek, and the East and West Forks of Williams Creek. 4. Peer Creek, Clear Creek, Draper Creek, Davis Creek, McMullin Creek, and Crooks Creek. 5. Illinois River, West Fork Illinois River, Mendenhall Creek, Rough and Ready Creek, Elk Creek, East Fork Illinois River, Kelly Greek, Tycer Creek, Sucker Creek, Democrat Gulch, Mulvaney Gulch, Althouse Creek, and Altbouse Slough. 10. Rogue River 11. Rogue River Right Overbank 12. Slate Creek 13. Waters Creek 4 2.2 Community Description Josephine County is located in southwestern Oregon, sharing its southern boundary with the State .of California. Established in 1856, the county has an area of 1,625 square miles. Residential land development is present throughout the county due to the moderate climate and recreational features of the region. The estimated population of the county was 52,100 in 1978 (Reference 4). The population as of the 2000 census was 75,726 (Reference 5). The climate of Josephine County is typical of other areas of Oregon west of the Cascade Range. The average July temperature is 71.2°F; hi January, the average temperature is 39.9°F. The Klamath Mountain Range to the west provides a minor orographic barrier to winter storms moving inland from the Pacific Ocean. Heavy winter rainfall usually occurs in the interior valleys, and deep snow accumulates at the higher elevations of the Cascade, Siskiyou, and Klamath Mountain Ranges. The average annual rainfall varies from approximately 30 inches in Grants Pass to over 60 inches in the Siskiyou Mountains. The Cascade Range, far to the east, accumulates almost 80 inches of precipitation (Reference 6). Josephine County is drained almost entirely by the Rogue River and its two principal tributaries, the Applegate and Illinois Rivers. Steep, mountainous terrain lends , to rapid runoff when mild temperatures and heavy rainfall melt snow at theJiigher elevations. The Rogue River originates in the Cascade Range where the highest elevations exceed 8,000 feet. The drainage area of the river as it enters Josephine County at Savage Rapids Dam is 2,430 square miles. As the river flows westerly through the county, flood flows are fairly well contained by both banks until reaching the City of Grants Pass, 5.5 miles downstream of the dam. From Grants Pass to Finely Bend (9.9 miles west of the city), vast areas of low- lying terrain are subject to severe flooding. From Finley Bend, the river meanders north of Jumpoff Joe Creek (8.5 miles downstream). In these reaches, flood flows are subject to natural bank constrictions which result in sizable ponding of water. Beyond Jumpoff Joe Creek, the Rogue River flows northwesterly toward the resort community of Galice. In this reach, flood flows are totally contained by steep canyon walls, especially at Hellgate Canyon and at an unnamed canyon-ending at Taylor Creek. In these canyons, flood flows become constricted.to a few hundred feet in width. Beyond Galice, the river continues its westward passage through the Klamath Mountain Range until it eventually reaches the Pacific Ocean. The Applegate River originates in the Siskiyou Mountains which form all but the northern boundary of the basin. The summit of the range reaches elevations of over 7,000 feet in some areas. The river enters Josephine-County from the southeast at a point 7.5 miles upstream from the small community of Murphy, The drainage area at a discontinued gaging station at the bridge in Murphy is 663 square miles. Flood flows in a sharply meandering channel inundate wide portions of the floodplain that lie upstream from natural constrictions. Five miles downstream from Murphy, the river passes through a short, narrow canyon. After leaving the canyon, o verbank flooding is moderate until the river becomes affected by backwater from the Redwood Highway (U.S. Highway 199) bridge near Wilderville. Here, extensive flooding occurs. Approximatély 0.6 miles downstream from the bridge, the Applegate River becomes affected by backwater from the Rogue River. The inundated Applegate River flood plain width exceeds 4,000 feet at its mouth (6.4 miles west of the City of Grants Pass). The eastern boundary of the Illinois River basin is also formed by the Siskiyou Mountains. The southern and western boundaries are formed by the Chetcò Divide of the Klamath Mountain Range. Summit elevations vary from 4,000 to 6,000 feet. The headwaters of Illinois River consist of two principal tributaries, the East and West Forks Illinois Ri ver. The 5 East Fork Illinois River enters Josephine County from the south at a point 3.9 miles upstream from the community'of Takilma. The drainage area at a gaging station located 0.3 miles north of the county limits is 42.3 square miles. General flooding occurs in most areas near Takilma except in a gorge east of the community. Farther north, extensive flooding occurs in the wide, flat floodplain downstream from the Redwood Highway Bridge near Cave Junction. The East Fork Illinois RiVer joins the West Fork Illinois River to form the main steiri of the Illinois River at the City of Cave Junction. The West Fork Illinois River also flows northerly into Josephine County at a point 7.1 miles upstream from the community of O'Brien. The drainage area of a gaging station located approximately 4 miles north of the county limits is 42.4 square miles. The most significant flooding in O'Brien occurs at the Redwood Highway Bridge, Overflow inundates portions of the community before re-entering the channel downstream from the bridge. Farther north, near Cave Junction, flooding is much more severe. Wide areas are inundated, especially near the drive-in theater located 2.5 miles south of the community. Below the confluence of its East and West Forks, the Illinois River flows northerly through fertile agricultural areas. Wide floodplains between Cave Junction and Kerby (2 miles to the north) become completely flooded. The flooding north of Kerby is equally severe, caused in part by a sharp bend in the river as it enters a narrow canyon. Beyond the mouth of the canyon (2.5 miles north of Kerby), the Illinois River continues westward through the Klamath Mountain Range until it meets the Rogue River at the summer resort community of Agness in Curry County, 50.2 miles downstream. Deer Çreek, a tributary of the Illinois River, is located entirely within Josephine County. The creek orijgihates in the Siskiyou Mountain foothills, south of Grants Pass, and flows westerly toward the community of Selma. The drainage area of the stream at a point 3.5 miles upstream from its mouth is 101 square miles. Flood plains in the Sehna area are low and flat. Extensive flooding occurs in this agricultural area. City of Cave Junction The City of Cave Junction is in the southwestern portion of Josephine County. The city, surrounded by unincorporated areas of Josephine County, is approximately 25 miles southwest of Grants Pass, Oregon, and 12 miles north of the Oregon-California State boundary. Cave Junction, incorporated, in 1948, is the second largest city in thé county, with an estimated 1978 population of over 800. Its population as of the 2000 census was 1,363 (Reference 5), Residential development is present throughout the area due to the moderate climate and recreational features of the region. The climate of Cave Junction is typieal of other areas of Oregon west of the Cascade Range. The average July temperature is 71.2°F; in January, 39.3°F. The Klamath Range to the west provides a minor orographic barrier tb winter storms moving inland from the Pacific Ocean. .Heavy winter rainfall usually occurs in the interior valleys, and deep snow accumulates at higher elevations of the Cascade, Siskiyou, and Klamath Mountain Ranges. (Reference 6). Citv.of Grants Pass The City of Grants Pass is situated along the Rogue River in eastern Josephine County approximately 25 miles northwest of Medford, Oregon, and 30 miles north of the Oregon- California State boundary. incorporated in 1887, Grants Pass is the county seat and had a population of23,023 as of the 2000 census. The city extends across a 3-mile-wide valley and is bounded by densely wooded hills to the north and south. Fertile lowland areas support a sizable agricultural industry; timber and related byproducts are also important to the economy. Seasonal recreation fishing and character excursion trips on the Rogue River make Grants Pass a very popular tourist center. The Rogue River floodplain within the city has areas of dense residential and commercial development. Aerial photographs show that some small tracts of land are undeveloped, but local land use measures may dictate the type and extent of future development. Gilbert Creek has a very high density of residential development. The drainage area of the Rogue River at the gage in Grants Pass is 2,459 square miles. The river originates in the Cascade Range, where heavily forested slopes reach elevations exceeding 8,000 feet. These steep slopes usually accumulate heavy winter, snowfall, and storm runoff is rapid when mild temperatures and sustained rainfall occur during the passage of a. Pacific storm front. An exception to this general runoff characteristic occurs above an elevation of 5,000 feet in the vicinity of Crater Lake. Highly permeable pumice soils and lava formations allow much of the rainfall and snowmelt to infdtrate the ground, thus reducing surface runoff (Reference 7). The drainage area of Gilbert Creek is 5.68 square miles at its mouth. The creek originates in the foothills north of the city, where the highest elevation is approximately 3,100 feet. The channel gradient is very steep until reaching the city, and peak flows usually occur within hours after the passage of a storm front. Topography varies from the steep, forested slopes of Blue Gulch in the northwestern part of the city to the more gently sloping floodplain of the rest of Grants Pass. Elevations range from approximately 900 feet along the Rogue River to over 1,500 feet in the northwestern portion of the city (Reference 8). The average annual temperature is 54°F, with historic extremes ranging from 114°F in 1928 to -l°F in 1972 (Reference 9). Average annual rainfall varies from approximately 30 inches in the vicinity of Grants Pass to almost 80 inches in the extreme northeastern corner of the basin near Crater Lake (Reference 6). 2.3 Principal Flood Problems Abnormally heavy or prolonged rainfall, sometimes combined with snowmelt and frozen or nearly saturated ground, may cause flooding in Josephine County. AU streams in Josephine County usually respond to the same storm event, but the quantitative response can vary considerably. For example,1 most steams reached record stages during the devastating floods of December .1964; peak stages oh the Applegate River, although high in 1964, were exceeded in January 1974. 7 A comparison of historical floods at gaging stations must consider the possibility of changes that might occur in the stream channels between storm events. The scouring of a stream channel' could result in the greater flood having a lower recorded elevation. Flood flows tend to attenuate as they move downstream due torthe lessening of the channel gradient and to the storage of water ¡n the flood plains. Gaging-station records collected in the upper part of a basin are, therefore, seldom representative of the runoff characteristics in the lower basin. The largest flood in recent times occurred on the Rogue River on December 23, 1964. A peak flow of 152,000 cubic feet per second (cfs) inundated large residential areas in and around the City of Grants Pass. A stonn hydrograph at the Grants Pass gaging station showed the maximum stage was reached within 2 days after the initial raise in stage, and overbank flows remained for almost 4 days after the peak occurred. Antecedent climatological conditions were: 90 inches of snow had accumulated at Crater Lake by December 21, the freezing level rose to ì 1,000 feet on December 22, and rainfall totaled 8 to 10 inches at several reporting stations on December 21 and 22, The Crater Lake snow depth decreased to 68 inches by December 23 with a loss of 4 to 5 inches in water content (Reference 10). Downstream from the city to approximately Finley Bend, thousands of acres of productive farmland were under as much as 10 feet of water. Severe erosion and siltation occurred, and extensive irrigation systems were déstroyed. It is estimated that 360 residences, 19 commercial establishments, and 2 industries were damaged in this area (Reference 10). Downstream from Finley Bend, the river meanders in and out of deep canyons where development consists of ranches, summer homes, and recreational facilities. In December 1964, it is estimated 70 residences were flooded, and 18 were completely destroyed (Reference 10). Based on 38 years of records collected at a gaging station in Grants Pass, it is estimated that a flood of that magnitude would have occurred on the average of once every 5 0 years prior to ' the construction of Lost Creek Dam. It would now occur on the average of once every 120 years with anticipated flood regulation in effect (Reference 11). In the past 120 years, the December 1964 flood is believed to have been exceeded twice in Grants Pass. The U.S. Army Corps of Engineers estimates a flood in December 1861 had a discharge of 175,000 cfs; in February 1890, 160,000 cfs (Reference 10). They estimated that, due to upstream storage, discharges of that magnitude would now occur on the average of once every 180 years and 140 years, respectively (Reference 11). Gilbert Creek in Grants Pass is ungaged and quantitative historical high-flow data are unknown. Residents living adjacent to the channel have observed road overflow at various culverts throughout the city. There is severe channel encroachment in many areas due, in part, to vertical retaining walls built at the edge of the low-water channel. A house on L Street spans the channel and will obstruct high flows. On the Applegate River, the largest peak recorded at a gaging station located 1.8 miles southeast of the Town of Applegate in Jackson County occurred on January 15, 1974. A peak discharge of37,200 cfs exceeded the December 22,1964 peak of2,500 cfs. Extremely unstable channel conditions make an exact comparison of instantaneous peak flows impossible, and revisions of previously published data have been necessary. Flood damage to agricultural lands was extensive, but most of the damage occurred in areas 8 upstream from the Town of Murphy.Tt'is estimated that 2900 acres of productive farmland were inundated (Reference 12). Most of tlie residential damage occurred downstream from Murphy when the river scoured a sharp bend and inundated almost 200 acres. Based on 38 years of data collected at the Applegate gaging station, it is estimated that a flood of the magnitude, of the 1974 peak would reoccur on the average of once every 20 years. Now that the Applegate Reservoir is completed, the recurrence interval has been lengthened. The largest flood on Slate Creek occurred on December 22, 1964. A peak flow of4,650 cfs was recorded at a gaging station located 3.6 miles upstream from the community of Wilderville. Flood damage was not extensive because of the sparse population at that time. Based on 19 years of data collected at the gage, a flood of this magnitude would reoccur on the average of once every 8 years. The largest flood recorded in the Illinois River basin occurred on December 22, 1964. Two gaging stations located in the upper basin near Takilma and O'Brien indicated unit runoff values of approximately 380 cfs. per square mile, instantaneous peak flows were 15,700 cfs near Takilma and 16,100 cfs near O'Brien. A gaging station loeated in the lower part of the basin near Kerby had a peak flow of92,200 cfs and a unit runoff of approximately 240 cfs per square mile. The above unit runoff values are the'highest ever recorded in Josephine County. Because of the sparse population at the time, flood damage primarily involved highway bridges and agricultural land. Water depths of over 15 feet covered the Redwood Highway north of ICerby, Some homes were observed floating away from their foundations during the flood. Based on 15 years of records collected at the gaging station on Illinois River near Kerby, it is estimated a flood of this magnitude would occur on the average of onee every 150 years. In the upper basin where the flood runoff was more intense, the recurrence interval is estimated to be 500 years at Takilma and 300 years at O'Brien. The Takilma gaging ¡station has 39 years of record; O'Brien, 22 years. Extensive flood damage also occurred in the small tributaiy basins of Josephine County. Deer Creek, Jumpoff Joe Creek, and Louse Creek, although ungaged, had the highest flows ever observed during the December 1964 storm. Many drainage structures were damaged, resulting in the disruption of traffic. Fannland on the narrow terraces of the valleys suffered erosion and silt accumulations. Without streamflow data, it is not possible to derive statistical flow data for this flood. 2.4 Flood Protection Measures There are two functioning flood-control reservoirs in the basin. Lost Creek Dam, located 55.4 miles upstream from the gage in Grants Pass, will reduce, the magnitude of peak-flow events. It is estimated that a flood of the magnitude of the 1964 Rouge River flood would have occurred approximately once every .50 years prior to the construction of Lost Creek Dam. It should now occur on the average of approximately once every 120 years with existing flood regulation in effect. Due to upstream storage, discharges of the magnitude of the 1861 and 1890 Rogue River floods would now occur approximately once every 180 years and 140 years, respectively (Reference 13). Applegate Reservoir on Applegate River 9 is also located in Jackson County, 33.6 miles upstream from the community of Murphy. Construction of Elk Creek Dam began in 1986 and ceased in 1988. The completed portion of the dam was subsequently breached beginning in July 2008. No flood control is provided by the remaining structure. There are no extensive levee systems in the county. Some private interests have constructed dikes adjacent to their property; their capability of withstanding sizable flood events is unknown. ENGINEERING METHODS For the flooding sources studied by detailed methods in the community, standard hydrologic and hydraulic study methods were used to determine the flood-hazard data required for.this study. Flood events of a magnitude that are expected tó be equaled or exceeded once on the average during any 10-, 50-, 100-, or 500-year period (recurrence interval) have been selected as haying special significance for floodplain management and for. flood insurance rates. These events, commonly termed the 10-, 50-, 100-, and 500-year floods, have a 10-, 2-, 1-, and 0.2-percent chance, respectively, of being equaled or exceeded during any year. Although the recurrence interval represents thè long-term, average period between floods of a specific magnitude, rare floods could occur at short intervals or even within the same year. The risk of experiencing a rare flood increases when periods greater than 1 year are considered. For example, the risk of having a flood that equals or exceeds the 100-year flood (1-percent chance of annual exceedence) in any 50-year period is approximately 40 percent (4 in 10); for any 90-year period, the risk increases to approximately 60 percent (6 in 10). The analyses reported herein reflect flooding potentials based on conditions existing in the community at the time of completion of this study. Maps and flood elevations will be amended periodically to reflect future changes. 3.1 Hydrologic Analyses Hydrologic analyses were carried out to establish peak discharge-frequency relationships for each flooding source studied by detailed methods affecting the community. Federal Emergency Management Agency standards require Flood Insurance Studies in adjacent areas to use consistent hydrologic analyses. Accordingly, the hydrology of the Rogue River in Josephine County is identical to that used in the Jackson County Flood Insurance Study (Reference 1). The U.S. Aiiny Corps of Engineers has since revised that hydrology (Reference 11) as shown in the following table (discharges are in cfs). Discharges Flood Event Josephine County Revised Hydrology 10-percent-annuaI-chance 73,000 70,000 2-percent-annual-chance 128,000 120,000 1-percent-annual-chance 144,000 . 153,000 1 0.2-percent-annual-chance 260,000 280,000 Both sets of data are based on 38 years of stream flow records collected at Grants Pass gaging station (1939-1976). Thè discharges are adjus ted for expected probability and include anticipated flood-control regulation from Lost Creek Dam. The revised values are still within the 90 percent confidence limi ts of the original values. The regulating effect of the proposed Elk Creek Dam currently in development by the COE has been evaluated. 10 -a d tí S o > o . o o o o. o - o- o o o o O O C3 O oo Vo" oo' in M N Oí m Ol CS i-< i-< o O O O O O O c» r^ ^ in Oí en (N " m ri " On o O O o o o o^ rn es o" en ov Chi oo •8 o o o o o o o o o o o o fN| VD O «O -sr oo c4 vo" cm" o" c— t— vo vo vo o o 0 O o 2 o, r^ g S5 2 n vi » r- co es o\ co r- o o o o o o eo vo rn o^ TJ^ (N TT O' ÖC irT m" of « vi t t t t O o o o oo r- o V «n ^ oo vo o oí vo oo vo 3 o o o o o o m vn t-T vo" en Is*- vo vo M I O O O O O O o o o o o o vo^ c^ . vn vi? oo vo" f i -^i o Ov CN —1 '—' o a o a en 0\ r-en tt t-oC oo vo t í o ^ o o o »/i on oo vO oo vi of cN n iri o _ 2 K Vi Os r-- m Ol ^ V] v¡ O oo en í—1 I—i 7—I §1 n o t» bJ I o E § s ! H c : 4J I O £ a a bL,. u On On S S Ô g * ^ ab j3 a "O > «i 8 > D * £ g < < < < > m < 3 fi » « •g 3 4J H U Ö "o w 4) •y O io >> « « a CA CL, D TZI 0=1 S I -S' "9 S -S ON O O" On ' NO ^ m o o o «Í-" m ö o-o . o o o. o" NO in CS CS o o o o O oo o o o en TÍ" ON es t- W-) o o ^ s r—i Ov en es" O o O O o O O O O o o o o o cd 6Ï vo" 3 es m tí- m Tf N N iN rt H O O O (N VI VI <7n O^ ON co" co" no" oo" no" —i O 0\ CS es es es •—< •—< 1 o o o o m no On i—1 es o o o O I-»n «—i o i o o Vi r-1 oo t - O o C3 § o o o es o o o o o o oC I—1 I—1 I—1 I—1 I—1 I—1 p £ o o o o On o\ t - I—< I—1 vo o r vT -ïf en I—1 O o o en co c- CS On V» fri o o O O O o m t- >o en V} cm ^ ^ en en tn" es" cN >o 00 t> On oo". en es 5 rH Tt . 0\ Construction of Elk Creek Dam ceased in 1988. The completed portion of the dam was subsequently breached beginning in July 2008. No flood control is provided by the remaining structure. However, since the regulated discharges, including the anticipated benefit of the Elk Creek facility, were found by OTAK, Inc. to fall within-the 90 percent confidence interval of the unregulated discharges (i.e., without the Lost Creek and Elk Creek facilities), no changes were made to the discharges shown in the Summary of Discharges (Table 4). The U.S. Army Corps of Engineers also provided concordant flood control from both Lost Creek and Applegate Reservoirs. The Applegate River data were based on records collected over an 18-year period at a discontinued gaging station near Wilderville. The magnitude of the design floods on Slate Creek, and Illinois, East Fork Illinois, and West Fork Illinois Rivers was derived by using a log-Pearson Type III probability distribution (Reference 14) of the gaging station data referred to in Section 2.3. A generalized skew coefficient was determined from U.S. Water Resources Council Bulletin 17 (Reference 15). Discharges at sites within 5 to 25 percent of the gaging station drainage area were estimated using the following transfer formula: Q„ = Q g ( A u / A g ) n Where "Qg" and "Ag" are the discharge and drainage area at the gage, "Qu" and "A«" are the discharge and drainage area at the ungaged location, and the exponent "n" is an exponent derived from regional flood-frequency equations published in the U.S. Geological Survey Flood-Frequency Analysis for Western Oregon (Reference 16). Design floods at all other ungaged sites were determined using the flood-frequency equations included in the western Oregon analysis. The 0.2-percent-annual-chance flood equation for the Rogue River basin, not included in that report, is: Q o m & O Q ) = 1 0 5 A ° ' 9 l ( S T + l ) ' l - 2 6 i l M Where "A" is drainage area in square miles, "ST" is the area of lakes and ponds (in percent), and'T' is the rainfall intensity (2-year, 24-hour) in inches. The Gilbert Creek hydrology is based on 25 years of peak-flow data collected at a gaging station on Jones Creek, a small basin east of the the City of Grants Pass with headwaters adjoining Gilbert Creek, Jones Creek has .a drainage area of 7.41 square miles at a gaging station located at the culvert entrance on Interstate Highway 5. The discharges.used in this study were computed using a direct drainage area ratio of the two basins even though runoff in the urban areas of Gilbert Creek may differ from the rural runoff in the Jones Creek basin. If was beyond the scope of this study to conduct a detailed study of the effects of the storm- sewer inflows within the city. In order to determine the magnitude of the design floods on Jones Creek, the 25 years of peak data were used in a log-Pearson Type III probability distribution, with a generalized skew coefficient determined from the U.S. Water Resources Council Bulletin 17 (Reference 15). The USGS computer program J-407 (Reference 14) detected no low outliers, and the discharges were not adjusted for expected probability. 14 'The Gilbert Creek drainage area was determined on the basis of drainage maps provided by 'tJie City of Grants Pass (Reference 17) and by a USGS topographic map (Reference 8). The 1989 OTAK, Inc. analysis computed flows for Louse Creek and Waters Creek using the USGS equations in the publication entitled "Magnitude and Frequency of Floods of Western Oregon" (Reference 16). The 0.2-percent-annual-chance Q equation, describe above, was also used. Salt Creek enters Waters Creek approximately one-half mile upstream of Waters Creek mouth. The hydrologic analyses for the upper portion of the Applegate River were conducted using records from the 42-year period of unregulated flow (i.e., 1939-1980) at the USGS gagingstation near Applegate (No. 14366000) and the regulated flow curves provided by the COE. The accepted regulated discharges (i.e., regulation due to the Applegate Dam) were projected to additional locations of interest upstream of Wildcat Gulch near Murphy using the flow transfer formula described above. Peak discharge information was provided for the 10-, 2-, 1-, and 0.2-percent-annual-chance floods on the Applegate River, although only the 1-percent-annual chance flood profile was computed. Hydraulic Analyses Analyses of the hydraulic characteristics of flooding from the sources studied were carried out to provide estimates of the elevations of floods of the selected recurrencc intervals-Users should be aware that flood elevations shown on the Flood Insurance Rate Map (FIRM) represent rounded whole-foot elevations and may not exactly reflect the elevations shown on the Flood Profiles or in the Floodway Data tables in the FIS report. Flood elevations shown on the FIRM are primarily intended for flood insurance rating purposes. For construction and/or floodplain management purposes, users are cautioned to use the flood elevation data presented in this FIS report in conjunction with the data shown on the FIRM. Water-surface elevations were estimated at all cross sections by a computer program that computes energy losses between sections, using conservation-of-energy equations (step- backwater analysis! This hydraulic model requires accurate measurements of channel cross sections, bridge and dam geometries, and a proper evaluation of the roughness of the main channel and floodplains. The water-surface elevations at each cross section were determined by using the U.S. Geological Survey computer program E-431 (Reference 18). Locations of selected cross sections used in the hydraulic analyses are shown on the Flood Profiles (Exhibit 1). For stream segments for which a floodway was computed (Section 4.2)j selected cross section locations are also shown on the FIRM. Channel and cross section properties were determined by photogrammetiy based on aerial photographs taken September. 3.0, 1978 (Reference 19). Bridge geometries and the underwater portion of the cross sections were surveyed in January 1979. Roughness coefficients (Manning's "n") were based on field observation and aerial photographs. The range of roughness values used for all floods is shown in Table 5. Table 5. Flood Source Applegate River Deer Creek Gilbert.Creek Range of Manning's Roughness Values Main Channel Flood Plain 0.032-0.042 . 0.032-0.080 0.034-0.045 0.035*0.080 0.032-0.055 0.035-0.085 15 Table 5. Range of Manning's Roughness Values (continued) Illinois River 0.038-0.065 0.045-0.050 0:038-0.042 0.050-0.065 ,0.040-0.0,45 0.035-0.055 0.045-0-.060 0.034-0.080 0.034-0.080 0.034-0.080 0.034-0.080 0.034-0.080 0.035-0.080 0.050-0.080 canyons near Kerby Sours Flat area near Pomeroy Dam gravel & rock areas. East Fork Illinois River West Fork Illinois River overflow reach near 0.035-0.070 0.040-0.080 Lone Mountain Road Jumpoff Joe Creek Louse Creek Murphy Creek Rogue River through Grants Pass Slate Creek Waters Creek 0.032-0.055 0,033-0.048 0.045-0.050 0.030-0.065 0.031-0.038 0.032-0.055 0.030-0.070 0,032-0.100 0.035-0.080 0.045-0.080 0.032-0.09Ô 0.031-0.200 0.038-0.150 0.038-0.110 The initial water-surface elevations for the flood profiles on the Rogue River were derived from a step-backwater .convergence study.made through a five-section reach ending at cross section A. (Reference 20). Profile convergence was attained for each of the prescribed flows by using the U.S. Geological Survey computer program E-431. The computation procedure requires a uniform change in channel conveyance between cross sections. Also, in rapidly expanding reaches, the program assumes 50 percent of the energy is recovered between sections (due to uncertain eddy losses). Program E-431 became invalid at the outlet of two narrow canyons where chute flows and hydraulic jumps occurred (cross sections R and AB). Therefore, water-surfaee profiles through these canyons were estimated, and the hydraulic model was reset at the eanyon entrances using elevations derived by slope-conveyance studies. Both Hellgate and Robertson bridges are built well above the 0.2-percent-annual-chance flood levels, and neither would constrict the flows. The main channel varied from long calm reaches of silt, interlaced with boulders, to the bedrock outcrops of Hellgate Canyon. Flood plain vegetation varied from smooth, after- harvest hqp fields to dense, forests. The Rogue River floodway analysis began at.cross section BU. The initial 1 -percent-annual- chance flood elevation for the floodway was taken directly from the normal profile computed for the cross section. Because encroachment was not allowed downstream from cross section BU, no surcharge was computed for that cross section. The hydraulic analyses of the reach of the Rogue River in Grants Pass began at a point approximately 2.3 miles downstream of the city, where the overbank flow breakout returns to the channel. Photographs of the 1964 flood revealed that there was divided flow downstream of the city. The December 1964 flood discharges in Grants Pass (152,000 eft) closely approximated the published 1-percent-annual-chance discharge of 144,000 cfs, This 16 discharge resulted in well-defined overflows at the sewage treatment plant and at the RogueHa Mobile Home Park. The initial hydraulic analyses were conducted to identify the various flow behaviors. Three distinct flow patterns occurred; 1. The 10-percent-annual-chance flow was contained in the channel. 2. The 2- and 1-percent-annual-chance floods caused overflows on the right bank. 3. The 0.2-percent-annual-chance flood completely inundated the floodplain, An iterative hydraulic analysis for divided flows around the islands was undertaken to determine the flow distribution. In order to assess the significance of the overflows, survey data .were collected to describe the control section over which these overflows would occur. These data were subsequently incorporated into the hydraulic model using the HEC-2 divided flow option. The hydraulic analyses required flow and water-surface elevation balances between the main stem and the north overbank at three different locations. The results of the analysis were then compared with the 1964 flood photographs. It was identified that overbank flow returned to the channel at a point located approximately 2.3 miles downstream of the sewage treatment plant. Surveys of typical cross sections for both the channel and the north overbanks were conducted and then compared to data used in the existing Flood Insurance Study hydraulic model of July 1980. It was determined that the variations between the old cross sections and the recently surveyed cross sections were less then one foot. Therefore the existing cross sectional data were retained for profile computations. Water-surface elevations of floods of the selected recurrence intervals were computed through use of the COE HEC-2 step- backwater computer program (Reference 21). The 1-percent-annual-chance profile on the. Rogue River agreed favorably with many 1964 high-water marks found throughout the study area. However, an exact comparison of profiles is impossible in the lower reaches because of ungaged tributaiy inflow during the 1964 flood. There was a small disagreement on the Rogue River between the computed profile elevations and elevations determined from a stage-discharge relation at a gaging station in Grants Pass. A minor adjustment was, therefore, prorated from the gage to.the Seventh Street bridge, 0.6 mile downstream. The 1989 restudy of the Rogue River analyzed the reach from a point approximately 3.5 miles downstream of the South 6th Street Bridge in Grants Pass to apoint 2.2 miles upstream of the South 6th Street Bridge. The restudy included the proposed Redwood Highway crossing. The hydraulic study was conducted by the Oregon Department of Transportation's Hydraulic Division and was provided by FEMA to OTAK, Inc. The restudy used discharge values based on the original values used in the Josephine County Flood Insurance Study of December 1* 1981, which included the regulating effect of the proposed Elk Creek. Dam, soon to be completed by the COE. The regulated discharges include most of the anticipated benefit for the Elk Creek facility and were found to fall within the 90 percent confidence interva I of the unregulated discharges (i.e., without the Lost. Creek and Elk Creek facilities). The original cross sectional'geometry and roughness 17 coefficients for the Rogue River restudy were retained from the original modeling for the restudy computations. Known elevations from the effective modeling were used for the startingwater surface elevations of the restudy reach. The selected recurrence intervals were •computed using of the COE HBC-2 step-backwater computer program (Reference 21). Photographs of the 1964 flood of the Rogue River at the Qty of Grants Pass revealed divided flows around the islands located just downstream of thCcity. To determine the flow distribution, the split-flow option of HEC-2 was used. It was identified that the right overbank flow returned to the channel approximately 2.3 miles downstream of the municipal sewage treatment plant, The resulting water surface elevations matched within 0.2 feet of those published previously. The floodway analysis for the Rogue River restudy was computed using the full 1-percent- annual-flood discharge assuming no breakout flows. Flood profiles for Gilbert Creek began at the culvert on Rogue River Avenue, the first point where energy controls would not be influenced by backwater from the Rogue River. The initial water-surface elevations were determined from composite stage-dischargc relation computed at the culvert entrance. A composite stage-discharge relation is a graphic presentation that combines the amount of water flowing through the culvert with the amount flowing over the road, then relates the total flows to an upstream water-surface elevation. Flows through 23 Gilbert Creek culverts were computed using USGS computer programs E-431 and A-526 (Reference 18 and 22). Most road overflow situations involved flat street surfaces where flow direction was difficult to determine. Where unconfmed overflow occurred, the effective width was based on either the upstream channel geometry or the location of houses and garages in the approach section. In all cases, the amount of road overflow was computed using coefficients published in the. USGS Techniques of Water-Resources_Inyestigations (Reference 23). Storm-sewer inflows were estimated at West B Street and at Hillcrest Drive using outlet pipe diameters and by assuming the pipe gradient was equal to the ground slope to the nearest manhole structure. Resultant discharges were derived from the Manning equation for pipe flow as given in King's Handbook of Hydraulics (Reference 24). Both Gilbert Creek and Jones Creek have a trans-basin irrigation canal in the upper basin. The Tokay Canal diversion from the Rogue River is at a pumping station at Savage Rapids Dam, located 6.1 miles, upstream from the Grants Pass gaging station. The canal contribution to flood flows is uncertain because some flows can enter the basin as spillage from the canal. The ditch capacity at the pumping plant is 47 cfs, but the capacity Upstream from Hawthorne Avenue is only 27 cfs. This study assumes ditch flows are negligible during peak events. Flood profiles were drawn showing computed water-surface elevations to an accuracy of 0.5 foot for floods of the selected recurrence intervals (Exhibit 1). Initial water-surface elevations for the profiles on Jumpoff Joe Creek reflected concordant flows of the Rogue Ri ver. The 1-percent-annual-chance flood elevations on Rogue River extended 2.2 miles up the Jumpoff Joe Creek channel. The initial water-surface elevation used for the floodway analysis was estimated from a slope-conveyance study that did not consider concordant flow or backwater. The Jumpoff Joe Creek profiles continued uninterrupted past the confluence of Louse Creek in Merlin. An increase in channel gradient 18 upstream from Merlin made it necessary to establish additional cross sections. These cross sections were estimated by interpolating "between the geometries of the (Wo nearest cross sections, and by using a map having 4-foot contour intervals (Reference 19). Supercritical flow situations were encountered at three cross sections. Each situation required a resetting of the model using critieal-depth elevations for each of the prescribed flows. ; . At Russell Road, the 0.2-pereent-annual-chance flood overflowed the highway at a point 800 feet south of the bridge. A composite flow situation could not be computed because the flow in the main channel and flow in the overflow section did not share a common headwater elevation. Road overflow was estimated. The main channel consisted of gravel and small boulders and the oyer bank areas varied from pastures to dense forests. The initial water-surface elevations for profiles on Louse Creek were headwater elevations computed for the railroad bridge in Merlin. The headwater elevations were manually computed from a critical-depth section at the outlet of the bridge. Exact discharge values could not be determined because of unknown inflow from Harris Creek, a large tributary with a bridge 450 feet north of the Louse Creek channel. There is an exchange of flow between the two channels via a large ditch at the toe of the railroad embankment. An apportionment of flow through each structure could not be made because there is no common headwater elevation due to the lateral slope of the terrain. For the purpose of this study, it was assumed no peak flow exchange occurs during flooding. The 1-percent-annual-chance flood on Louse Creek was found to be contained within the main channel except at the railroad bridge in Merlin and at a bridge on Monument Drive. A portion of the Louse Creek floodplain, downstream of Monument Drive, was found to be susceptible to 1-percent-annual-chance sheet flow, a condition of overland flow where elevations and directions of flow are difficult to determine. Small embayments at the mouths of tributaries also would experience flooding. A floodway was designed to oceupy the entire width of the 1 -percent-annual-chance floodplain because any encroachment on the main channel would increase the stream velocities and aggravate bank erosion. Supercritical flow occurred at 18 cross sections in this reach. Because of the steep channel gradient, 21 additional cross sections were needed to define a continuous profile. The additional cross sections were estimated as described in the Jumpoff Joe Creek discussion. Approximately 30 percent of the I-percent-annual-chance flood flow on Louse Creek bypasses the bridge at Monument Drive at a point 600 feet north of the channel. The flow capacity of the bridge would not allow any encroachment on the flood plain, and a floodway analysis was not attempted. The channel consisted of gravel and cobbles, with some overhanging brush, and overbank values ranged from pasture grass to dense forest. The. 1989 study by OTAK, Inc. extended the portion of detailed study for Louse Creek by adding a reach extending from approximately 4.70 feet downstream of Monument Drive upstream to its crossing of Granite Hill Road, a distance of 2.9 miles. The starting water 19 surface elevation for the extended reach was based on known elevations froin;the effective modeling. Channel and cross section properties were surveyed between February and Juue of 1989. Water-surface elevations of floods of the selected recurrence intervals were computed through use of the COE HEC-2 step-backwater computer program (Reference 21). The average fall of Louse Creek throughout the study reach was approximately 90 feet per mile. This steep slope resulted in many supercritical flow conditions even though surveyed cross sections were taken at an average interval of 600 feet along the creek, Because of the steep channel gradient; 24 additional cross sections were added to the hydraulic model. Overall, the l-percent-annual-chance floodplain width on the upper Louse Creek varied from 50 feet to 1,000 feet. Because of the steep channel gradient for Louse Creek, the equal conveyance encroachment option that operates on the energy gradelirie was used for the floodway analysis. This method is suggested for steep waterways since it will not allow unreasonable encroaehments. The resulting floodway widths varied from 30 feet to 230 feet. The flood profiles for Applegate River began at its confluence with the Rogue River. Initial water-surface elevations were based on coneordant flows where backwater extended 1,180 feet up the Applegate River channel. The initial water-surface elevation for the floodway analysis was determined from a stage-discharge relation established at cross section BZ on Rogue River and does not consider coneordant flow or backwater. A natural constriction at cross section Z caused a supercritical flow situation for the 0.2- per cent-annual-chance flood. The change in the state of flow caused an unrealistic shape in the stage-discharge relation, and the 0.2-percent-annual-chance elevation was, therefore, estimated by extrapolating the rating curve. Supercritical flows were also encountered at a low diversion dam at the mouth of Murphy Creek. The hydraulic model was reset using elevations derived by critical-depth computations. A direct weir formula could not be used because of excessive bypass flow around the ends of the dam. The bed material of Applegate River varies from areas of unstable gravel and rock deposits to bedrock outcrops overlain by boulders and gravel. Much of the reach is subject to change due to scour and filling of bed material and to gravel mining. Floodplain vegetation varied from pasture grass to dense deciduous brush. On the south bank at cross section AE, an upstream bank projection would cause a portion of the cross section to become ineffective for transmitting flows due to a large eddy current. An unrealistically high V value was therefore assigned to reduce the conveyance in that portion of the cross section. The 1989 OTAK, Inc. analysis extended the Applegate River study from the previous upstream limit of detailed study to the Josephine-Jackson County line, an addition of approximately 5.6 miles. Known water surface elevations from the effective modeling were used as the downstream boundary for the extended modeling. Gross section properties were surveyed between February and June of 1989. Water-surface elevations of floods of the selected recurrence intervals were computed through use of the COE HEC-2 step-backwater computer program (Reference 21). No floodway was computed as a part of the 1989 analysis due to the lack of development pressure. The average fall of the Applegate River throughout the 1989. study area was approximately 17 feet per mile. With surveyed cross sections taken at an average interval of one every 3,000 feet, many critical depth statements were encountered during the initial hydraulic 20 simulations. This problem was solved By using the interpolated cross sections option of the HEC-2 model. Approximately 21 cross sections were automatically inserted by the hydraulic model throughout this reach of the Applegate. Overall, the 1-percent-annual- chance floodplain width on the limited detail study portion of the Applegate varied from l,200.feefto 2,700 feet. ' Initial water-surface elevations for profiles on Slate Creek reflect concordant flows of Applegate River. Backwater extended 5,500 feet up the Slate Creek channel. The initial elevation for the Slate Creek floodway analysis was determined by a slope-conveyance study through the first five cross sections of the reach (to cross section C). Concordant flow with backwater was not a consideration for the floodway analysis. Main channel bed material consisted of areas of rock and gravel deposits interlaced with boulders. The upper reach consisted of bedrock outcrops and boulders. Floodplain vegetation varied from moderate to extremely dense brush and tree growth. Waters Creek, a small tributary to Slate Creek, was studied by OTAK, Inc. in 1989 from its confluence with Slate Creek upstream for a length of approximately I mile. The starting water-surface elevation was computed using the slope-area method. The backwater elevations from Slate Creek at the confluence were computed based on a normal depth approximation for Slate Creek using a discharge computed from the flow/area transfer formula (Reference 16). The Waters Creek confluence is located approximately 3 miles upstream of the confluence of Hound Prairie Creek, Channel and cross section properties were surveyed between February and June of 1989. Water-surface elevations of floods of the selected recurrence intervals were computed through use of the COE HEC-2 step- backwater computer program (Reference 21). The average fall of Waters Creek throughout the study reach was approximately 50 feet per mile. This steep slope resulted in many supercritical flow conditions, even though surveyed cross sections were taken at an average interval of 300 feet along the creek. Because of the steep channel gradient, 17 additional cross sections were added to the hydraulie model. Overall, the 1-percent-annual-chance floodplain varied from 80 feet to 420 feet, Because of the steep channel gradient for Waters Creek, the equal conveyance encroachment option that operates on the energy gradeline was used for the floodway analysis. This method is suggested for steep waterways since it will not allow unreasonable encroachments. The resulting floodway widths varied from 30 feet to 100 feet. Initial elevations for the design-flood profiles for Murphy Creek were determined from a slope-conveyance study in the lower reach where all but the 0.2-percent-annual-chance flood were well contained in a rectified channel. A floodway analysis was not required on Mutphy Creek. Headwater elevations at the Southside Road bridge were computed using the U.S Geological Survey computer program A-526 (Reference 22). Supercritical flows were encountered at two cross sections (E and 1), and the model was reset using critical-depth elevations at each cross section. The.0.2-percent-annual-chance flood overflows Southside Road near the intersection of Williams Highway. Bypass flows then merge with Applegate River and do not re-enter thé Murphy Creek channel. The extent of road overflow was estimated because a composite stage-discharge relation could not be established at the bridge. Murphy Creek main-channel bed material consisted of loose rocks and boulders, and floodplain vegetation consisted of areas of unimproved pastureland, and moderate to dense brush and tree growth. 21 The flood profiles for the Illinois River began at a point 300 feet downstream from a gaging . station near ICerby (No. 14377100). The stage-discharge relation developed at the gage was used to determine initial elevations. The velocity distribution in a vast ponding of water at Sauers Flat, upstream from the gage, is uncertain due to eddy currents and slack water. The limits of the effective velocities were then estimated until upstream.profile elevations agreed with a stage-discharge relation established at a discontinued gaging station (No. 1437000) located at the Finch Road bridge in ICerby^ 3.6 miles upstream from the .initial cross section. A low diversion dam near Cave Junction (Pomeroy Dam) was completely submerged by all flows and did not affect profile elevations. As previously mentioned, the computation of flood profiles continued uninterrupted up East Fork Illinois River to Sucker Creek. As the Illinois and East Fork Illinois Rivers were treated as essentially one river, cross section locations on the East Fork Illinois River refer to the starting point of the profiles, Illinois River Mile 50.0, approximately 6.4 miles downstream from the confluence of the Illinois, East Fork Illinois, and West Fork Illinois Rivers. Cross section data for Illinois and East Fork Illinois Rivers were obtained from photogrammetry based on aerial photographs taken on September 30,1978 (Reference 19). Bridge geometry and underwater portions of the cross sections were surveyed in January 1979. There was a wide range in main-channel bed material throughout this study reach. In the canyon area north of Kerby, bed material consisted of boulders and bedrock outcrops. In the ponded reaches of Souers Flat, bed material consisted of soft bottom material with .brushy banks. Floodplain vegetation consisted of pastureland grass, cultivated farm lands (often bare during flood season), moderate to heavy brush and tree growth, and dense, deciduous brush and tree growth. Effective velocities at Sauers Flat were estimated by assigning high "n" values to reduee the conveyance in the noncoritributing areas of the floodplain. This technique was also used on East Fork Illinois River, upstream from the Redwood Highway. Extensive areas of shallow flooding were judged noncontributing because of the bank configuration upstream from cross sections M and N. Initial water-surface elevations for the second segment of the East Fork Illinois River were determined by using the converging profile technique through five cross sections ending at cross section A. The effective channel at cross sections A and B was adjusted to exclude the embayment at the mouth of Little Elder Creek. Supercritical flows were encountered at a narrow canyon near cross section J. The hydraulic model was reset using a critical depth elevation, and the profiles continued uninterrupted through the remainder of the reach. Bed material in the commonly braided main channel consisted of large areas of unstable rock and gravel deposits. There are bedrock outcroppings and large, rounded boulders in the narrow confines of the canyons,. but, generally, the entire reach appears subject to considerable movement of bed material. Flood plain vegetation consisted of some areas of pastureland, but moderate to heavy brush and trees predominated. 22 Flood profiles for the first segment of the West Fork Illinois River began at its mouth and reflect concordant flow conditions from the main stem of the Illinois River. Backwater from a 1-percent-an nil a 1-chance flood would extend 4,460 feet up the West Fork Illinois River channel. The initial Concordant flow (or backwater) and was derived by modeling the base flood from Pomeroy Darri to the initial section at the mouth. The effective velocities at the west bank of cross section J were uncertain due to the configuration of the upstream channel. The cross section width was therefore arbitrarily reduced to exclude an eddy flow situation. The main-channel bed material consisted of large areas of irregular bedrock outcropping overlain in places by loose sand and gravel deposits. Wide gravel bars are evident where the low-water channel is deeply entrenched near one of the banks. Flood plain vegetation consisted of moderate to dense brush and tree growth. Initial water-surface elevations for the second segment of the West Fork Illinois River profiles were derived by a convergence run through a reach (five cross sections) ending at cross section A. Flow was tranquil throughout the reach; the only problem encountered was a bypass-flow situation at the Redwood Highway bridge in O'Brien. The low north bank of the channel upstream from the bridge allows water to flow toward the intersection of Lone Mountain Road and Redwood Highway, located 1,800 feet north of the channel. It is possible that some of the water overflows the intersection and bypasses the entire reach downstream from the bridge. For.the purpose of this study, it was assumed that the entire road overflow was limited to 850 feet of roadway immediately north of the bridge. This limitation was based on the position of the upstream berm which contains all flow at the approach cross section (cross section L). Main channel bed material consisted of gravel bars at sharp channel curvatures, bedrock outcrops that formed deep low-flow pools and boulder-strewn reaches that appear unstable. Floodplain vegetation varied from pastureland grass to areas of dense brush and trees. The initial elevations for the flood profiles on Deer Creek were estimated by a convergence run through a reach with six cross sections ending at cross section A. McMullin and Thompson Creeks are tributaries that parallel Deer Greek throughout much of the central portion of this study reach. Although there is an exchange of peak flows near cross section R, it was assumed most inflow occurred at cross section P. Main channel bed material consisted of sizable areas of rock and gravel deposits which are subject to considerable movement during flood stages. Floodplain vegetation varied from pasture grass to dense brush and tree growth. Large acreages of cultivated farmland also occupy die floodplains. Flood profiles were drawn showing computed water-surface elevations to an accuracy of 0.5 foot for floods of the selected recurrence intervals (Exhibit 1). The hydraulic analyses for this study were based on unobstructed flow conditions. The flood elevations, thus derived are considered valid only if there are no significant changes made to the existing drainage structures or to other physical features of the channels (such as changes 23 in a l ignment and vegetat ion) . 3.3 Vertical Dátüni' All FIS reports and FIRMS"are referenced to a specific vertical datum. The vertical datum provides a starting point against which flood, ground, and structure elevations can be referenced and compared. Until recently, thestandard vertical datum used for newly created or revised FIS reports and FIRMs was the National Geodetic Vertical Datum of 1929 (NGVD 29). With the completion of the North American Vertical Datum of 1988 (NAVD 88), many FIS reports and FIRMs are now prepared using ÑÁVD 88 as the referenced vertical datum. Flood elevations shown in this FIS report and on the FIRMs are referenced to NAVD 88. These flood elevations must be compared to structure and ground elevations referenced to the same vertical datum. For information regarding conversion between the NGVD and the NAVD, visit the National Geodetic Survey website at www.ngs.noaa.gov, or contact the National Geodetic Survey at the following address: NGS Information Services N0AA,N/NGS12 National Geodetic Survey " SSMC-3, #9202 1315 East-West Highway Silver Spring, Maryland 20910-3282 (301)713-3242 (301) 713-4172 (fax) The conversion factor from NGVD to NAVD for all flooding sources in this report is +3.36 feet. Temporary vertical monuments are often established during the preparation of a flood hazard analysis for the purpose of establishing local vertical control. Although these monuments are not shown on the FIRM, they may be found in the Technical. Support Data Notebook associated with the FIS report and the FIRMs for this community. Interested individuals may contact FEMA to access these data. To obtain current elevation, description and/or location information for benchmarks shown on the FIRMs, please contact information services Branch of the NGS at (301) 713-3242, or visit their website at www.ngs.noaa.gov. FLOODPLAIN MANAGEMENT APPLICATIONS TheNFIP encourages State and local governments to adopt sound floodplain management programs. To assist in this endeavor, each FIS report provides 1-percent annual-chance floodplain data, which may include a combination of the following: 10-, 2-,l-, and 0.2-percent-annual-chance flood elevations; delineations of the 1-percent-annual-chance and 0.2-percent-annual-chance floodplains; and t-percent-annuail-chance floodway. This information is presented on the FIRM and in many components of the FIS report, including Flood Profiles, Floodway Data tables and Summary of Stillwater Elevation tables. Users should reference the data presented in the FIS report as well as 24 additional information that may be available at the local community map repository before making flood elevation and/or floodplain boundary determinations. 4.1 Floodplain Boundaries To provide a national standard without regional discrimination, the 1 -percent annual chance (100:year) flood has been adopted by FEMA as the base flood for floodplain management purposes. The 0.2-percent-anriual-chance (500-year) flood is employed to indicate additional areas of flood risk in the community. For each stream studied by detailed methods, the 1- and 0.2-percent-annual-chance floodplain boundaries have been delineated using the flood elevations determined at each cross section. Between cross sections, the boundaries were interpolated using topographic maps at scales of 1:2,400, 1: 4,800, and 1:62,500, with contour intervals of 2, 4, and 80 feet, respectively (References 8, 17, and 19). Gilbert Creek boundaries were determined on the basis of random topographic elevations taken during the field surveys. They may, therefore, not show local variations of either higher or lower terrain between points of definition. For streams studied by approximate methods, the boundary of the Lpercent-annual-ehance flood were taken from the Flood Hazard Boundary Map (Reference 3). The 1- and 0.2-percent-annual-chance floodplain boundaries are shown on the Flood Insurance Rate Map. On this map, the 1-percent-annual-chance floodplain boundary corresponds to the boundary of the areas of special flood hazards (Zones A and AE), and the . 0.2-percent-annual-chance floodplain boundary corresponds to the boundary of areas of moderate flood hazards. In cases where the 1- and 0.2-percent-annual-chance floodplain boundaries are close together, only the 1-percent-annual-chance floodplain boundary has been shown: Small areas within the floodplain boundaries may lie above the flood elevations but cannot be shown due to limitations of the map scale and/or lack of detailed, topographic data. For the streams studied by approximate methods, only the 1-percent-annual-chance floodplain boundary is shown on the Flood Insurance Rate Map. Countvwide Update As part of the countywide update, floodplain boundaries were digitized from the effective FIRM and Floodway panels. USGS topographic maps (Reference 25) and aerial photography (Reference 26) were used to adjust floodplain and floodway boundaries where appropriate. The 1- and 0.2-percent-annual-chance floods were redelineated on Gilbert Creek and portions of the Rogue River using new topography with a one-foot contour interval provided by the City of Grants Pass (Reference 27). The cross section locations were digitized from the effective Floodway panels or work maps. Elevations used for the redellneation were taken from the effective floodway data tables and adjusted to theNAVD88 vertical datum. The redelineation along Gilbert Creek extended from SW Rogue River Avenue to just upstream of NW Windsor Drive, a distance of approximately 2.5 miles. Redelineation along the Rogue River extended from approximately river station 111,810 (cross section CD) to river station 158,250 (cross section DJ). 25 in accordance with FEMA Procedure Memorandum 36 (Reference 28), profile baselines have been included in all areas of detailed study. Profile baselines are shown in the location of the original stream centerline or original profile baseline without regard to the adjusted floodplain position on the new base map. This was done to maintain the relationship of distances between cross sections along the profile baseline between the hydraulic models, flood profiles and floodway data tables. Floodways Encroachment on floodplains, such as structures and fill, reduces flood-carrying capacity, increases flood heights and velocities, and increases flood hazards in areas beyond the encroachment itself. One aspect of floodplain management involves balancing the economic gain from floodplain development against the resulting increase in flood hazard. For purposes of the NFIP, a floodway is used as a tool to assist local communities in this aspect of floodplain management.. Under this concept, the area of the 1-percent-annual-chance floodplain is divided into a floodway and a floodway fringe. The floodway is the channel of a stream, plus any adjacent floodplain areas, that must be kept free of encroachment so that the 1-percent-annual-chance flood can be carried without substantial increases in flood heights. Minimum Federal standards limit such increases to 1 foot, provided that hazardous velocities are not produced. The floodways in this study are presented to local agencies as minimum standards that.can be adopted directly or that can be used as a basis for additional floodway studies. The floodways presented in this study were computed for certain stream segments on the basis of equal-eonveyance reduction from each side of the floodplain. Floodway widths were computed at eross sections. Between cross sections., the floodway boundaries were interpolated. The results of the floodway computations are tabulated for selected cross sections (seeTable 6). In cases where.the floodway and 1-percent-annual-chance floodplain boundaries are either close together or collinear, only the. floodway boundary is shown. For the purpose of developing the 1-percent-annual-chance floodway for the Rogue River,, all of the flow was assumed to be confined to the main stem channel and its immediately adjacent overbank. As agreed upon by county representatives and FEMA, the computation of floodways on the Rogue River, downstream of Pass Creek, on Murphy Cieek, and on Gilbert Creek were not a requirement of this study. The area between the floodway and 1 -percent-annual-chance floodplain boundaries is termed the floodway fringe. The floodway fringe encompasses the. portion of the floodplain that could be completely obstructed without increasing the water-surface elevation of the 1- percent-annual-chance flood more than 1 foot at any point. Typical relationships between the floodway and the floodway fringe and their significance to floodplain development are shown in Figure 1. 26 R O O D W A Y FWPWE 1 -PERCE NTVWN'JSAJL-CHANCC F W O O P L A W — FLO 0 0 W A Y — 5TR5AM . C H A N N E L F L O O D E L I V A T T O N W H E N CONFLNED W I T H I N K O O O W A Y ENCROACHMENT • 04 * è 94tf»ir >«•(•••r»rt m »«•*» »F- J • wm rnm m « VlKtlMlOl -uZfT' WtólKltM' . J ^ F T O O D W A Y _ FRINGE AÄEAOf FL00MLAIH THATC0U10 8EUSÈD FOR, KVELOPMENtjiV ftAliffW GROUND FWOO ELEVATION BE FOflE ENCROACHMENT ON FljOODPlAIN UWMffTHeftOOÓEUVATlOflttf^ EHGÌOAÌHMEfiT. U$E£0tSTft£ FLOOD EÜVÄTÖN AFTÉÌtENCWÀCHMENT. . I^fflÒM^ EBHÌ^ TOaCEE&^ afWTtFtAKQUIiÌÉME^ CWlISSEKA Figure 1. Eloodway Schematic 27 OL til H < Q O ¿ o I i o o _J l l Ul £ Ö Q i > x 5 < 1- Q Z ^ O ti J Ui U. U. • n if w o o o o d d d o w o o (O m r> n o o ö o oo o (N o f. h iq s in w er» «n. ^ cj r^ tf) n rJ p-5 q (D r^ ui er» d i-" oi (d cri vi ei r-.* ui o CO in OJ (D d r- Iii oi (O r- CO « cn Ol CT» O) Ol Ol cn Ol SI z uio 2 " OiO iE IliUl >U- jjj CO 111 "" <0 I s Ul o »i w Q O £> Ui w CO CO § o "ob Tovj « ei O) » " s co » ? CO CO LO o>. it N vj Ol o s e) n ui • oi oi t£> ci tri aOOi-r-r-fMCM oi (D o iq „ _ vi oi d «i in to to to oo" oQ CO CT1 CT- CT»CT)0)0>0)CT>ai<7»0)iT»0)CT)CnCT)CT) T- CT ai ai cn oi o> oo to (O ri O (D r Ii) Oi oi t" (D oi <0" CO l*i 8) + _ CO CT CTO O O O r t - r W N n i t J W ( D ( O l f l ( O o 3 c o o o o o o o o ) o > o > o ) c > o ) 0 ) c t c t o ) o > o > o i c t o > c t o i o > N Ul O) ^ N in VI Ol N Ol n N O) VI «i tr -r ui o-- öd yf cJ «i if d «i CT <71 CT CT) cn O » to' cn T~" (O o o> ii £ K ir oi o S o o o o g g g o o o o o o o N . q s n « « l ^ * n N 4 o CO S (O to (O oo s § 1 ö in ^ * o a o 2 a «o g X Q> . fl> I • • . o < H < D I a o o - J Li. >-o z Ul § s Ul s UJ s >• o 2 Ul <5 OL UJ s Ul TABLE 6 1- PE R C EN T- AN N U AL -C H AN C E F LO O D W A TE R SU R FA C E E LE VA TI O N IN C R EA SE . (F EE T) - 0. 4 0. 5 0; 0 1. 0 0. 5 0. 3 0. 3 0. 5 0. 4 0. 0 0. 7 0. 0. 0. 8 0. 9 0. 9 0. 8 0. 6 0. 2 1. 0 0. 9 1- PE R C EN T- AN N U AL -C H AN C E F LO O D W A TE R SU R FA C E E LE VA TI O N W IT H FL O O D W AY (F EE T N AV D ) 99 9. 2 10 04 10 12 .5 10 17 .2 10 20 .3 1. 02 7. 0 1, 03 3. 9 1. 03 9. 1 1, 04 2. 6 1. 04 5. 9 1. 04 9. 2 1, 05 3. 6 1, 05 5. 5 1 1, 05 8. 0 1, 06 2. 9 1, 06 7. 2 1. 07 0. 1 1. 07 6. 2 1, 08 2. 1 1, 08 9. 0 1- PE R C EN T- AN N U AL -C H AN C E F LO O D W A TE R SU R FA C E E LE VA TI O N W IT H O U T FL O O D W AY (F EE T N AV D ) 99 8. 8 • 10 03 .5 10 12 .5 10 16 .2 10 19 .8 1, 02 6. 7 1, 03 3. 6 1, 03 8. 6 1. 04 2. 2 1, 04 5. 9 1. 04 8. 5 1. 05 3. 6 1. 05 4. 7 1, 05 7. 1 1, 06 2. 0 1. 06 6. 4 1. 06 9. 5 1. 07 6. 0 1. 08 1. 1 1, 08 8. 1 1- PE R C EN T- AN N U AL -C H AN C E F LO O D W A TE R SU R FA C E E LE VA TI O N R EG U LA TO R Y (F EE T N AV D ) 99 8. 8 10 03 .5 10 12 ,5 10 16 .2 10 19 .8 1. 02 6. 7 1, 03 3. 6 1, 03 8. 6 1, 04 2. 2 1, 04 5. 9 1. 04 8. 5 1. 05 3. 6 1. 05 4. 7 1, 05 7. 1 1. 06 2. 0 1. 06 6. 4 1. 06 9. 5 1. 07 6. 0 1. 08 1. 1 1, 08 8. 1 FL O O D W AY M EA N VE LO C IT Y (F EE T/ SE C ) 5. 2 16 .5 11 .2 6. 9 10 .4 5. 2 7. 9 5. 2' 10 .2 13 .0 14 .3 9. 9 6. 5 8. 8 9. 1 9. 8 11 .6 5. 8 7. 2 9. 7 FL O O D W AY SE C TI O N A R EA (S Q . FE ET ) 13 ,6 00 4, 30 0 6, 36 0 10 ,2 00 - 6, 84 3 13 ,7 00 • 8, 99 0 13 ,7 00 6, 93 0 5, 10 0 4, 66 0 6. 72 0 10 ,2 00 7, 57 0 7, 30 0 6, 80 0 5, 73 0 11 ,4 00 9, 25 0 6, 85 0 FL O O D W AY S LU 1, 83 0 52 0 55 0 90 0 60 0 16 90 10 90 '1 30 Ò 83 0 52 0 45 5 56 2 11 10 85 3 67 8 65 0 57 5 17 65 19 30 87 2 LU O OL O D IS TA N C E1 51 83 0 54 ,1 60 55 ,5 30 57 ,7 40 59 ,5 20 61 ,5 20 64 ,5 40 67 ,4 70 69 ,3 60 69 ,8 10 70 ,3 70 70 ,8 20 71 ,7 10 73 ,5 10 75 ,2 30 76 ,7 70 77 ,8 70 79 ,8 40 82 ,8 00 84 ,8 70 v/ o 2 5 o o u. C R O SS S E C TI O N g, "S ^ N < < < < < < < < < < < < < < < < < < ai o Q-Ä ex < < < Û î a o o - j LL ÙL LU > Ui ì III -1 û. CL < TABLE 6 £ LLI 1- < Q O II O UJ o z < X o -J < D Z Z < V-z ULI o or HI a. > - 0 a o o Ui o tc o « 0 z a o o u. UJ Ui _ < V- UJ UJ Q: LU u u. >; O < > H Q 2 > O h > o LU _J UJ UL LU 1 8 Hi < _J LLI o N o o CO CM "<* Q O O c o o i n O N N m o i c c i a i i n o i c o t i n o o o o o o o o o o o • o N Ol (M tO O) O) " ' CO 00 «11 00 N CO 00 ui CM T}; a> CO €0 CO , CM CM CM CO CO W t (S N N CO N U) _. .. . . _ .. . N t 0) (O o i c n o o o o o O T - c M c N C M c o c o T f T t - v n i o c o c a i D S c o c o c n CMCMCOCOCOrOCOCOCO co.co cocococococococococococococo co O) rr CO CM o oo CO co T- O) C0 00 CO CM r-' CO «) o> TT o CM 00* CM CO d o ui d o> co cri (D Ol Ol 00 o o o o o T— CM CM CM CO co Tf io IO co k t O 7 b m < o « L d O h 5 -i Iii mai > U- F a o » ui—' o> Q ui CO O) 00 r- CM co o co co CO T- 01 CO 00 to CO r-' CM CO 00 o> Tf o CM" aa ts cd d CJ) 01 O O o o o o CM CM CM CO co •«f CM CM CO co_ CO co co co_ co. co co_ co. CO co_ CO v- r T- i - T- i - t- T- T- T- i0OTf0>CD^0) - i Q O O —J LL fc z UJ o < I— 2 UJ £ tu 8 Z « £ S 2 UJ o at UJ £ ill ui Q HI u. TABLE 6 UJ al w < <~ UJ i - < LLI UJ q o o T— co in CD CO O) O) CO CT1 o o r-; K; 00 cq CM CM M; ct LU o i t 7 O d d d d d d d d o d d Q d d d CD d d d d a — Q O ¿ o > o < > H Q Z CM to * h- o in co in 00 m 00 CD CO CO CD CO r _ ^ cq o T-T r-' T-J ,-T tM CM -CM CO co co* in d co" in co" h-' ai CM iri r^ LO in m LO m m in m in in m m in in CO CO co «3 CO CD ID r- h- S g f t tM_ CM CM. CM_ CM CM_ CM_ CM_ CM CM CM CM_ CM CM CM_ CM. CM CM CM CM CM. CM^ CM_ CM _l 111 Ll t . , > a ^ ^ > CM co CO in O) ^ ^ CO O CO 00 Oi a> co h- ^ Ol 00 in cn O) CM d T- ^ T—° CM CM tM co to ^ CD cn CM to' in in to' 00 ^ -in m in m in in in in in m in m m m m CD co ^ CC Q ctr LU PZ CM to co m CD ^ co O in m m m in m in m co CO to CO co CO r- h-• h- CM_ CM_ CM_ CM CM. (M CM_ CM CM CM CM_ CM CM CM CM CM. CM CM CM. CM CM CM. CM CD UJ a: [u UJ LL > • o z t U J ^ r- to 00 cq to to O. CM in to CO cn to o CM CO CD 00 to § s t j UJ UJ (D CM cj cö cö co' co to cm" co V in CO cd h-' CO U-, < < UJ o£ < =5 ¡j 3 W 00 o co m in CO cn CM CO CO cn f- ^ m co 03 CM tM f 1 T CM CM CM CM CM CM to CM CM • T- T— T— T^ _J O W li. Uf « E l O CO o O CM CM O CO CM O 00 co co O o O o CO to. to tn CM_ o O o CO to co t- cn CJ f- cn CM CO OO co h- •rj- to CO co m CO to 9 ui > t- CM s o $ o CM. co o to f i co 3 ij-CM tsl cm" UJ UJ o Q - Q o o O o o o o o o o o o o o O o G) o -O z •n o CD co 0 01 > i O UJ cn [£1 o w M < o O UJ U- CD . re — _1 5 2 O a. O a: (A 3 > 3 K « O UL . « o a: o c l < f -< Q > - s Q O O - J S. Ö z UJ o < £ UJ -£• UJ (9 < -£ O z UJ o fc UJ E UJ UJ a tu TABLE 6 a: UJ i— < a o 3 LU UJ 0 2 < 1 O < -I < z> z z H 2 UJ o tf. UJ CL >-I o o LL UJ o a: 8 2 a O o u. vu co ^ K U J Ufe v a x S | K- O Z §815 ¿tü IP i s t 1 ' Ü ÜJ UJ L l oC — b "J S o ^ 5 ui w > u- If Hi CO 8 2 g a z o § to CO to o q; o « W CO CO to « N « N if (D CO CO CO WWW if N O) Cvi ^ j N n a s » 8 5 $ 8 t? 5 o s 0} < H < Q > - i a o o - j u_ >-o Z UJ 3 K Z UJ £ UJ s 5 s > o 2 <3 a UX •E ui 2 ui a ÜI u. TABLE 6 — • — — - F L O O D W A Y D A T A E A S T F O R K I L L IN O IS R IV E R 1- PE R C EN T- AN N U AL -C H AN C E F LO O D W A TE R SU R FA C E E LE VA TI O N I 1 IN C R E A S E (F EE T) i C. 5 : 0. 8 ,0 .8 0. 0 0. 0 0. 5 1. 0 0. 9 .1 .0 1. 0 1. 0 0. 7 0. 2 1. 0 1. 0 . 0 .5 0. 9 0. 6 1. 0 0. 1 0. 9 0. 9 1. 0 1. 0 0. 8 F L O O D W A Y D A T A E A S T F O R K I L L IN O IS R IV E R 1- PE R C EN T- AN N U AL -C H AN C E F LO O D W A TE R SU R FA C E E LE VA TI O N I W IT H FL O O D W AY (F EE T N AV D ) 1. 29 1. 3 1, 29 2. 9 1, 29 7. 0. 1. 30 2. 4 1, 30 3. 4 1. 30 6. 3 1, 30 9. 2 1. 31 1. 7 1. 31 5. 8 1, 32 1. 2 1, 32 5. 2 1, 32 7. 7 1. 33 0. 6 1. 33 4. 4 1. 33 8. 2 1. 34 3. 5 1. 33 8. 3 1. 35 1. 6 1. 48 4. 7 1. 49 0. 2 1. 49 6. 3 1. 50 3. 9 1. 51 3. 7 1, 52 3. 1 1, 52 7. 0 1 Fe et A bo ve Il lin oi s R iv er M ile 5 0. 0 2 In cl ud es W es t F or k Illi no is R iv er F lo od w ay F L O O D W A Y D A T A E A S T F O R K I L L IN O IS R IV E R 1- PE R C EN T- AN N U AL -C H AN C E F LO O D W A TE R SU R FA C E E LE VA TI O N I W IT H O U T FL O O D W AY (F EE T N AV D ) 1, 29 0. 4 1. 29 2. 1 1. 29 6. 2 1, 30 2. 4 1, 30 3. 4 1, 30 5. 8 1, 30 8. 2 1, 31 0. 8 1, 31 4. 8 1, 32 0. 2 1. 32 4. 2 1, 32 7. 0 1, 33 0. 4 1, 33 3. 4 1, 33 7. 2 1. 34 3. 0 1, 34 7. 4 , 1, 35 1. 0 1, 48 3. 7 1. 49 0. 1 1, 49 5. 4 1. 50 3. 0 1, 51 2. 7 1. 52 2. 1 1. 52 6. 2 1 Fe et A bo ve Il lin oi s R iv er M ile 5 0. 0 2 In cl ud es W es t F or k Illi no is R iv er F lo od w ay F L O O D W A Y D A T A E A S T F O R K I L L IN O IS R IV E R 1- PE R C EN T- AN N U AL -C H AN C E F LO O D W A TE R SU R FA C E E LE VA TI O N I R EG U LA TO R Y (F EE T N AV D ) 1, 29 0. 4 1. 29 2. 1 1. 29 6. 2 1, 30 2. 4 1, 30 3. 4 1, 30 5. 8 1, 30 8. 2 1, 31 0. 8 1, 31 4. 8 . 1, 32 0. 2 1, 32 4. 2 1, 32 7. 0 1, 33 0. 4 1, 33 3. 4 1, 33 7. 2 1, 34 3. 0 1, 34 7, 4 • 1. 35 1. 0 1, 48 3. 7 1. 49 0. 1 1, 49 5. 4 1. 50 3. 0 1, 51 2. 7 1. 52 2. 1 1. 52 6. 2 1 Fe et A bo ve Il lin oi s R iv er M ile 5 0. 0 2 In cl ud es W es t F or k Illi no is R iv er F lo od w ay F L O O D W A Y D A T A E A S T F O R K I L L IN O IS R IV E R FL O O D W AY ' M EA N I VE LO C IT Y (F EE T/ SE C ) 4. 1 8. 0 12 .5 6. 2 8. 1 7. 4 4. 9 6. 8 5. 2 7. 4 6. 9 6. 9 5. 2 6, 1 5. 5 5. 4 5. 7 7. 7 7. 6 5. 0 ' 8. 3 5. 4 12 .3 5. 6 11 .2 ' 1 Fe et A bo ve Il lin oi s R iv er M ile 5 0. 0 2 In cl ud es W es t F or k Illi no is R iv er F lo od w ay F L O O D W A Y D A T A E A S T F O R K I L L IN O IS R IV E R FL O O D W AY ' SE C TI O N A R EA (S Q . F EE T) • ^ I N ' T N N R A Q P I D I J B J ' I T R T O S R J ^ S O O F F L N ^ S I t í ro O to" ^ CM I N to " " ( 4 ? Í ch oí ™ CÑ- S Q N Œ T ® I D n s to" to JB r-* en cd" f-" N CO" f»" eo co N I O CM" en" co" CM" 1 Fe et A bo ve Il lin oi s R iv er M ile 5 0. 0 2 In cl ud es W es t F or k Illi no is R iv er F lo od w ay F L O O D W A Y D A T A E A S T F O R K I L L IN O IS R IV E R FL O O D W AY ' tJ LU § t 1.9 48 2 57 9 34 5 65 7 77 0 90 0 90 0 1, 01 0 1, 14 0 1, 00 0 ,8 35 80 0 1,1 18 ' 1, 32 5 1, 58 0 1, 45 0 1, 40 0 1, 26 0 46 0 , 69 0 49 9 66 0 27 4 42 4 58 2 1 Fe et A bo ve Il lin oi s R iv er M ile 5 0. 0 2 In cl ud es W es t F or k Illi no is R iv er F lo od w ay FE D E R A L EM ER G EN C Y M AN AG EM EN T AG EN C Y JO S E P H IN E C O U N TY , O R E G O N AN D IN C O R PO R AT ED A R E A S LU o O CO D IS TA N C E1 37 ,4 90 38 ,4 80 39 ,6 90 40 ,1 40 • 40 ,8 70 ' 41 ,8 70 43 ,0 10 44 ,3 70 45 ,5 30 47 ,2 60 48 ,3 50 49 ,2 40 I 50 ,5 50 52 ,1 70 53 ,1 60 54 ,4 50 55 ,7 30 56 ,4 90 82 ,4 00 83 ,3 10 ,8 4, 09 0- . 84 ,9 20 85 ,9 90 87 ,0 70 87 ,7 70 1 Fe et A bo ve Il lin oi s R iv er M ile 5 0. 0 2 In cl ud es W es t F or k Illi no is R iv er F lo od w ay FE D E R A L EM ER G EN C Y M AN AG EM EN T AG EN C Y JO S E P H IN E C O U N TY , O R E G O N AN D IN C O R PO R AT ED A R E A S o " z o o o _J u. C R O SS S E C TI O N * S " ° £ m M < O O Q I 1 1 ( L ( J I — "" î i£_JSZOQ.Oû£WI— 5 X >• S O S i 1 Fe et A bo ve Il lin oi s R iv er M ile 5 0. 0 2 In cl ud es W es t F or k Illi no is R iv er F lo od w ay FE D E R A L EM ER G EN C Y M AN AG EM EN T AG EN C Y JO S E P H IN E C O U N TY , O R E G O N AN D IN C O R PO R AT ED A R E A S TABLE 6 LU a: U) < H m H < UJ LU q q q q co co q CO cn q q r-. q CM VL Hi Ü t z ci o d ò o o d d d o d o o T " d d Q O g 2 ¿ o > O x i i 1- O z OJ IO co co (O co CO co q CM CO q M c\i CM co « I CO V I CM" co* CO rt co <71 d lU H O < CO co co "J- io co R- co co cn o CM co CO in IO in IO. IO IO IO. IO 1- V* in LO. in in CD. ID CÛ co. CO. q _l UI g u i ». UJ í ¿ CM co co co co iq q o IO - _ ( £ Q D : UI O > 1 - < S í CM CD co co CO IO a» OL q I O T- q co in q q co CM* CM ed IO CM co" R-' co' h-" cn eò co CM CO ai H-' A . co co co M- io co 00 «A co O) o CM co co in I w lo KÏ tr> io. IO. IO in f i có co CO to. co_ (Ô co. UJ TZ a: — T- £ o •7 H U I < O W o H~ co co V co co q io "J" co CM cn vl; M q g S S ¡ I O u> co co" cri \f r-' ai IV.* ai ai co" CO vi - LU UJ > U^ < á < ÍD ! h» o IO cn co CO CM CM Q ai O) IO ai co Tf r- co xf >o O IO XL- io Q co (fi co t - en CM O o " : CO •«f CM. o CM q in co. co. A I q (Ö CM. « O F a <*» cvf ^ CM" L U A W UJ to g e CO (fi h» Q co cn S CTI o •«T «ci co O CO Q O O I H co CM O CM o 00 O IO O) H - T—• CO CO co co _ _ UJ 1 I L r> co CV| CM to co CM co co CO CM CM CM CM io I O Ui "LU o. Q Q O O o o O O o O O O O O CM CO • o co CM o z ^— co CO CO en co Oí CO OJ co aÌ CM CM co. O) O oc n O < ^— co CO CM (o co. o . O. o O o Q . 00 ; oo oo" oí Q R-" CM" t" io" CO- oo" aì oT o" CM* Q s W 5 co co CD en (fi (fi cn OL CA ai Ol w 0 z tft 'o 2 o T3 a> O H a c c O O UJ w m c N < m O Û Ili LL ò X 5 5 Z O CL O o u < < < < < < < < < < < < < < < -J £2 i LL. LU to o i o 1 M S> M li£C < h -< Q > - s Q O O _J LL oc HI F-< Q O S z ¿ O i O o LU ë S w o z a o o ILI to — < UJ LU CC LU Ö t. >; a < > I ? < H Û Z J in l i s ¡§t¡ $ Zi UJ te Q S Ë UJ lZ Oí ~ ¡>-0 h III < U W ¡ 3 Ë ILI ILI > U-. S < LÛ z UJ O ^ b « ILI OT 9 ui ai o z g UJ' M « « g o O G) O o o o* iri m io o o if R^ T-' T-1 Ò o ' o R^ O o o o o o o o O O V- d o d "to "o d co" co CO OI O) CM CM CM in cri^in cd r-' ri N co m o W ui ra w o¡ m od CM -¡T co co coco co co co co (O p) n n ci o_ ^ t^ ^ ^ tïo tî- s SÌ s o Ô o CO O) O) -CM CM CM CM CO CO p ^ «O CM A O M" 00 CO M" m n N ra N q n cr>cr>o)OT-T-T-CM T-; co r¡ oí co' m w n w o ^ r a f j o i n n N O i N O n f f l N t i ^ N O O O T - R - T - C M O I < O E Û W A > C D O ) O > O - T - T - T - C M C O C O C O C O C O C O C O C O C O C O C O C O C O C O C O - 1 - T I - T J - T J - ^ J - «1 N M r N <- Ul N n o oi N m N ffl co" io" to m7 co vi vi CONN M Ç4 IO R I I ) O ) CO I O CO CO CM O O T - C O O C O O O o c o c o o o c o o c o .CO CO .R- CO CM R- CM CO CO IO >f o o o o o o o a o o o o o. o o o o 9 p | N O l N O O « i - O N n ^ r ( M I 9 r N n lo « Íñ S ? t « <0 1 o « ^ °>- ^ »". °í " " ? ç s s ? O) tf) . " ' - k V r-- rf * «r h-- Ó» o i? î2 ç' í? Qi ^ N ^ I O I O N * J II < B l ü Q l l l l t ( ¡ I I - - i ! ¿ - 1 S Z Ú t L O t t : w i - 3 > 5 K cu. o o tu o < H < Q >- i • o o Li- er: LU > DC co o z * a: o IL H w UJ 5 1- PE R C EN T- AN N U AL -C H AN C E FL O O D W A TE R S U R FA C E EL EV AT IO N IN C R EA SE (F EE T) N o f i in a o ò d 1- PE R C EN T- AN N U AL -C H AN C E FL O O D W A TE R S U R FA C E EL EV AT IO N W IT H FL O O O W AY (F EE T N AV D ) 1. 43 2. 5 1. 43 7. 6 1, 44 2. 4 î 1, 44 8. 6 1- PE R C EN T- AN N U AL -C H AN C E FL O O D W A TE R S U R FA C E EL EV AT IO N W IT H O U T FL O O O W AY (F EE T N AV D ) 00 (D 1-. T-- T^ CM* CO CO O "t Tf ^ "d- ^ 1- PE R C EN T- AN N U AL -C H AN C E FL O O D W A TE R S U R FA C E EL EV AT IO N R EG U LA TO R Y (F EI ET N AV D ) 1, 43 1. 8 1, 43 7. 6 1, 44 2. 1 1, 44 6. 1 1 O O -J U- M EA N VE LO C IT Y (F EE T/ SE C ) 10 .7 12 .8 12 .4 14 .1 SE C TI O N A R EA to. *-" C\f Csf CO" in in - in in FL O O D IN G SO U R C E C R O SS S EC TI O N W es t F or k Illi no is R iv er ( co nt in ue d) Y Z AA AB ' < Û î a o VJ Li- tt: tu > a: Iii UJ < I-LLJUJ -a: w o t >; Q i > f i s 5 § t i _j UJ Ll U. |8tn < JUJ U- U- o o c j c > o c M r - - - c o w r - - O T - o d d o o o d d o o o o d o n « (o ifl o d d O O W O IN CO t Q ^ o o o o a o o "a 'cq *p CO (N M N IN 0O M (D (>) CO IO o Tj- f*- 1—CO CO CO CO o c o o ) o o o 3 c o < o ^ ^ r ; i : o W m s r t N O J i i i ' t N n N - - 4 \ ~ CO a> _- _ r .- . - O T- CM co O Q O O O O O O O W N I i l i l W N O O l r CM in co_ r^ co CN. oi q —r O," - I'M c in. M-J5ZOCLO. Q i W I - D > 5 X > - 2 < Q > i Q O O LL •Ö z UJ o < £ UJ s UJ o £ < E $ z UJ CD K UJ E Ul 2 Ul Q UJ li. TABLE 6 oc lu I— < Q O ¿ O ü ! ^ O z < X o § UJ LJ (n < t - 111 UJ CiL UJ O t 2 > Q < > I ? < ^ ÛZ ' SE Lu LL. UJ ü_ (t cO q T- q Ö d O O ló (O Ol N IO co o o o d d h- CO O o o O 00 O O O CM 'Sf o o o- ' o o o o (O W N W V) W o) co oo (O s CM ra ai co" oo V ri IRI N N s r N o in o H N o oí N oí ri cd oí ai N M M l D O O Û r T - C J N n t O t ' f t i n i I l i û i û N N S d ) c û o o o o o Q Q ) 0 ) 0 ) 0 ) 0 ) 0 ) o i ( j ) o } o ) 0 ) 0 ) G > ( ^ o ) a ) a } o i o ) o i o co (O CM m p co 1- I"» en f - O) ra oq IO oq CM ><* vn CM h- h- O) O) Oí ai 0) cr> O) en cr> O) CTI Ol O) O) O) 0 c io N io o t M V s oí s œ co o in to N M; io CM ^ f-; CM 01 n » ^ n iti N r i n r t o o ^ Q r V ' o ai (ri o i r i n oí ai S to o) O) O O O r i - M N (1 rt t >í to y (Û ® r Î- N «) C 5 A C I I 0 G 1 0 I U I O ) O 1 0 ) 0 ) 0 ) 0 ) 0 ) C I ) 0 1 £ I L 0 ) 0 ) 0 ) C D 0 ) T I L A > >-I o o o _ ! U_ -p. h UJ < o ( 2 | S f c ¡ lU ILI > U-. S < & § ¡ U P a o w LU "" in gis 9 uj c^ioiû. N. s à t m h w m n h oi n ® N N ° ra ai S S io co £ O) oq CM co œ (ó oi N to ai s ^ CM CO K-- ™ & ÎC £ ÏS E? i2 £? _• • N m 01 N (0 s I £ ( û t ï a i m s s K ) ( o o î > i i a i n x i - t o a c M T - c n T - t M i o o o i o o t --OJCO.COOl I - S W Ol S ^ -J 5 z o o . o k w i - D > 5 < < < < < < < < < < < < < < < < < < < < < < < Ol LU f-< Q O ¿ o ai f- o < 1 5 3 ™ ! < P «f CO z UJ g UJ Q_ >-S Q O o I i i . ü cc D O CO o z Q O Q -I u. LU kW o Ü> 2 > Q i l l Za "4 i t ¡SE 2 WW Tu s w I ü tri r^ o Q O ö ö ö CD I N CM -if (7) Ol Ol m T- cn cn cn cn x* 00 CM CM O TJ"' 5 o s S J5 to to o ° M O O O O O Sen co oo _ C0_ CO. (!) ffl O* r n n t t M at £ _ O -n Ai i^J u 1 $ 'S 5 a : 1.8 E 3 < I— < Q >- i Q O O - J LL S z UJ <9 Ul CD < 2 Ö 2 Ul O cc Ul s . tu t tu o UJ TABLE 6 a: UJ t- < Q O 3* LU I - u < >-I o o LL UJ o a; r> o CO (D " Z a o o uj w --<£ H LU UJ a: LU o t >- Q < > x 5 < 1- Q 2 ^ o tj j U i - U. U- pi £ o h E o UJ W > ^ CC Q H ¡S >- o -R B UJ < o w gsta UJ LU > U . < £ 2 UJ o"; h a o w LU w Ui 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 o o' o o' o' o' d d d o d d o d d o d . d o o d d d o d o_ if v to «1 in 'f o d d d CM' N. d •M- T- r- o O) (D o 1; CO x— q T- O CO in «J o> V CO oi N." cm' in d in •tt CM f ^ in d cm' o o o T— CM CO co xj- in in (O CD CO cn cn Ol Ol CT1 o> Ol cn cn Ol Ol CO Ol Ol o? Ol Ol cn o o o o o o o o q a » 00 d N^ CM in d in •«t od CM in d cm' o o o T- CM co co t -M- in in CO CO CO cn O) O) cn cn Ol CT1 a> O) Ol O) Ol CJ> Ol Ol CD cn a ) O) t r- <0 W in V d cn O) Ol O) o a> cn T R ( D K) UL T co" co D CM R^ co o o O T- T- CM o o o o o o ^ a> 9 CM ^ 2 r cri N £ oo r ^ • U I F M N N I O O I T O U I A V I Q I D S N O I O T T I I O N cocomcocoinoor^cnoovncnr-cocnot^cMinmT-i^coco - - - - - - " " " ~~ w n t ' f n i t n ' t n i i i n n i n i f o vn co " ^ — ™ . - W. co co co co in to co II ? LL UJ o z g o 2 o UJ w w w o cn o t J i n c o T t c o o o o o ^ -¡Ü N I O l O S O l C l t O o Tt oi m co U R- L^ L «4J 1— rT\ N T- T- T- T- ® " M 2 -^ m ~ it pe pi s 5 S o o o o o o a o a o o a o o a o o a o o a o a a CM CM CM CO. in H - CM v-" T-" T-" CM" CM" CO" co xt Tf" in co co" co" r->" h- oo" cn ai 3 c N N i - i s z o a. a ct to h d > 5 x >• o < I -< Q > - < Q O O LL z UJ H Z UJ £ Ul (3 < Z I s z UJ ¡3 UJ £ Ul t UJ a UJ Ll TABLE 6 OL UJ H < Q O 3 - z e o UJ H UJ ? - 1 g l l J V U J d o 3 < 5 L L 5 £ ULI o UJ D. >-I o o - J LL UJ o üt D O (0 CD 2 a o s LL Ui w —. < I-UJ UJ OC W Ott > D < > x 5 < (— Q Z -jUJ . >- Q i o t i § I I UJ LL. LL en a R S UJ u. Oi — ¡5 t UI O S f c UI UJ > UL. s < JJ Z o LLI LL PO o UJ to a tu > u. 2 O K O UJ w w w o q: o o o o a o o o o o o o o o o a o in in «q vi ai (N r--' ai oi vi -t M Q ™ < < < < < < < a: — < H UJ UJ q Q Q o o O o CO q o q CM O O q q K W O i t z o d o o d o d d d o d o O d d d D o S z ¡ Z o £ Q x l | H Q Z m CM o i n o> CM CM o> i n i f CM in CD d t r o i CD T-' CO d r-* È r- ' d d CM i n I i i t o < 00 CO Ol i— CO M- c - Ol * - xf CD CO ä B f c i T-. 1-. r - . CM. CM T - t— CM CM. CM. V" CM CM CO q CO co. co 1 § g w _ 1 I U LL U-_ l i s I g t ü m CM q i f O) cn CM OJ •n CM CM r - i n q d i f O) d 1 - oo' d CD f^ d T^ d CM d r - CO oo cr> r- CO (D t-- CD T- T— CD CO I S r - * - T-. v " r - CM CM. t- T— CM Oi T— CM. CM CM T*- q q q CO. CO. w 5 - j tu u . i - z U J OC Q Q Ì ££ I f UJ l i . te — vn CM q i n vf- O) CM CF1 m P i CM i n - t^ d •T- d I CM i n C L co co O) R CD K OJ T- co co • T^ r - CM CM CM w CM co o) . rt T - 1 ' T- 1 - T - T - t— T- o - F i— U J i o » q o o i n i n CO o CM q « Ì o ¡ S f c LU U J CD (J CM t— d d r - T- d d o d CM' d CM CM « d > LL 0 ä < & Q z U J CM o to CD cn T- CM o « j co CM CO CO CM oo r - O o 1 1 : co ä K CO « - - o 1 - f - o o f co CM o i f CM co co co t o CO CO CM CM CM CO O F O _ J u . UJ OT O) CM CM 00 CD o < AO o N w i CD CO O g LU i b CM. IO CD CD 0Q o o 00 Ol CO o T- t IO co i n T u U J o 2 CM s s S S 5 i n cn £ f ? s o CD CO CM - t to T-•n f*- o < O CO f^ - " 1 cn cn CO Co cn LCI « 3 5 C o AY a . s CD CD U Q £0 CO U J m U . m (0 CD I CD £ 2 CD ÜQ 5 Z ca m < % Q > - I Q O O - J LL * LU Ili ttÌ o III w :d o TABLE 6 UJ in ^ Q: UJ i < H UJ UJ q CM r; CM CM CM q if in CM C7J q TO CO CO q q CD d q q CT) O q q t£ LU d o d d o d d d o d d d o o o d o d d d d d r- T- T—' < O t z £ a o O >- Q < > \L g x S < if CM CO q co o q T~ O) Ui in q CM O) q r-- CM q q q o q CT) q H Q 2 d if xf if xf d d d d ^ d d V^ d d d CM d d - d if d LU 1 Jj UJ CO CO 00 a> a> CT) a> O) o o o t— i— t— O < 00 CO CO 00 CO 00 00 CO CO 03 CO 00 00 oo CO CO oo CO O) CT) O) a> aj O) CD z ?! <5 o " ! LL LU •i w P w 1 o g z if d q CM if if CO q if xf CO q d d CM d f-- r-* q CM d <6 q d q if CM q if q d 'f 00 O eo d q CM q d q "f* r- r- r- . r- co CO 00 00 cn O) cn CD o a c? T— T— i -CO CO 00 00 a) CO co CO 00 CO oo CO oo CO eo 00 CO OO O) O) O) cn cn Ol cn 1— z UJ o > ^ EC a Di o > UJ % If q CM CO CO oo co CM q CM f-; OJ q If q if q q q q a. d if f^ if if if d d d 1= to d O) CM if d if d d CM d r- r- r- r- r- t-- CO CO CO CO a> O) CT) O) a o o => tj CO 00 CO CO CO tO 00 ao 00 CO CO CO CO CO CO CO 00 CO cn o> cn CJ> cn a> cn Ul EC ~ £ O 2; t UJ u> q in if q q q in co • q If q in q q q q o cn q if u-' if xf d CO d d d - « d CM JI d d d d d d UJ Ul' > U. < < UJ _ < Lj o O O o a o o o o o o o o o if co 3 o oo CO CM co 00 tn 5 Q 1IJ o a o o o o o o o O o o O o CM f- co ^— O) co cn co r- O § v in a) co o. co CM a> CM. CM it CO It in co o co it • T— o •«t CO rs r^ , ~ n nj s 60 d ^ co" in" to d co d cm" CM d Tt d CM" CD Tf d o F a co Ul ID in in co co T— T— T— T— 7—• T- T—' O CO LU iU "" Ui o o to in a m o m tn in tn o o o o co s CO 00 oo CM s CM CO r-- co to co •M- o> co co CM it to CO o It in "it CO s a .in in Offi CO o> if co co f-. CM co CM T; CO €» m (O o CO 00 P > LL T-" CM CM" CM d d co" CM CM" CM" co co" CM* CM" Tu o z o o o o o o o o O o o O o CJ o o CM cn cn' cn cn cn. cn CO ip UJ o o S 3 m m CO A> CO <4 " ^ X >- BZ < to u ' Q Ul u. t9 X 3 s- Z O a. a 01 O CD CO QQ m m BZ O o o O O O O o O O O o o O o o o O _J 11 Ui Ul o> o o o: D; o 2 < Q i Q O O _ l UL >-o z UI a v- z Ui E tu 3 >-0 z Ul s Ul § 1 Ul a ui TABLE 6 or Ui H < Q O ¿ O UJ H UJ U J tn < J - UJ UJ tt Hi o t > O i > H D 2 >Ol - > o UJ Zj UJ U. U- ¡ g I 5 ¿8! > q: a b S L L £ o ffl to «•) in t o in rt o d 0 0 0 d o 0 0 o o M- « c \ i M - < r ) o o o o o c o 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 o o (o o 10 n o in q it n n 01 ^ io ai to n if n in n o N CO M oi (S ^ in (D N Ol I-' pj O tü K r N ri Iii ffl O) (D r ffl0)0)0)0)ffla)oo)0)0)oi0)0)(j)oi0)0)0)cna)0)0)a)a)0i 3 s OO 1— f^ - Tf CM CO Oi Tf T— cn \rr | lNUJUWNINO (D h h ® N ri in (D (O CO r « cna)0)0)0)(i)cno)0)0)0)0)ma)(ji(ji(jicji0) R-- 10 a O CM CM O o o t- CM CO f-' h-* CO T- 1- 1- i- . . to o) a> a> o> T^ N n; N a oi Tf t- oi t- t^ —' (o ^ - 1 Q O O - J LL I O O - J LL < o i 5 g S f c ui ui > L L < fc 2 UJ I": <3 TO UJ W 9 tu 5 U - ' «f r O . q CO CM CO CO O) oi Ifl Ol ffi N q q q o : CM T-" T-" T-' CO 10 1 - CM T - CO I - 1 CM CO- c^ co co co o cn T- cn co cm 00 S 8 S g g CO O OJ CM 1 -JO JJ g Oi CO s? CM. CM O O O O O O O o o o o o 0 0 cMr-co«h-oocn 0 iNTiNTiNT o" O C3 N N t- CO t- -f to O 2 A O O UJ O 2 g a 2 O UJ TO to CO O a: O CV^ CO CO S S N CD. 0)_ O) Q COO O) OO O O O O O O O O O O O O a\ ,o> cn cn T- q o r. « N 10 N K o P I ^ CM CM CJT to co Q." co o CM" N jo ai co cn CM co co eg lOlOlOCOCOCOCOCOCO S 1 5 3 3 , ö ö 8 S S 8 ' 8 5 111 li. Ü 1 - 2 _ Q Q Q O Q ^ J 5 Z q a q a O a O K w D O Q Q Q CC TABLE 6 tí. Ui H < Û o S z ¿ o Ui H O < z < 3: o < Z Z «í H Z Ul ü ft Ui ü_ >- I Q O O LL Ui O ce rs o « CD z Q O O [LI CO < t- UJ LU OL UJ O t Z > Q 5 > I- Q Z _J UJ L l LL ¡ 1 S I s t i ? Zi UJ L l L l q q q q q CM q q q q d Q o o d o ö d o ò d o q co o co q d o d ^ d o q q ( O N O ) « " ' ï--- q r-- q T- q q O q q q CM q q CD d CM CD r--' d -f" r-' 00 CM co d d. d ï - CM CM CM CM co CO •M" IO m co co r--en O) O) en O) en en O) 05 en O) en en 05 05 CD iD UJ li. a: —- ¡3 h ui o Ö UJ UJ > LL 1 & O«h p a o w UJ "" 03 S uj 5 u_ 7-- "o "d "CM ^ ^ T-; q q q CM q q R- q v ^ q q ' q Ul N O) N ® ö « «> lû oi xf r C) N r- (D cri f^ f-^ a ) O ) O ) a ) o ) C T > o > C T , a , o ) a > c 0 O , O ) a , < n a , O ) c n q ta q r- q T-; o q CM CM q q r-; q T- q q q d d CM d d CM d d d d T- d d CM CM CM CM CM CO TJ- ij- •Sf VI m IO co r--en O O) O) en O en en ai en O) a> er> en O) Ol en ai q oo i - -tf" "f" xf M o t*. CD co iri CO T-cd d q q q CD OO O ) O io o o i o «3 (D eo CD q t- h- T-" T-" CM" CM" a a a o T - O) Ö) CM 5 n •t s h co co o T " CO CM o 9 UJ 0 1 O z o g UJ co m co O a: o T - T O C O I O I O H - O O I O R - S O C M S G R ^ ' o O O o o o o o o O . h- (û CD 00 IO N O (û T- CT) O) OD (O N If Q cm" co co" to cd" h-T (C oo" aT oí ^ „ „ O O Q O O O O Q 9 2 W O ) d l O ) í O r O l r j ? S r . h. "I \ i ^ - - - — T—" (M* co" -rt IO" IO* to" O < m u O Ul l i lu I - o i i J 5 Z O û . O K ( D O o: ô S O 0) < 1 s ® 4} Q. < < Q >• < ? û O O - J LL FL O O D W A Y D A TA W AT ER S C R EE K 1- P E R C E N T- A N N U A L- C H A N C E F LO O D W A TE R SU R FA C E EL EV AT IO N IN C R E A S E (F EE T) o i n q t D q i r j q q q n o c M <"""-. T - t i " ) * ~ o q o o o o o" o <- O Q Q x^ o o o o" a d ò 1 Fe et A bo ve C on flu en ce w ith S la te C re ek FL O O D W A Y D A TA W AT ER S C R EE K 1- P E R C E N T- A N N U A L- C H A N C E F LO O D W A TE R SU R FA C E EL EV AT IO N W IT H , FL O O D W AY (F EE T N AV D ) 1, 09 6. 2. I 1, 09 7. 7 1, 10 6. 1 1, 10 7. 1 1, 11 1. 7 I 1, 11 5. 7 1, 11 6. 5 1. 11 0. 7 1. 12 2. 4 1. 12 2. 8 1 ;1 33 .3 1, 14 0. 7 1. 14 4. 1 1. 14 5. 2 1. 14 5. 5 1, 14 7. 4 1, 1. 50 .6 1, 15 3. 1 1 Fe et A bo ve C on flu en ce w ith S la te C re ek FL O O D W A Y D A TA W AT ER S C R EE K 1- P E R C E N T- A N N U A L- C H A N C E F LO O D W A TE R SU R FA C E EL EV AT IO N W IT H O U T FL O O D W AY (F EE T N AV D ) 1, 09 6. 2 1, 09 7. 2 1, 10 6. 1 1, 10 6. 5 1, 11 1. 7 1. 11 5. 2 I 1, 11 5. 5 1, 11 8. 7 1. 12 2. 4 1. 12 2. 5 1. 13 3. 3 1. 14 0. 5 1. 14 3. 4 1. 14 5. 1 1. 14 5. 0 1, 14 7. 3 1. 15 0. 6 1. 15 3. 1 1 Fe et A bo ve C on flu en ce w ith S la te C re ek FL O O D W A Y D A TA W AT ER S C R EE K 1- P E R C E N T- A N N U A L- C H A N C E F LO O D W A TE R SU R FA C E EL EV AT IO N R EG U LA TO R Y {F EE T N AV D ) 1, 09 6. 2 1, 09 7. 2 1, 10 6. 1 1, 10 6. 5 1, 11 1. 7 1. 11 5. 2 I 1, 11 5. 5 1, 11 8. 7 1. 12 2. 4 1. 12 2. 5 1. 13 3. 3 1. 14 0. 5 1. 14 3. 4 1, 14 5. 1 1. 14 5. 0 1, 14 7. 3 1. 15 0. 6 1. 15 3. 1 1 Fe et A bo ve C on flu en ce w ith S la te C re ek FL O O D W A Y D A TA W AT ER S C R EE K FL O O D W AY M EA N VE LO C IT Y | (F EE T/ SE C ) ( D r t O i a J ^ ^ q ' l q o i ' P i n h . p i o i q c D m 1 Fe et A bo ve C on flu en ce w ith S la te C re ek FL O O D W A Y D A TA W AT ER S C R EE K FL O O D W AY SE C TI O N A R EA {S Q . F EE T) W T f l û N i f l i o a i s o œ i i i o r O t ô N t û m . IO OO I f O) (O (O r r l D I D M n i O T - x r ' t W i i ) i f i - r t r O l N N r N r i - N P I P l r r r r 1 Fe et A bo ve C on flu en ce w ith S la te C re ek FL O O D W A Y D A TA W AT ER S C R EE K FL O O D W AY § 6 gs to to-Tf x J - w n r t W T f r t T f o D M n n ejoJ 1 Fe et A bo ve C on flu en ce w ith S la te C re ek ! FE D E R A L EM ER G EN C Y M AN AG EM EN T AG EN C Y JO SE PH IN E CO UN TY , O RE GO N AN D IN C O R PO R AT ED AR EA S FL O O D IN G S O U R C E D IS TA N C E1 23 0 ' 8 40 1, 74 2 2, 10 3 2, 34 8 2, 73 1 2, 86 6 3, 16 3 3. 3B 7 3, 67 1 • 4, 58 7 4, 96 1 5, 14 8 5, 33 6 5, 59 7 5, 85 2 6,1 12 6, 20 0 1 Fe et A bo ve C on flu en ce w ith S la te C re ek ! FE D E R A L EM ER G EN C Y M AN AG EM EN T AG EN C Y JO SE PH IN E CO UN TY , O RE GO N AN D IN C O R PO R AT ED AR EA S FL O O D IN G S O U R C E C R O SS S EC TI O N ' M Ö> flî 0 g < ea o o uj H. (J I - - » M - I S Z O O - O Q : 0» 1 1 Fe et A bo ve C on flu en ce w ith S la te C re ek ! FE D E R A L EM ER G EN C Y M AN AG EM EN T AG EN C Y JO SE PH IN E CO UN TY , O RE GO N AN D IN C O R PO R AT ED AR EA S TÄBLE6 INSURANCE APPLICATION For flood insurance rating purposes, flood insurance zone designations are assigned to the community based on the results of the engineering analyses. These zones are as follows: Zone A Zone A is the flood insurance rate zone that corresponds to the 1 -percent-annual-chance floodplains that are determined in the Flood Insurance Study by approximate methods. Because detailed hydraulic analyses are not performed for such areas, no base (1-percent-annual-chance) flood elevations (BFEs) or depths are shown within this zone. Zone AE Zone AE is the flood insurance rate zone that corresponds to the 1 -percent-annual-chance floodplains that are determined in the Flood Insurance Study by detailed methods. Whole-foot BFEs derived from the detailed hydraulic analyses are shown at selected intervals within this zone. Zone X Zone X is the flood insurance rate zone that corresponds to areas outside the 0.2-percent-annual- chance floodplain, areas within the 0.2-percent-annual-chance floodplain, areas of 1-percent-annual- chance flooding where average depths are less than 1 foot, areas of 1-percent-annual-chance, flooding where the contributing drainage area is less than 1 square mile, and areas protected from the 1- percent-annual-chance flood by levees. No BFEs or depths are shown within this zone. ZoneD Zone D is the flood insurance rate zone that corresponds to unstudied areas where flood hazards are undetermined, but possible." Table 7 lists the flood insurance zones that each community is responsible for regulating. Table 7. Flood Insurance Zones Within Eaeh Community Community Flood Zone is) Cave Junction, City of AE, X Grants Pass, City of AE, X Josephine County, Unincorporated Areas A, AE, X , D FLOOD INSURANCE RATE MAP The Flood Insurance Rate Map is designed for flood insurance and floodplain management applications. ;For flood insurance applications, the map designates flood insurance rate .zones as described in Section 5.0 and, in the 1 -percent-annual-chance floodplains that were studied by detailed methods, shows selected whole-foot BFEs or average depths. Insurance agents use the zones and BFEs in conjunction with information on structures and their contents to assign premium rates for flo.od insurance policies. -47 For floodplain management applications, the map shows by tints, screensv and symbols, the 1 - and 0.2-percent-annual-chance fl'oodplains floodplains, floodways, and the locations of selected cross sections used in the hydraulic analyses and floodway computations. The county wide Flood Insurance Rate Map presents flooding information for the entire geographic area of Josephine County. Previously, Flood Insurance Rate Maps were prepared for each incorporated community and the unincorporated areas of the County identified as flood-prone. This countywide Flood Insurance Rate Map also includes flood-hazard information that was presented separately on Flood Boundary and Floodway Maps, where applicable. Historical data relating to the maps prepared for each community are presented in Table 8, "Community Map History." OTHER STUDIES In December 1965, the U.S Army Corps of Engineers published a Flood Plain Information report which described the flooding in Josephine County during the 1964 flood (Reference 29). Flood boundaries for the 1964 flood, and estimated boundaries for the 1861 flood were shown on aerial photographs. No profiles were presented. In July 1966, the U.S. Army Corps of Engineers published a statewide Post Flood Report describing the floods that had occurred in December 1964 and January 1965 (Reference 10). A discussion of flooding from streams within Josephine County included graphic displays of cumulative precipitation and storm hydrographs. In November 1970, USGS published a profile study for the Rogue River in a reach extending from the Grants Pass gaging station to the Lost Creek for the 1964 flood and for the 10- and 20-year floods, based on hydrology considered to be effective at that time. Also presented were cross sections and channel plan views. Profile concurrence for the design floods was not attempted because of significant changes in the hydrologic analyses due to revised flood-control estimates. Also present were cross sections and channel plan views. Profile concurrence for the design floods was not attempted because of significant changes in the hydrologic analyses due to revised flood- control estimates. In July 1971, the U.S. Geological Survey prepared a Flood Insurance Study for Josephine County (Reference 30). The report presented base flood elevations and estimated flood boundaries which were shown on enlarged portions of 10-minute quadrangles having 80-foot contour intervals. Flood profiles for the 500-, 100-, and 10-year floods were based on the same hydrology used in the previously described Profile Study (Reference 31). The Type-10 study did not include the incorporated area of Grants Pass. In July 1975, the U.S. Army Corps of Engineers published a statewide Post Flood Report describing floods that had occurred in January 1974 (Reference 12). A discussion of flood magnitudes and storm damage was similar to their report issued after the 1964 floods in Oregon. A Flood Insurance Studies have been published for the unincorporated areas of Jackson County (Reference 1 and 32). The hydrologic analysis used in the Grants Pass study is consistent with the analysis used in the Jackson County study. 48 O \ RO 0 \ 0 \ CO ON CT\ i—I .—I R-" R-^ FNT 1 U G & U Q & M en •a > o 0\ & O g 3 t-ON S i-l Ü l-H (N G T (N u 4Î P 1 ä w S 0 Flood Studies were prepared for the incorporated area of Cave Junction (Reference 33), and for the incorporated area of Grants Pass (Reference 34). All data presented in these studies agree exactly with data presented herein. .., Irf November T974, a Flood Hazard Boundary Map was published for Cave Junction (Reference 35). This Flood Insurance Study is more detailed and, thus, supersedes that map. This report either supersedes or is compatible with all previous studies published on streams studied in this report and should be considered authoritative for the purposes of theNFlP. 8.0 LOCATION OF DATA Information concerning the pertinent data used in the preparation of this study can be obtained by contacting FEMA, Mitigation Division, Federal Regional Center, 130 228th Street, SW, Bothell, Washington 98021-9796. 9.0 BIBLIOGRAPHY AND REFERENCES 1. Federal Emergency Management Agency, Flood Insurance Study, Jackson County, Oregon (Unincorporated Areas), January 5, 1979 •• 2. Northwest River Basin Commission, Columbia Basin Inter-Agency Committee, River Mile Index. Rogue River and Tributaries in Oregon. Vancouver, Washington, 1967 3. U.S. Department of Housing and Urban Development, Federal Insurance Administration, Flood Hazard Boundary Map. Josephine County. Oregon (Unincorporated Areas). Scale 1:24,000,1977 4. State of Oregon, Oregon Blue Book. Salem, Oregon, 1977-1978 . 5. U. S. D epartment of Commerce, B ureau of the Census websi te, http://www.census.gov/mainywww/cen2000.html 6. Oregon State Water Resources Board, Rogue River Basin. Salem, Oregon, January 1959 7. U.S. Department of the Interior, Geological Survey, Water-Supply Paper 1649, Water for Oregon. 1965 8. U.S. Department of the Interior, Geological Survey, 15-Minutes Series Topographic Maps. Scale 1:62,500, Contour Interval-80 feet: Grants Pass, Oregon (1954) 9. Ü.S. Department of Commerce, National Oceanic and Atmospheric Administration, National Climatic Center, Climatographv of the United States No. 81 (Oregon). Monthly Normals of. Temperature. Precipitation, and Heating and Cooling Degree Days. 1941-1970 10. U.S. Department of the Army, Corps of Engineers, Portland District, Post Flood Report. Portland, Oregon, July 1966 50 -11. U.S. Department of the Army, Corps df Engineers-, Portland District, Cumulative Frequency Curve - Maximum Annual Discharge, Rogue River at Grants Pass. Portland. Oregon, 1976 and 1978 12. U.S. Department of the Army, Corps of Engineers, Portland District, Post Flood Report. Portland, Oregon, 1975 13. U.S. Department of the Army, Corps of Engineers, Portland District, Cumulative Frequency Curve--Maximum Annual Discharge, Rogue River at Grants Pass. Portland, Oregon, 1976 and 1978 14. U.S. Department of the Interior, Geological Survey, Log-Pearson Type III Flood-Frequency Analysis Using Guidelines of Water Resources Council (Program. J-407). Chapter 1, Section C, vol. 4, P.Ii. Corrigan and W. Kirby, 1976 15. U.S. Water Resources Council, "Guidelines for Determining Flood Flow Frequency," Bulletin 17, 1976 16. U.S. Department of the Interior, Geological Survey, Open-File Report 79-553, Magnitude and Frequency of Floods in Western Oregon. D.D. Harris, L.L. Hubbard, and L.E. Hubbard, 1979 17. City of Grants Pass, Contour and Drainage Maps, Scale 1:2,400, Contour Interval 2 feet: Grants Pass, Oregon (1957) 18. U.S.. Department of the Interior, Geological Survey, Water Resources Division, Open-File Report 76-499, Computer Applications for Step-Backwater and Floodwav Analysis, Program E-431, J. O. Shearman, 1976 19. U.S. Department of the Interior, Geological Survey, Oregon District, Contour Map of Selected Reaches of Streams in Josephine County. Oregon, Scale 1:4800, Contour Interval 4 feet: Josephine County, Oregon, 1979 20. U.S. Department of the Interior, Geological Survey, Water-Supply Paper 1869-A, Definition of Stage-Discharge Relations in Natural Channels by Step-Backwater Analysis. J.F. Bailey and H.A. Ray, 1966 21. U.S. Army Corps of Engineers, Generalized Computer Program HEC.-2 Water-Surface Profiles, September 1988, Error Correction 03, Hydrologie Engineering Center, Davis, California 22. U.S. Department of the Interior, Geological Survey, "Preparation of Input Data for Automatie .Computation of Stage-Discharge Relations at Culverts," Techniques of Water-Resources Investigations. Book 7, Chapter C-3, H.F. Matthai, H,E. Stull, and Jacob Davidian, 1968 23. U.S. Department of the Interior, Geological Survey, Water Resources Division, "Measurement of Peak Discharge at dams by Indirect Methods," Techniques of Water-Resources Investigations. Book 3, Chapter A-5, Harry Husling, 1967 24. H.W. and E.F. Brater, Handbook of Hydraulics, 4lK Edition, New York: McGraw-Hill Book Company, 1954 51 25. U.S. Department: of the Interior, Geological Survey, 7.5-Minute'Series Topographic Maps: Map Name Date Scale Contour Interval Applegate 1983 \ 24,000 40 ft Buckskin Peak 1989 1 24,000 40 ft Bunker Creek 1989 1 24,000 40 ft Cave Junction 1989 1 24,000 40 ft Eight Dollar Mountain 1989 1 24,000 40 ft Gal ice 1989 1 24,000 40 ft Glendale 1986 1 24,000 40 ft Go Idea 1986 1 24,000 40 "ft Grants Pass 1986 1 24,000 40 ft Holland 1989 1 24,000 40 ft ICelsey Peak 1989 1 24,000 40 ft Kerby Peak 1986 1 24,000 40 ft King Mountain 1983 1 24,000 40 ft Merlin 1986 1 24,000 40 ft Mount Reuben 1989 1 24,000 40 ft Murphy 1986 1 24,000 40 ft Murphy Mountain 1986 1 24,000 40 ft O'Brien 1989 1 24,000 40 ft Onion Mountain - 1989 1 24;0QQ 40 ft Rogue River 1983 1 24,000 40 ft Selma 1989 '1 24,000 40 ft Sexton Mountain 1986 1 24,000 40 ft Takihna 1989 1 24,000 40 ft Wilderville 1986 1 24,000 20 ft 26. Josephine County, Aerial Photography, 2005 27: City of Grants Pass, OR, Topographic Mapping, Contour Interval I-foot, 2004 28. Federal Emergency Management Agency, Procedural Memorandum No. 36 - Profile Baselines on Digital Flood Insurance Rate Mans (DFIRMs) with Orthophoto Bases. Washington, D.C., July 7, 2005 29. U.S. Department of the Army, Corps of Engineers, Portland District, Flood Plain Information - Interim Report. Portland, Oregon, 1965 30. U.S. Department of the Interior, Geological Survey, Water Resources Division, Flood Insurance Study. Josephine County, Oregon (Unincorporated Areas). Preliminary Draft Report, unpublished 31. U.S. Department of the Interior, Geologieal Survey, Water Resources Division, Open-File Report, Water-Surface Elevations and Channel Characteristics for Selected Reaches of the Rogue River and Elk Creek'. Jackson and Josephine Counties. Portland, Oregon, 1970 32. Federal Emergency Management Agency, Flood Insurance Study. Jackson County. Oregon. (Unincorporated Areas). September 27, 1991 33. Federal Emergency Management Agency, Flood Insurance Study. City of Cave Junction. Oregon, unpublished, September 27, 1991 52 34. Federal Emergency Management Agency, Flood Insurance Study, City of Grants'Pajs; Oregon, November 1980. 35. U.S. Department of Housing and Urban Development, Federal Insurance'Administration, Flood Hazard Boundary Map, City of Cave Junction, Oregon. Scale 1:12,000, 1974 10.0 REVISION DESCRIPTIONS This section has been added to provide information regarding significant revisions made since the original Flood Insurance Study was printed. Future revisions may be made that do not result in the republishing of the Flood Insurance Study report. To assure that any user is aware of all revisions, it is advisable to contact the community repository for your community. All previous study revision descriptions have been incorporated into the appropriate sections of this FIS. Table 9 summarizes the flooding sources updated since the original study was completed. Table 9. Revised Study Descriptions Flooding Source Community Rogue River Rogue River LouseCreek Applegate River Waters Creek Gilbert Creek Josephine County Unincorporated Areas and the City of Grants Pass Josephine County Unincorporated Areas and the City of Grants Pass Josephine County Unincorporated Areas Josephine County Unincorporated Areas Josephine County Unincorporated Areas City of Grants Pass Limits of Study From approximately 3.5 miles downstream to 2.2 miles upstream of the South ó"1 Street bridge From approximately 5.2 miles downstream to 3,5 miles upstream of the South 6th Street bridge From approximately 470 feet downstream of Monument Drive to Granite Hill Road From the upstream end of the initial analysis to the Josephine- Jackson County line From its confluence with Slate Creek upstream approximately 1 mile From SW Rogue River Avenue to just upstream of NW Windsor Drive Revision Date September 19, 1990 November 2008 September 19, 1990 September 19, 1990 . September 19, .1990 November 2008 Panel Numberfs) 0484, 0492, 0503,0511, 0512, and 0516 0491,0492, 0503,0511, 051.2, 0516, 0517 0314, 0501, and 0502 0708,0710, 0720,0740, and 0750 0656 0504 53 Countywide Update ("December 3, 2009) The countywide update was completed in November 2008 by WEST Consultants, Inc. for FEMA under Contract No. EMS-2OO1-CO-O068. This update combined the Flood Insurance Rate Maps and Flood Insurance Study reports for Josephine County and incorporated communities into the countywide format. Under the countywide format, FIRM panels have been produced using a single layout format for the entire area within the county instead of separate layout formats for each community. The single-layout format facilitates the matching of adjacent panels and depicts the flood-hazard area within the entire panel border, even in areas beyond a community's corporate boundary line. In addition, under the countywide format this single FIS report provides all associated information and data for the entire county area. As part of this revision, the format of the map panels has changed. Previously, flood-hazard information was.shown on both FIRMs and Flood Boundary and Floodway Maps (FBFMs). In the new format, all base flood elevations, cross sections, zone designations, and floodplain and floodway boundary delineations are shown on the FIRM; the FBFM has been eliminated. Some of the flood insurance zone designations were ehanged to reflect the new format. Areas previously shown as numbered Zone A were changed to Zone AE. Areas previously shown as Zone B were changed to Zone X (shaded). Areas previously shown as Zone C were changed to Zone X (unshaded). In addition, all Flood Insurance Zone Data Tables were removed from the FIS report and all zone designations and reach determinations were removed from the profile.panels. All flood elevations shown in this FIS reportand on the FIRM panels were converted from NGVD 29 to NAVD 88. The conversion factor from NGVD to NAVD for all streams in this report is +3.36 feet. The 1- and 0.2-percent-annual-chance floods were redelineated on Gilbert Creek and portions of the Rogue River using new topography with a one-foot contour interval provided by the City of Grants Pass (Reference26). The cross section locations were digitized from the effective Floodway panels or work maps. Elevations used for the redeiineation were taken from the effective floodway data tables and adjusted to the NAVD 8 8 vertical datum. The redeiineation along Gilbert Creek extended from S W Rogue River Avenue to just upstream of N W Windsor Drive, a distance of approximately 2.5 miles. Redeiineation along the Rogue River extended from approximately river station 111,810 (cross section CD) to river station 158,250 (cross section DJ). The floodplain boundaries for all other flooding sources.were digitized from the effective FIRM and Floodway panels. Aerial photography (Reference 25) and USGS 7.5* Quadrangles (Reference 24) Were used to adjust floodplain and floodway boundaries where appropriate. 54 c N : O M P L E T E R E P O R T L O C A T E D I N .'• application. (1) Plan drawn to scale showing the nature, location, dimensions and elevations of the area in question; • ." (2) Existing and proposed structures, manufactured housing pads, fill, storage of materials, drainage facilities, and the location of the foregoing items; - (3) Elevation in relation to mean sea level, of the lowest floor (including basement) of all structures; (4) Elevation in relation to mean, sea level of floodproofing in any structure; (5) Certification by a registered professional engineer or ~ architect that the floodproofing methods for any non- residentxal structure meet the floouproofing criteria in Section 13.262; (6) Description of the extent to which any watercourse will be altered or relocated as a result of the proposed development; (7) Existing and proposed roadways; (8) Area, location and finish elevations of all fill walls and rip-rap; (9) Location and elevation of stored materials; (10) Location and elevation of drainage facilities;- ( .(11) Location and elevation of utilities; and (12) Other plan requirements of this Code as applicable; 13.243 Elevation Certification. All required elevations shall be tied into known bench marks shown on the: Flood Insurance Rate Map by a registered professional surveyor. Said surveyor shall attest to the procedure, bench marks used and accuracy of the required elevation over his signature and seal upon the required plan displaying the élévation information.~ 13.244 Designation of Local Administrator. The Community Development Director is hereby appointed to administer and implement this Article by granting or.denying development permit applications in accordance with its provisions. 13.245 Duties and Responsibilities of Director. The duties of the Director shall include, but not be.limited to, the following: ( 1) Permit Review. (a) Review all development permits to. determine that the permit requirements and conditions of this article have been satisfied. (b.) Review all development permits to determine that all necessary permits have.been obtained from those Federal,. State or local governmental agencies from which prior.approval is required. . (c) Review all development permits to determine if the proposed development is located in the floodway. If located in the floodway, assure that the encroachment provisions of Section 13.270 are met. (2) Use of Other Base Flood Data (in A and V Zones). When base flood elevation data has not been provided as required by this article, the applicant shall obtain and the Director shall review and reasonably utilize any base flood elevation and floodway data available from a Federal, State or other source, in order to administer this article. (3) Information to be Obtained and Maintained by the Director. (a) Where base flood elevation data is provided through the Flood Insurance Study, Flood Insurance Rate Maps, or as required in Section (2) above: Obtain and record the actual elevation (in relation to mean sea level) of the lowest floor (including basements and below-grade crawlspaces) of all new or substantially Improved structures, and whether or not the structure contains a basement. (b) For all new or substantially improved floodproofed structures where base flood elevation data is provided through the Flood Insurance Study, FIRM, or as required in Section (2) above: (i) Verify and record the actual elevation (in relation to mean sea level); and (ii) Maintain the floodproofing certifications required in Section 13.242(5). (c) Maintain the records of all appeal actions and variances, and report any appeal actions or variances to the Federal Insurance Administration upon request. (d) Maintain for public inspection all records pertaining to the provisions of this ordinance. (4) Alteration of Watercourses. fa) Notify adjacent ..communities, the Oregon Department of Land Conservation and Development (the State's' NFIP Coordinating Agency), the Oregon Water Resources Department, and any other appropriate... state and federal agencies, prior to any alteration or relocation of a watercourse, and submit evidence of such notification to the Federal Insurance Administration. (b) Require that maintenance is provided within the altered or relocated portion of said watercourse so that the flood carrying capacity is not diminished. (5) Interpretation of FIRM Boundaries. Make interpretations and determinations where needed, as to exact location of the boundaries of the areas of special flood hazards (for example, where there appears to be a conflict between a mapped boundary, and actual field conditions). If the location of a boundary is contested, the person contesting the location of the boundary shall be given a reasonable opportunity to appeal the interpretation or determination as provided in this article. Such appeals shall be reviewed consistent with the standards of this code and Section 60.6 of the Rules and Regulations of the National Flood Insurance Program (44 CFR 59-76). (6) Location o,f FIRM Boundaries and Elevations. (a) Make all information relating, to.the 100-year flood plain and floodway location and elevations available to the applicant, including the Flood Insurance Study with flood sections, the Flood Insurance Rate Maps showing flood elevations and elevation data reference points, and other floodplain development surveys in the immediate vicinity. (b) Certify that the location of the floodway and 100- year flood plain,, and existing and proposed elevations, have been made for the applicant by a professional land surveyor registered in Oregon, and that the signature and seal are affixed certifying the accuracy of' such determination. (c.) . Certify that the finished floor elevations, and other finished elevations of the. proposal affecting the floodway or 100-year flood plain have been constructed or developed to . the approved elevations', as certified by a registered professional surveyor over, his signature, and seal. (d) Upon request, provide the information in this Section to the applicant, applicant's lender and/or insurance agent.. -(e) Should an applicant pursue a change in floodplain. or . floodway designation.from the Federal Emergency - . . Management Agency,.assist the applicant with information about the process. Variances. Variances to the provisions of this Article shall be processed in accordance with the procedures of Article 2 and the provisions of Article 6 of this Code. Any variance to the Flood Hazard provisions of this Article shall include a recommendation of the City Engineer as specified in Section 6.060(B)(11) and shall address the additional provisions of this Section, except as provided in Subsection (3) of this Section. Factors to Consider. The review body shall consider all. technical evaluations, all relevant factors, and standards specified in this Article, and the following: (a) The danger that materials may be swept onto other lands to the injury of others; (b) The danger to life and property due to flooding or erosion damage; (c) The susceptibility of the proposed facility and its contents to flood damage and- the effect of such damage on the individual owner and occupants; (d) The importance of the services provided by the proposed facility to the community; (ej The necessity to the facility of a waterfront location, where applicable; (f) The availability of alternative locations for the proposed use which are not subject to flooding or erosion damage; (g) The compatibility of the proposed use with existing and anticipated development; (h) The relationship of the proposed use to the comprehensive plan and floodplain management program; (i) The safety of access to the property in times of flood for ordinary and emergency vehicles; (j) The expected heights, velocity, duration, rate of :ri-se, and sediment transport of the flood waters and the effects of. wave action, if applicable, expected at the site; and (k) The costs of providing governmental services during and after flood conditions, including maintenance . and repair of public utilities and facilities such . as' sewer, "gas, electrical,, and water systems, and streets' and" bridges . Additional Guidelines and Requirements for Variances, to the Provisions, of this Article. In addition to the variance criteria in Article 6, the review body shall address the provisions, of this Section. (a) Generally, the only condition under which a variance from the elevation standard may be issued is for new construction and substantial improvements to be erecced on a lot of one-haIf ac^e or less in size contiguous to and surrounded by lots with existing structures constructed below the base flood level, providing the iterns in Subsection (1) of this Section have been fully considered. As the lot size increases, the technical justification required for issuing the variance increases. (b) Variances shall not be issued within a designated floodway if any increase in flood levels during the base flood discharge would result. (c) Variances shall only be issued upon a determination that the variance is the minimum necessary, considering the flood hazard, to afford relief. (d) Variances to the provisions of this Article shall only be issued upon findings of: (i) A showing of good and sufficient cause; (ii) A determination that failure to grant the variance would result in exceptional hardship to the applicant; (iii)A determination that the granting of the variance will not result in increased flood heights, additional threats to public safety, or extraprdinary public expense; create nuisances; cause fraud on or victimization of the public in consideration of the factors of Subsection (1) of this Section; or conflict with existing local laws or ordinances. (e) Variances as interpreted in the National Flood Insurance Program are based on the general zoning law principle that, they pertain to a physical piece of. property; they are not personal in nature and do not pertain to the structure,. its inhabitants, -.economic or financial circumstances. They primarily address small lots in densely populated residential neighborhoods. As such, variances from the flood -elevations should be quite rare. -(f) ..Variances may be issued for non-residential buildings in very limited circumstances to allow a lesser degree of flood-proofing than watertight ox ; dry-proofing, where..it can .be determined, that such .aqtion will have low damage potential, comply with all other provisions of this Subsection other than (a), and otherwise comply with the provisions of Section 13.252 (Anchoring) and 13.253 (AH Zone Drainage). (3) Exceptions ror Historic Properties. Variances may be issued for the reconstruction, rehabilitation, or restoration of structures listed on the National Register of Historic Places or the Statewide Inventory of Historic Properties in accordance with Article 6, without regard to the additional provisions of Subsections (1) and (2) of this Section. In such case, the variance shall be part of the review and approval by the Historic Buildings and Sites Commission required in Article 13.400 of this Code. In addition: (a) Such variances shall be only the minimum deviation from NFIP criteria that is necessary to assure that the historic character and design is not destroyed; and (b) The variance must not preclude the continued designation of the structure as an historic structure. Any measures that can be taken to reduce future flood damage consistent with this Subsection shall be required, such as elevating an air conditioner or using flood- resistant materials. (4) Conditions Attached to Variances. Upon consideration of the factors in Subsection (1) and the purposes of this Code and Article, if à variance is granted, the review body may attach conditions to the variance as it deems necessary to further the purposes of this Code. (5) Notification of Effect on Flood Insurance Rates. Any applicant to whom a variance is granted shall be given written notice that the structure will be permitted to be. built with a lowest floor elevation below the base flood elevation and that the cost of flood insurance will be commensurate with the Increased risk resulting from the reduced floor elevation. (6) Record-Keeping. The Director shall maintain the records of all variances and- shall report any variances to the Federal Insurance Administration upon request. 13.247 Appeals. Appeals to Interpretations of the provisions of this Article or determinations regarding the application, of the provisions of this Article shall be undertaken in as provided in Article 10 of this Code. The Director shall maintain the records of all appeal actions and shall report any appeal actions to the Federal Insurance Administration upon request. 13.250 Provisions for Flood Hazard Reductio^ 13.251 General Standards. In all areas of special flood hazards, the standards set forth in this Article are required. 13.252 Anchoring. (1) All new construction and substantial improvements shal1 be anchored to prevent flotation, collapse, or lateral movement of the structure. (.2) All manufactured homes shall likewise be anchored to prevent flotation, collapse or lateral movement, and shall be installed using methods and practices that minimize flood damage. Anchoring methods may include, but are not limited to, use of over-the-top or frame ties to ground anchors (Reference FEMA's "Manufactured Home Installation in Flood Hazard Areas" guidebook for additional techniques). 13.253 AH Zone Drainage.. Adequate drainage paths are required on slopes to guide floodwaters around and away from proposed structures. 13.254 Construction Materials and Methods. (.1) All new construction and .substantial improvements shall be constructed with materials and utility equipment resistant to flood damage. (2) All new construction and . substantial improvements shall • be constructed using methods and. practices that minimize flood damage. . (3) Electrical, heating, ventilation, plumbing, and air conditioning equipment :an.d other service, facilities -shall be designed and/or otherwise, elevated or located so as to prevent water from entering or accumulating within the components during conditions of flooding. 13.255 Utilities and- Services. (1) All new and replacement water supply systems.shall be-.- ; designed.to minimize or eliminate infiltration of floodwaters into the system; . . (.2) New and replacement sanitary sewage, systems shall be designed to minimize or eliminate infiltration of floodwaters into the systems and discharge from the . systems into floodwaters; . - (3) On-site waste disposal systems shall be located to avoid impairment to them or contamination from them during flooding consistent with the requirements of the Oregon Department of Environmental Quality; 13.256 Subdivision and Development Proposals, Partitions, and Planned Unit Developments. No proposed subdivision or partition of land or planned unit development plan, or other development located within an area of special flood hazard shall be approved without meeting the requirements of this article. All of the applicable mapping and certification requirement's of this article shall be met at the Tentative. Map, Plat or Plan stage of review for subdivisions, partitions, and planned unit developments (See also Article 17, Lots and Creation of Lots, and Article 18, Planned Unit Development.) (1) All development proposals, including subdivision proposals, shall be consistent with the need to minimize flood damage; (2) All development proposals, including subdivision proposals, shall have public utilities and facilities such as sewer, gas, electrical, and water systems located and constructed to minimize or eliminate flood damage; (3) All development proposals, including subdivision proposals, shall have adequate drainage provided to reduce exposure to flood damage; and (4) Where base flood elevation data has not been provided or is not available from another authoritative source, it shall be generated for development.proposals, including subdivision proposals, which have the potential for 5 dwelling units or more or contain 1 acre or more, whichever is less. 13.257 Review Where Elevation Data Not Available. Where elevation data is not available through the Flood Insurance Study FIRM, or another authoritative source, applications for building permits shall be reviewed to assure that proposed construction will be reasonably safe from flooding. The test of reasonableness is a local judgment and includes use of historical data, high water marks, photographs of past flooding, etc.., where available; Failure to elevate the lowest floor at least two feet above grade in these zones may result in higher insurance rates. 13.260 Specific Standards. In all areas of special flood hazards where base flood elevation data has been- provided (Zones Al-30, AH, and AE) as set forth in Section 13.232 (Basis for Establishing the Areas of Special Flood Hazard) or Section 13.245(2) (Use of Other Base Flood Data), the following provisions are required. 13.261 ,Residential Construction. (1) . New construction and substantial improvement of any residential structure shall have the lowest floor, including basement, elevated to a minimum of one foot above the base flood elevation. (2) Fully enclosed areas below the lowest floor that are subject to flooding are -prohibited, or shall be designed to automatically equalize hydrostatic flood forces on exterior walls by allowing for the entry and exit of floodwaters. Designs for meeting this requirement must either be certified by a registered professional engineer or architect or must meet or exceed the following minimum criteria: ; (a). A minimum of two openings having a total net area of not less than one square inch for every square foot of enclosed area subject to flooding shall provided. (b) The bottom of all openings shall be no higher than one foot.aboye grade. , (c) Openings may be equipped with screens, louverg, or other coverings or devices provided that they permit the automatic entry and exit of floodwaters. 13,2.62 Non-Residential Construction.. (1) New construction and substantial improvement of any commercial, industrial or other non-residential structure : . .shall either have the lowest floor, including, basement, elevated to a minimum of one foot above the.base flood /elevation; or, together with attendaint utility and • sanitary -facilities, shall: - (a) Be floodproofed so that the. structure is watertight. 'with walls substantially impermeable to the passage of. water to a level of one foot above, the base flood elevation; (b) Have structural components capable of resisting hydrostatic and hydrodynamic loads and effects of buoyancy; and (c) Be certified by a registered professional engineer or architect that the design and methods of construction are in accordance with accepted standards of practice for meeting provisions of this section based on their development and/or review of the structural design, specifications and plans. Such certifications shall also provide that the provisions of 13,254 are satisfied. Such certifications shall be provided to the Director as set forth in Section 13.245(3)(b) . The certification by a registered professional engineer or architect shall specify that the floodproofed methods for any commercial or industrial structure are adequate to withstand the flood depths, pressures, velocities, impacts and uplift forces and other factors associated with the base flood. (2) Non-residential structures that are elevated, not floodproofed, must meet the same standards for space below the lowest floor as described in Section 13.261(2). (3) Applicants floodproofing non-residential buildings shall be notified that flood insurance premiums will be based on rates that are one foot below the floodproofed level (e.g. a building floodproofed to the base flood level will be rated as one foot below that level)'. 13,263 Manufactured Homes. (1) -All manufactured homes to be placed or substantially improved oh sites listed below shall be elevated on a permanent foundation such that the finished floor of the manufactured home is elevated to a minimum of 18 inches (46 cm) above the basé flood elevation and be securely anchored to an adequately designed foundation system to rèsist flotation, collapse, and lateral movement: • (NOTE: See 2.002 Oregon Manufactured Dwelling and Parks -Specialty Code., Chapter 3 Manufactured Dwelling . Installations and Chapter 10 Manufactured Dwelling Park • Construction. That code also includes the following provisions: 3-2.4.1. (b) 1 requires that the top of the dwelling stand be at least one foot above base flood elevation unless openings are provided per FEMA Technical • Bulletin 1-93. 10-2/2(d) specifies that manufactured dwelling parks or park expansions shall not be permitted in a flood hazard area unless the stands are elevated above the base flood elevation). (a) Outside of a manufactured home park or manufactured home subdivision; (b) In a new manufactured home park or manufactured home subdivision; (c) In an expansion to an existing manufactured home park or manufactured home subdivision; (d) In an existing manufactured home park or manufactured home subdivision on which a manufactured home has incurred "substantial damage" as the result of a- flood. (2) Manufactured homes to be placed or substantially improved on sites in.an existing manufactured home park or manufactured home subdivision within Zones Al-30, AH, and AE on the community's FIRM that are not Subject to the above manufactured home provisions shall be elevated so that either: (a) The finished floor of the manufactured home is elevated to a minimum of 18 inches (46 cm) above the base flood elevation; or (b) The manufactured home chassis is supported by reinforced piers or other foundation elements of at least equivalent strength that are no less than 36 inches in.height above grade.and be securely anchored to an adequately designed foundation system to resist flotation, collapse, and lateral movement. 13.264 • Recreational Vehicles.» Any recreational vehicle placed on a site within Zones Al-30AH, AE shall either: (1) be on the. site for fewer than 180 consecutive days; (2) be fully licensed and ready for highway use,, on its . wheels or jacking.system, attached to.the site only by quick disconnect type utilities and security devices,. . with no permanently attached .additions; . (3) . meet the requirements of 12=. 263 above and the elevation and anchoring requirements for manufactured homes; or (4) be stored within a fully enclosed building that is floodproofed or elevated in.accordance with the requirements of Section 13.262. Nothing in tne Sect ion is intended to authorize the use of a recreational vehicle in a manner otherwise prohibited by this Code or other laws. 13.2 65 Crawlspaces and Below-Grade Crawlspaces. At-grade crawlspaces are the preferred method of crawlspace construction within flood hazard areas. However, below- grade crawlspaces are permitted, and are not considered basements, if all of the following are satisfied. See Figures 13-1, 13-2 and 13-3. Otherwise, below-grade crawlspaces are considered basements and subject to applicable requirements for basements. A basement floor is considered the lowest floor (see definition) and must meet requirements for the lowest floor. (1) Except as provided in this paragraph, because of hydrodynamic loads, the velocity of floodwaters at the site shall not exceed.5 feet per second where a below- grade crawlspace is used. For velocities in excess of 5 feet per second, other foundation types shall be used, or the design shall be approved and stamped by a qualified registered architect or professional engineer. . Other types of foundations are recommended for these areas. The determination of velocity shall be- based on the mean floodway velocity in Table 6 of the Flood Insurance Study for Josephine County and Incorporated Areas with a December 3, 2:009 effective date where that information is available. In areas where the mean floodway velocity may exceed 5 feet per second and flood velocity information is not available, such as for-the floodway fringe, flood Velocity at the building site shall be determined by an engineer knowledgeable in hydraulics and hydrology who is qualified to determine flood-velocities at the building Site, unless the Building Official determines flood •velocities at the. building site do not exceed 5 feet per second based on accepted practices or presumptive determinations in accordance with NFIP standards. (2) .The building must be designed and adequately anchored to resist or eliminate flotation, collapse, and lateral movement of the structure resulting from hydrodynamic and hydrostatic loads, including the effects of buoyancy. Hydrostatic loads and. the effects of buoyancy can usually be addressed through the required openings described in Subsection (3) of this Section. \ {3) Below-graae crawlspaces (and other crawlspaces designs) are enclosed areas below the base flood elevation (BFE) and, as such, must have openings that equalize hydrostatic pressures by allowing the automatic entry and exit of floodwaters. The bottom of each flood vent opening shall be no more than 1 foot above the lowest adjacent exterior grade. ( 4 ) For all crawlspaces, portions of the building below base flood elevation shall be constructed with materials resistant to flood damage. This includes not only the foundation walls of the crawlspace used to elevate the building, but also, any joists, insulation,, or other materials that are below the base flood elevation. If flood-resistant materials are not used for building elements, those- elements shall be elevated -above base flood elevation. The recommended construction practice is to elevate the bottom of joists and all insulation at least one foot above base flood elevation. Most types of insulation are not flood-resistant materials. Flood-resistant materials shall be determined and where used, shall be in accordance with FEMA Technical Bulletin 2, Flood Damage-Resistant Materials Requirements, August 2008, or as revised. (5) Any building utility systems within a crawlspace shall be elevated above BFE or.designed so that floodwaters cannot enter or accumulate within, the system components during flood conditions. Ductwork, in particular,- must either be placed above the base flood elevation or sealed from floodwaters. FEMA Bulletin 34 8, Protecting Building Utilities from Flood Damage, provides detailed guidance on designing and constructing, flood-res is tarit utility systems.. . (NOTE:. Section R324.1.5 of the residential "Building Code also addresses mechanical and electrical systems.. Section 7 and. Table 7-1 of. AS CE Standard 24-05, Flood Resistant Design and Construction, also address utility .requirements and may include requirement for elevation" higher than base flood elevation for certain situations). (6) The interior" grade of a below-grade crawlspace below.the base flood elevation shall not be more than 2 feet below thé., lowest adjacent exterior grade as shown in Figure 13- 3. (7) The height of a below-grade crawlspace,. measured from the . interior grade of the crawlspace to the top of the crawlspace foundation wall shall not exceed 4 feet at any point as shown in Figure 13-3. The'height limitation is the maximum allowable unsupported wall height according to the engineering analyses and building code requirements for flood hazard areas. (8) The drainage system shall be designed to remove floodwaters from the interior area of the crawl-space in a maximum time of 72 hours. The type of drainage system will vary because of the site gradient and other drainage characteristics, such as soil types. Options include, but are not limited to, natural drainage through porous, well-drained soils, drainage systems such as perforated pipes, drainage tiles, or gravel or crushed stone .... drainage., by .gravity, ox., mechanical ..means . The drainage, system shall be a system approved by the Building Official or shall be designed and stamped by the applicant's engineer. (NOTE: Buildings that have below-grade craw I.spaces will have higher flood insurance premiums, than buildings that have the preferred crawlspace construction with the interior elevation at or above the lowest adjacent grade, even when the ..crawlspace meets the requirements of this section and FEMA Technical Bulletin 11-01. Buildings with below-grade "crawlspac.es currently cannot be rated by an insurance agent .using the NFIP Flood Insurance Manual. They must be submitted for a:special rating under the "Submit-to-Rate" process by underwriters knowledgeable in this type: of construction) . Figure 13-1. Preferred Crawlspace Construction Figure 1^-2. Below-Grade Crawlspace Construction Figure 13-3. Requirements for Below-Grade Crawlspace Construction Roar Joist L = 4ft Maximum- D'= 2 ft'Maximum Crawlspace Interior Grade 7 — W r r ^ T T ïp: -Lowest Floor f Foot Above BFE .Portions of BuMng/Ulililies Below BFE Shall Be Resistant io Flood Damage/Sealed frani FtoOdwatera - Foundation Wall -Flood Vent Lowest Adjacent Exterior Grade (LAG) i 'f 13.270-• Floodways. Located within, areas of special flood hazard are areas designated as .floodways. Since the floodway is an extremely hazardous area due to the velocity, of floodwaters which- carry debris, potential projectiles, and erosion potential, the - provisions of this Section apply. 13;271 Designated Floodways. (1) Except as.provided in Section. (3) below, encroachment, •..fill, new construction, substantial improvements or other development shall not occur within a floodway designated by Flood Insurance Study or Flood Insurance1 Rate Maps unless a tecnnical evaluation is performed and certified by a registered professional civil engineer, and demonstrates through hydrologie and hydraulic analysis performed in accordance with standard engineering practice that encroachments, including any surrounding property modifications or improvements, shall not result in any increase in flood levels during the occurrence of the base flood discharge. (2 ) If subsection fl) is satisfied, all new construction and substantial improvements shall comply with all applicable flood hazard reduction provisions of this code. (3) Projects for stream habitat restoration may be permitted in the floodway provided: (a) The project qualifies for a Department of the Army, - Portland District Regional General Permit for Stream Habitat Restoration (NWP-2007-1023); and (b) A qualified professional (a Registered Professional Engineer-; or staff of NRCS ; the county, or fisheries, natural resources, or water resources agencies) has provided a feasibility analysis and certification that the project was designed to keep any rise in 100-year flood level as close to zero as practically possible given the goals of the project; -and (c) No structures would be impacted by a potential rise in flood elevation; and (d) An agreement to monitor the project, correct problems, and ensure that flood carrying capacity remains unchanged is included as part of the local approval. (-4) New installation of manufactured dwellings is prohibited, except as provided in this Section (as regulated by the 2002 Oregon Manufactured Dwelling and Park Specialty Code). Manufactured dwellings may only be located in floodways according tb one of the following conditions : (a) If the manufactured dwelling.already exists in the floodway,. the placement" was permitted at the time of the original installation, and the continued use is not a threat to life, health, property, or thé general welfare of the public; or (b) A new manufactured dwelling is replacing an.existing manufactured dwelling whose original placement was permitted at the time of installation and the replacement home will not be a threat to life, health, property, or the general welfare of the public, and it meets the following criteria: (i) As required by 44 CFR Chapter 1, Subpart 60.3(d)(3), it must be demonstrated through hydrologie and hydraulic analyses performed in accordance with standard engineering practices that the manufactured dwelling and any accessory buildings, accessory structures, or any property improvements (encroachments) will not result in any increase' in flood levels during the occurrence of the base flood elevation; (ii) The replacement manufactured dwelling and any accessory buildings or accessory structures- (encroachments) shall have the finished floor elevated a minimum of 18 inches (46 cm) above the base flood elevation as identified on the Flood Insurance Rate Map; (iii)The replacement manufactured dwelling is placed and secured to a foundation support system designed by an Oregon professional engineer or architect and approved by the Community Development Department; (iv) The replacement manufactured dwelling, its foundation supports, and any accessory buildings, accessory structures, or property improvements (encroachments) do not displace water to the degree that it causes a rise in the water level or diverts water in a manner that causes erosion or damage.to other properties; (v) The location, use,, and improvements of a replacement manufactured dwelling complies with all provisions of this Code, other applicable Codes, and any conditions of approval; and 13.272 Floôdways Not Designated. (1) In areas where a regulatory floodway has not- been designated in the Flood Insurance Study or on the Flood. Insurance Raté Maps, no new construction, substantial improvements, or other development (including fill) shall be permitted within Zones Al-30 and AE on the Flood Insurance Rate.Map, unless it is demonstrated that the cumulative effect of the proposed development, when combined with all other existing and anticipated development, will not increase the water surface elevation of the base flood more than one foot at any point within the community. (2) Development shall not occur on any floodplain lands, where a floodway has not been designated for that reach of. a stream or river in the Flood Insurance Study referenced in Section 13.232 of this Code unless: (a) The Director has evidence which in his judgment would indicate the proposed development site is located in an area of shallow flooding, and the proposed development complies- with the provisions of Section 13.280 and will not divert the flood or cause a rise in the level of the discharge above the base flood elevation; or (b) A technical study is completed which establishes the probable location of the floodway as defined in this Code, and the proposed development complies with the applicable provisions of this Code', whether it is within the floodway or the floodway. fringe. (3) If a technical study is completed under the requirements of this section, demonstrating that the encroachment will not increase the. flood levels, any permitted construction or substantial improvements shall comply with all other applicable standards of this Code. 13.280 Standards for Shallow Flooding Areas (AO Zones). Shallow flooding areas appear on Flood Insurance Rate Maps as AO zones with depth designations. The base flood depths in these ones range from 1 to 3 feet above ground where a clearly defined channel does not exist, or where the path of flooding is unpredictable and where velocity flow may be evident. Such flooding is usual 1y characterized as sheet flow. In these areas, the following provisions apply: . (1) Residential Structures. New construction and substantial improvements of residential structures and manufactured homes within AO zones shall have the lowest floor. (Including basement) elevated above the highest grade adjacent to the building, a minimum of one foot above the depth number specified on the Flood Insurance Rate Map, or at least two feet above the highest grade adjacent.to the building if no depth number is specified. (2) Nonresidential Structures. New construction and substantial improvements of nonresidential structures within AO zones shall either: (a) Have the lowest floor (including basement) eLevated above the highest adjacent grade of the building site, a minimum of one foot above the depth number specified on the Flood Insurance Rate Map, or at least two feet above the highest grade adj acent to the building if no depth number is specified; or (b) Together with attendant utility and sanitary facilities-, be completely floodproofed to a minimum of one foot above the depth number specified on the Flood Insurance Rate Map, or at least two feet above the highest grade adj acent to the building if no depth number is specified, so that any space below that-level is .watertight with walls substantially impermeable to the passage of water and with structural components having the capability of resisting hydrostatic and hydrodynamic loads and effects of buoyancy. If this method is used, . compliance shall be certified by a registered professional engineer or architect as in Section -. 13.26,2. 13.290 Critical Facilities and Essential Facilities 13.291 Critical Facilities. (1) It is recommended that construction of new critical facilities is/ to the extent possible, located outside the limits of the Special Flood. Hazard Area. (SFHA) also known as the 100-year floodplain, (2) It is recommended that construction of new critical facilities occur within the SFHA only if no feasible alternative site is' available. (3) The following are .recommended when .Critical Facilities are constructed within-the SFHA'.. . Recommendaitions in this Section do not affect other mandatory.provisions of this Code or other .applicable codes. . (a) It. is recommended that Critical. Facilities cpnstructed; within-the SFHA have.the ;lowest floor . , elevated a minimum of three feet or to the height of ..the of the 500-year, flood, whichever is higher. (b) It is recommended that access to and. from the critical facility should also be protected to the height utilized above. When, those heights are not feasible, .it is at least -recommended that access routes, be .elevated to .or.above the' level grewe okay with just doing that much? [He was advised that it was all right, off microphone.] ! 7 City Council Meeting November 4, 2009 6. EXECUTIVE SESSION 192.660 (2)(h): To consult with counsel concerning the legal rights and duties oTsa public body with regard to current litigation or litigation likely to be filed. MOTION It was moved by Cotmcilor Ren fro and seconded by Councilor Gatlin to go into executive session. The vote resulted asfollows: Renfro, Cummings, Michelon, Wheatley, Hitchcock, Gatlin, Boston and Webber. "NAYS": Nhne. Abstain: None. Absent: None. The motion has passed. Interim City Attorney Bartholomew statecvthe Council will now meet in executive session for the purpose of discussing those subjects previously noticefckfar this session. This executive session is held pursuant to ORS 192.660, and more specifically, under the sebtjons of that statute which had been publically noticed for this meeting. Representatives of the news media ar^ d designated Staff are allowed to attend the executive session. All other members of the audience arenasked to leave the room. Representatives of the news media are specifically directed not to report on any oi^he deliberations during the executive session, except to state the general subject of the session as previously announced. No decision making will be made in executive session. At the end of executive session, we^will return to open session and welcome the audience back into the room. MOTION It was moved by Councilor Gatlin and seconded by Councilor Renfro to^go out of executive session. The vote resulted as follows: Renfro, Cummings, Michelon, Wt^ eatley, Hitchcock, Gatlin, Boston and Webber. "NAYS": None. Abstain: None. Absent: Nbue. The motion has passed. 7. ADJOURN: There being no further business to come before the Council, Mayor Murphy adjourned the meeting at 8:30 p.m The ordinances, resolutions, and motions contained herein and the accompanying votes have been verified by: Finance Director These minutes were prepared by contracted minute taker, Wendy Hain. City Council Meeting November 4, 2009 35 I fe ET E? Ü H-L • Cfl r> CO C« t—>-• o 2 3 o o o> i-t H o B CA) o ë o l-t ^ O n P O o Ht a oo Ci C GO GO h- O VJ n O P T J O o C/3 EXHIBIT 73 / V w t r i O P O OP ET p ^ P - O F-y S Z O» n> > i-fc o p p co P h-1 p-» P ft) a . en e <1 ft) •"Ö m m P O O P n n> 3 3 . p fD ft cf rt en P CD CO rt P n p p P-n> •S p r-t m ^ T3 m O m o r-f O 3 m en O O al S 3 çiu m co p p p SO p p et. g s E M ft flu 01 O P n O-m n O 3 o p M a . & o o p o . rï & O t r ÊT n> y ^ 9 SS I p 05 n> * g Cu ß O S P! i-t m n 0 1 B" I O i-h B- S S 8 m m m É2. O-n> P rf tf. p 0 1 t-t B Z l r j i— • t i C/Ì B 4 » o o p ¡3 H r+ o - o p ct. o ¡3 t t í rt> D rt> t h r+ C/5 O o D C/5 0> HO £ 0> D o o> C/Î •j H O 2 Z o s td r ™ w TJ S o • o s. O £ W rD £ rD Ö ) C/3 n o £ C/3 rD rD £ o rD co 8 S ö 5 r-h P . O t—i- • n j P Ht. O D W ro D ro t=h C/3 O o P C/3 ro o> o a C/3 fl> ti. D Ü j ü O K ft ¿L S V g p K" n Ui R=> pt. O p B ^ B" « s •-»• O ^ g- Ui cw ^ B-vo n> O B ÊL O) C^ rt-ET B-O M n> o il ^ h r+ H * S, « O 3 2 o H S n> p . D ß £ I g" n p O n a ft en i l o tf. O § o 3 B s l-rí Sû fr p p P-* s fil o o o o p- p ft ra G 5" 8 Tí n Ci- ni s « P I S* B co p >-d Ê 0 K S ^ O S Tí O £ p m << Ö B. i § ? O P-* fe* Tí P-* er I Cu ft> m p.* ET n a> CITY OF GRANTS PASS COMMUNITY DEVELOPMENT DEPARTMENT FLOOD HAZARD DISTRICT ZONING MAP AMENDMENT, SPECIAL PURPOSE DISTRICT MAP AMENDMENT AND DEVELOPMENT CODE TEXT AMENDMENT STAFF REPORT - CITY COUNCIL Procedure Type: Type IV: Planning Commission Recommendation and City Council Decision Project Number: 09-40500004 & 09-40500006 Project Type: Zoning Map Amendment, Special Purpose District Map Amendment and Development Code Text Amendment Applicant: City of Grants Pass Planner Assigned: Lora Glover Application Received: July 17, 2009 Application Complete: July 24, 2009 Date of Staff Report: September 14, 2009 Date of UAPC Hrng: September 23, 2009 Date UAPC Findings of Fact Signed: October 14, 2009 Date of City Council Hearing: November 4, 2009 I. PROPOSAL: The proposal includes the following: 1) Amend the Special Purpose District Map for.the Flood Hazard District by adopting the current Flood Insurance Study (FIS) Volumes 1 and 2 and Flood Insurance Rate Maps (FIRM) for Josephine County, Oregon and Incorporated areas effective date December 3, 2009, issued by the Department of Homeland Security's Federal Emergency Management Agency (FEMA). 2) Amend Section 13.200 (Flood Hazard District) of the City of Grants Pass Development Code to be consistent with the National Flood Insurance Program (NFIP) and Oregon Model Code Provisions. 3) Update Element 5 of the Comprehensive Plan, specifically the section under Flood Hazard (5.3Ó) to reference the new FIS and FIRM effective December 3, 2009. The revision is a modification to the narrative of the Comprehensive Plan and the change is reviewed as a minor amendment to the database in accordance with Section 13.5.2 of the Comprehensive Community Development Plan Policies document. No criteria are reviewed with the narrative change. 09-40500004 & 09-40500006 ~ Flood Hazard District Zoning Map Amendment, Special Purpose District Map Amendment, and Development Text Amendment City Council - Staff Report Page 1 o f 4 75 W 4) The adopting ordinance for City Council adoption will repeal any conflicting or duplicate provisions contained in the Municipal Code related to flood hazard provisions. II. AUTHORITY AND CRITERIA: Sections 4.032, 4.042 and 4.102 of the City of Grants Pass Development Code provide the procedures for initiation of a Special Purpose District Map Amendment and Development Code Text Amendment. The proposed Special Purpose District Map Amendment and Development Code Text Amendment were initiated by the Community Development Director. Sections 2.060, 7.040 and 7.050 authorize the Urban Area Planning Commission to make a recommendation to the City Council and authorize the City Council to make a final decision on a land use matter requiring a Type IV procedure, in accordance with procedures of Section 2.060. The applicable criteria from the Development Code to be met include the following: • Section 4.033 -Zoning Map Amendment Section 4.044 — Special Purpose District Amendment • Section 4.103 - Development Code Text Amendment III. APPEAL PROCEDURE: The City Council's final decision may be appealed to the State Land Use Board of Appeals (LUBA) as provided in state statutes. A notice of intent to appeal must be filed with LUBA within twentyrone (21) days of the Council's written decision. IV. BACKGROUND AND DISCUSSION: Detailed background and discussion are provided in the Planning Commission's Findings of Fact. The Planning Commission recommends the City Council approve the proposed amendments. V. CONFORMANCE WITH APPLICABLE CRITERIA: The Planning Commission found that the request was in conformance with the criteria contained in Section 13.5.2 of the Comprehensive Community Development Plan Policies and the criteria contained in Sections 4.033, 4.044 & 4.103 of the Development Code. VI. RECOMMENDATION: The Urban Area Planning Commission found that the request meets the criteria contained in Section. 13.5.2 of the Comprehensive Community Development Plan Policies and the criteria contained in Sections 4.033, 4.044 & 4.103 of the Development Code, and recommends the City Council: 09-40500004 & 09-40500006-Flood Hazard District Page 2 of 4 Zoning Map Amendment, Special Purpose District Map Amendment, and Development Text Amendment City Council - Staff Report 1. Approve the amendment of the Special Purpose District Map for the Flood Hazard District by adopting the current Flood Insurance Study (FIS) Volumes 1 and 2 and Flood Insurance Rate Maps (FIRM) for Josephine County, Oregon and Incorporated areas effective date December 3, 2009, issued by the Department of Homeland Security's Federal Emergency Management Agency (FEMA); 2. Approve the amendment to Section 13.200 (Flood Hazard District) of the City of Grants Pass Development Code to be consistent with the National Flood Insurance Program (NFIP) and Oregon Model Code Provisions; and 3. Approve the amendment to update Element 5 of the Comprehensive Plan, specifically the section under Flood Hazard (5.30) to reference the new FIS and FIRM effective December 3, 2009. VII. CITY COUNCIL ACTION: A. Positive Action: 1. Approve the proposal as recommended. 2. Approve the proposal with revisions (list): B. Negative Action: deny the request and adopt no amendments for the following reasons (list): C. Postponement: Continue item 1. Indefinitely. 2. To a date and time certain. VIII. INDEX TO EXHIBITS: 1. Planning Commission's Findings of Fact and the Attached Record. Index to Exhibits: A. UAPC Staff Report: 1. Flood Insurance Study (FIS) for Josephine County, Oregon and Incorporated areas, dated December 3, 2009 (full report is available in the Planning file). 2. Flood Insurance Rate Maps (FIRM) dated December 3, 2009 (full set of maps is available in the Community Development office). 3. Revised Section 13.200 ~ Flood Hazard District Development Code. 09-40500004 & 09-40500006 ~ Flood Hazard District Page 3 of 4 Zoning Map Amendment, Special Purpose District Map Amendment, and Development Text Amendment City Council - Staff Report 4. Revised Element 5, Section 5.30, Flood Hazard located in the Comprehensive Plan. 5. FEMA's "Letter of Final Determination" dated June 3, 2009. B. Minutes from September 23. 2009. UAPC hearing C. PowerPoint Presentation 2. Revised Title 9 of the Municipal Code (fulf text is available in the Planning file). 3. Letter of concern received from Sandra Loghry, dated 11/03/09. 4. Letter of concern received from Nadine Ham, dated 11/04/09. NOTE: The application is not subject to the 120 day requirement per ORS 227.178. 09-40500004 & 09-40500006 ~ Flood Hazard District Page 4 of 4 Zoning Map Amendment, Special Purpose District Map Amendment, and Development Text Amendment City Council - Staff Report CITY OF GRANTS PASS COMMUNITY DEVELOPMENT DEPARTMENT FLOOD HAZARD DISTRICT ZONING MAP AMENDMENT, SPECIAL PURPOSE DISTRICT MAP AMENDMENT AND DEVELOPMENT CODE TEXT AMENDMENT FINDINGS OF FACT ~ URBAN AREA PLANNING COMMISSION Procedure Type: Type IV: Planning Commission Recommendation and City Council Decision Project Number: 09-40500004 & 09-40500006 Project Type: Zoning Map Amendment, Special Purpose District Map Amendment and Development Code Text Amendment Applicant: City of Grants Pass Planner Assigned: Lora Glover Application Received: July 17, 2009 Application Complete: July 24, 2009 Date of Staff Report: September 14, 2009 Date of UAPC Hrng: September 23, 2009 Date Findings of Fact Signed: October 14, 2009 I. PROPOSAL: The proposal includes the following: 1) Amend the Special Purpose District Map for the Flood Hazard District by adopting the current Flood Insurance Study (FIS) Volumes 1 and 2 and Flood Insurance Rate Maps (FIRM) for Josephine County, Oregon and incorporated areas effective date December 3, 2009, issued by the Department of Homeland Security's Federal Emergency Management Agency (FEMA). 2) Amend Section 13.200 (Flood Hazard District) of the City of Grants Pass Development Code to be consistent with the National Flood Insurance Program (NFIP) and Oregon Model Code Provisions. 3) Update Element 5 of the Comprehensive Plan, specifically the section under Flood Hazard (5.30) to reference the new FIS and FIRM effective December 3, 2009. The revision is a modification to the narrative of the Comprehensive Plan and the change is reviewed as a minor amendment to the database in accordance with Section 13.5.2 of the Comprehensive Community Development Plan Policies document. No criteria are reviewed with the narrative change. 4) The adopting ordinance for City Council adoption will repeal any conflicting or duplicate provisions contained in the Municipal Code related to flood hazard provisions. 09-40500004 & 09-40500006 ~ Flood Hazard District Zoning Map Amendment, Special Purpose District Map Amendment, and Development Text Amendment UAPC - Findings of Fact Page 1 of 11 EXHIBIT I to ôc srm= HEfmr II. AUTHORITY AND CRITERIA: Sections 4.032, 4.042 and 4.102 of the City of Grants Pass Development Code provide the procedures for initiation of a Special Purpose District Map Amendment and Development Code Text Amendment. The proposed Special Purpose District Map Amendment and Development Code Text Amendment were initiated by the Community Development Director. Sections 2.060, 7.040 and 7.050 authorize the Urban Area Planning Commission to make a recommendation to the City Council and authorize the City Council to make a final decision on a land use matter requiring a Type IV procedure, in accordance with procedures of Section 2.060. The applicable criteria from the Development Code to be met include the following: • Section 4.033 -Zoning Map Amendment • Section 4.044 - Special Purpose District Amendment • Section 4.103 - Development Code Text Amendment III. APPEAL PROCEDURE: The City Council's final decision may be appealed to the State Land Use Board of Appeals (LUBA) as provided in state statutes. A notice of intent to appeal must be filed with LUBA within twenty-one (21) days of the Council's written decision. IV. PROCEDURE: A. An application for a Comprehensive Plan Amendment, Flood Hazard District Zoning Map Amendment, Special Purpose District Map Amendment and Development Code Text Amendment was submitted and deemed complete on July 17, 2009. The application processed in accordance with Section 2.060 of the Development Code, and Sections III and V of the 1998 Intergovernmental Agreement. B. Notice of the proposed amendment was mailed to the Oregon Department of Land Conservation and Development (DLCD) on July 17, 2009, in accordance with ORS 197.610 and OAR Chapter 660-Division 18. C. Notice of the proposed amendment was mailed to Josephine County on July 17, 2009, in accordance with the 1998 Intergovernmental Agreement. D. Notice of the September 23, 2009, Planning Commission hearing was mailed to potentially interested parties on September 3, 2009. 09-40500004 & 09-40500006 - Flood Hazard District Page 2 of 11 Zoning Map Amendment, Special Purpose District Map Amendment, and Development Text Amendment UAPC - Findings of Fact E. Public notice of the September 23, 2009, Planning Commission hearing was published in the newspaper on September 19, 2009, in accordance with Sections 2.053 and 2.063 of the Development Code. F. A public hearing was held by the Planning Commission on September 23, 2009, to consider the proposal and make a recommendation to City Council. V. SUMMARY OF EVIDENCE: A. The basic facts and criteria regarding this application are contained in the staff report, which is attached as Exhibit "A" and incorporated herein. B. The minutes of the September 23, 2009, Urban Area Planning Commission public hearing are attached as Exhibit "B" and incorporated herein. C. The PowerPoint Presentation given by staff at the September 23, 2009, public hearing is attached as Exhibit "C" and incorporated herein. VI. FINDINGS: The Urban Area Planning Commission found that the request meets the criteria contained in Section 13.5.2 of the Comprehensive Community Development Plan Policies and the criteria contained in Sections 4.033, 4.044 & 4.103 of the Development Code based on the reasons stated in the findings below. The vote was 7-0-0, with Commissioners Berlant, Kellenbeck, Arthur, Fowler, Fitzgerald, Fedosky and Richardson in favor. (Note: There is currently one vacancy on the commission.) VII. GENERAL FINDINGS OF FACT - BACKGROUND AND DISCUSSION: The City of Grants Pass participates in the National Flood Insurance Program (NFIP). By having ordinances that comply with the NFIP, residents are eligible to obtain flood insurance through the program. FEMA has recently completed the process of updating the Flood Insurance Study (FIS) and Flood insurance Rate Maps (FIRMs) throughout the country and state, including Josephine County. Both the City of Grants Pass and Josephine County will be adopting the complete FIS and all of the FIRM maps covering Josephine County and the incorporated areas. By doing so, there will not be a need to undertake an additional amendment in the event the Urban Growth Boundary is adjusted in the future. The purpose of the new FIS is to revise and update information on the existence and severity of flood hazards in the geographic area of Josephine County, to include the Cities of Cave Junction and Grants Pass. The original hydrologic and hydraulic analyses were performed by the U.S. Geological Survey (USGS), and completed in 09-40500004 & 09-40500006 ~ Flood Hazard District Page 3 of 11 Zoning Map Amendment, Special Purpose District Map Amendment, and Development Text Amendment UAPC - Findings of Fact 1979. The countywide updated was performed by WES i uonsultanis, inc., and was completed in October 2008. On June 3, 2009, FEMA mailed their "Letter of Final Determination" instructing the City that the new study and maps must be adopted by December 3, 2009, to maintain its participation in the flood insurance program. The FIS and FIRM maps currently in effect are dated September 27, 1991. The floodway boundary and floodway maps have been incorporated into the new FIRM maps. The existing FIS and FIRM maps will be maintained for historical reference. Failure to adopt the study and maps by December 3 means the City would be suspended from the flood insurance program effective on that date, leaving citizens at risk of flood damage that would not be covered by the National Flood Insurance Program. Adoption of the new FIS and FIRM maps requires that Element 5 of the Comprehensive Plan, specifically the section under Flood Hazard (5.30) be amended to reference the new FIS and FIRM effective December 3, 2009. The revision is a modification to the narrative of the Comprehensive Plan and the change is reviewed as a minor amendment to the database in accordance with Section 13.5.2 of the Comprehensive Community Development Plan Policies document. No criteria are reviewed with the narrative change. In addition to adopting the new FIS and FIRMs, FEMA's "Letter of Final Determination" states additional requirements must be met under Section 1361 of the National Flood Insurance Act of 1968, as amended, within six (6) months of the date of their letter. Specifically, the standards of Paragraph 60.3(d) of the NFIP regulations must be met. The letter goes on to list the following actions in order to be in compliance: • Amend existing regulations to incorporate any additional requirements of Paragraph 60.3(d); • Adopt all standards of Paragraph 60.3(d) into one new, comprehensive set of regulations; or • Show evidence that regulations have previously been adopted that meet or exceed the minimum requirements. The "Letter of Final Determination" included a "Summary of Map Actions" documenting previous "Letter of Map Change (LOMC) actions (including Letters of Map Amendment and Letters of Map Revision) which will be superseded by the revised FIRM panels. Many property owners will find little change in the flood information for their property, while others will be required to meet the new elevation requirements for all new structures and substantial improvements to existing structures. An example of the existing and amended maps is provided: 09-40500004 & 09-40500006 ~ Flood Hazard District Page 4 of 11 Zoning Map Amendment, Special Purpose District Map Amendment, and Development Text Amendment UAPC - Findings of Fact EXISTING FLOOD MAPS A 09-40500004 & 09-40500006 ~ Flood Hazard District Page 5 of 11 Zoning Map Amendment, Special Purpose District Map Amendment, and Development Text Amendment UAPC - Findings of Fact 09-40500004 & 09-40500006 ~ Flood Hazard District Page 6 of 11 Zoning Map Amendment, Special Purpose District Map Amendment, and Development Text Amendment UAPC - Findings of Fact The summary notes one LOMC for 643/645 SW Balsam Drive, Grants Pass, Oregon, which will be superseded by new detailed flood hazard information based upon revised hydrologic and hydraulic analyses. The property owners were mailed a separate notice concerning the revised FIRMs, but they have not responded as of the date of this report. The existing regulations in Article 13 of the Development Code have been reviewed against Paragraph 60.3 (d) and the State's Model Flood Plain Ordinance for consistency. The additions and changes to Section 13.200 are reflective of the regulations from the above documents. The Municipal Code also includes flood hazard regulations. All flood hazard provisions have been incorporated into Section 13.200 of the Development Code. The final ordinance for approval by the City Council will repeal any old ordinances and existing language that has been incorporated into the Development Code. VIII. FINDINGS OF FACT - CONFORMANCE WITH APPLICABLE CRITERIA ~ SECTION 4.033 OF THE DEVELOPMENT CODE Criteria for Amendment. The Zoning Map may be amended by the review bodies provided that all the following criteria are met: (1) The proposed use, if any, is consistent with the proposed Zoning District. (2) The proposed Zoning District is consistent with the Comprehensive Pian Land Use Map designation. (3) A demonstration that existing or proposed levels of basic urban services can accommodate the proposed or potential development without adverse impact upon the affected service area or without a change to adopted utility plans. (4) A demonstration that the proposed amendment is consistent with the functions, capacities and performance standards of transportation facilities identified in the Master Transportation Plan. (5) The natural features of the site are conducive to the proposed Zoning District. (6) The proposed zone is consistent with the requirements of all overlay Districts that include the subject property. (7) The timing of the zone change request is appropriate in terms of the efficient provision or upgrading of basic urban services versus the utilization of other buildable lands in similar zoning districts already provided with basic urban services. (8) In the case of rezoning from the Urban Reserve District, that the criteria for conversion are met, as provided in Section 4.034. 09-40500004 & 09-40500006 ~ Flood Hazard District Page 7 of 11 Zoning Map Amendment, Special Purpose District Map Amendment, and Development Text Amendment UAPC - Findings of Fact Planning Commission Response: Not Applicable. Although the proposed amendments do noi related to zoning, it was found that review and acknowledgement of the criteria was important. The adoption of the new FIS and FIRM will result in a map change to the flood hazard, one of the special purpose districts regulated by the City of Grants Pass. The amendment affects properties along the Rogue River and Gilbert Creek. However, the above listed criteria are found not applicable to the amendment. IX. FINDINGS OF FACT - CONFORMANCE WITH APPLICABLE CRITERIA ~ SECTION 4.044 OF THE DEVELOPMENT CODE (1) The Flood Hazard District map is the Flood Boundary - Floodway Map established by the Federal Emergency Management Agency (FEMA) in the scientific and engineering reports entitled "The Flood Insurance Study for the City of Grants Pass" and the "The Flood Insurance Study for the County of Josephine County, State of Oregon". The flood hazard district map may be amended only by FEMA in the procedure provided for Flood Boundaries - Floodway Maps. (2) Upon receipt of proper authorization from FEMA, the Director shall begin administering the revised Flood Hazard District, as designated by FEMA. Planning Commission Response: Satisfied. As noted above, on June 3, 2009, FEMA mailed their "Letter of Final Determination" instructing the City that the new FIS and FIRM maps must be adopted by December 3, 2009, to maintain its participation in the flood insurance program. Upon adoption, the updated FIS, FIRM and Section 13.200 of the Development Code, will be used to regulate properties in the flood hazard area. X. FINDINGS OF FACT - CONFORMANCE WITH APPLICABLE CRITERIA ~ SECTION 4.103 OF THE DEVELOPMENT CODE The text of the Development Code may be recommended for amendment and amended provided that all of the following criteria of Section 4.103 of the Development Code are met. CRITERION 1: The proposed amendment is consistent with the purpose of the subject section and article. Planning Commission Response: Satisfied. The proposal amends Section 13.200 "Flood Hazard District". The purpose statement of Section 13.210 states that the intent of the Flood Hazard District is to designate areas that may be hazardous to development due to flooding. The District is to provide standards that specify how development will minimize public and private losses due to flood conditions in specific areas by provisions designed to: 09-40500004 & 09-40500006 ~ Flood Hazard District Page 8 of 11 Zoning Map Amendment, Special Purpose District Map Amendment, and Development Text Amendment UAPC - Findings of Fact • Protect human life and health; • Minimize expenditure of public money; • Minimize need for rescue and relief efforts; • Minimize prolonged business interruptions; • Minimize damage to public facilities; • Help maintain a stable tax base; • Notify potential buyers of special flood hazard; and • Ensure those who occupy flood hazard areas accept responsibility for their actions. The proposed amendment is consistent with the purpose statement of Section 13.210 because it brings the Development Code into compliance with regulations of the National Flood Insurance Program (NFIP, Paragraph 60.3(d)) as required under Section 1361 of the National Flood Insurance Act of 1968, as amended. Specifically, the proposed text amendment will: • Consolidate various flood ordinances currently located within the Municipal Code, into one iocation in the Development Code; • Provide additional terms and definitions for the flood hazard district; and • Brings construction standards for crawlspaces and below-grade crawlspaces into compliance. CRITERION 2: The proposed amendment is consistent with other provisions of this code. Planning Commission Response: Satisfied. As noted under Section 13.010 of the Development Code, special purpose districts, to include the Flood Hazard District, provide standards intended to mitigate natural hazards, to protect natural features and to mitigate land use conflicts. The standards applicable for the Flood Hazard District are in addition to the standards of the underlying zoning district. Therefore, the proposed amendment is internally consistent with other provisions of the Development Code. CRITERION 3: The proposed amendment is consistent with the goals and policies of the Comprehensive Plan, and most effectively carries out those goals and policies of all alternatives considered. Planning Commission Response: Satisfied. The proposed amendment is consistent with the goals and policies of the Comprehensive Plan. Section 5.2 of Element 5 of the Comprehensive Plan Policy document states that the Development Code shall: 09-40500004 & 09-40500006 ~ Flood Hazard District Page 9 of 11 Zoning Map Amendment, Special Purpose District Map Amendment, and Development Text Amendment UAPC - Findings of Fact • Regulate development within the 100-yearfloodplain and floodway as required to maintain participation in the National Flood Insurance Program; • Provide methods to determine and appeal the location of the 100- year floodplain and floodway boundaries when there appears to be discrepancies between official mapped boundaries and actual field conditions. • Facilitate flood hazard policies. The proposed changes to Section 13.200 of the Development Code and the narrative of the Comprehensive Plan help implement the policy statements. As noted above, the narrative of Element 5 of the Comprehensive Plan (Section 5.30 ~ Flood Hazard) is being modified to reference the new FIS and FIRM effective December 3, 2009. The alternative of not adopting the new FIS, FIRM and Code sections is not a viable option as it would cause suspension with the City's participation in the NFIP. CRITERION 4: The proposed amendment is consistent with the functions, capacities, and performance standards of transportation facilities identified in the Master Transportation Plan. Planning Commission Response: Not Applicable. The proposed amendments do not pertain to the performance standards of the Master Transportation Plan. XI. RECOMMENDATION: A. The Urban Area Planning Commission recommends that City Council APPROVE the amendment of the Special Purpose District Map for the Flood Hazard District by adopting the current Flood Insurance Study (FIS) Volumes 1 and 2 and Flood Insurance Rate Maps (FIRM) for Josephine County, Oregon and Incorporated areas effective date December 3, 2009, issued by the Department of Homeland Security's Federal Emergency Management Agency (FEMA). B. The Urban Area Planning Commission recommends that City Council APPROVE the proposed amendment to Section 13.200 (Flood Hazard District) of the City of Grants Pass Development Code to be consistent with the National Flood Insurance Program (NFIP) and Oregon Model Code Provisions. C. The Urban Area Planning Commission recommends that City Council APPROVE the amendment to update Element 5 of the Comprehensive Plan, specifically the section under Flood Hazard (5.30) to reference the new FIS and FIRM effective December 3, 2009. 09-40500004 & 09-40500006 ~ Flood Hazard District Page 10 of 11 Zoning Map Amendment, Special Purpose District Map Amendment, and Development Text Amendment UAPC - Findings of Fact XII. APPROVED BY THE URBAN AREA PLANNING COMMISSION this 14,h day of October, 2009. Commissioner Gary Beriant, Chair NOTE: The application is not subject to the 120 day requirement per ORS 227.178. 09-40500004 & 09-40500006 ~ Flood Hazard District Page 11 of 11 Zoning Map Amendment, Special Purpose District Map Amendment, and Development Text Amendment UAPC - Findings of Fact CITY OF GRANTS PASS COMMUNITY DEVELOPMENT DEPARTMENT FLOOD HAZARD DISTRICT ZONING MAP AMENDMENT, SPECIAL PURPOSE DISTRICT MAP AMENDMENT AND DEVELOPMENT CODE TEXT AMENDMENT STAFF REPORT-URBAN AREA PLANNING COMMISSION Procedure Type: Type IV: Planning Commission Recommendation and City Council Decision Project Number: 09-40500004 & 09-40500006 Project Type: Zoning Map Amendment, Special Purpose District Map Amendment and Development Code Text Amendment Applicant: City of Grants Pass Planner Assigned: Lora Glover Application Received: July 17, 2009 Application Complete: July 24, 2009 Date of Staff Report: September 14, 2009 Date of UAPC Hrng: September 23, 2009 I. PROPOSAL: The proposal includes the following: 1) Amend the Special Purpose District Map for the Flood Hazard District by adopting the current Flood Insurance Study (FIS) Volumes 1 and 2 and Flood Insurance Rate Maps (FIRM) for Josephine County, Oregon and Incorporated areas effective date December 3, 2009, issued by the Department of Homeland Security's Federal Emergency Management Agency (FEMA). See Exhibit 1 for FIS and See Exhibits for FIRMs Note: FIS Volume 1 is attached in its .entirety; Volume 2 contains all the flood profiles . and is available at the Community Development office for review. 2). Amend Section 13.200 (Flood Hazard .District) of the City of Grants Pass Development Code to be consistent with the National Flood Insurance Program (NFIP) and Oregon Model Code Provisions. See Exhibit 3 3) Update Element 5 of the Comprehensive Plan, specifically the section under Flood Hazard (5.30) to reference the new FIS and FIRM.effective December 3, 2009. The revision is a modification to the narrative of the Comprehensive Plan and the change is reviewed as a minor amendment to the database in accordance with Section 13.5.2 of the Comprehensive Community Development Plan Policies document. No criteria are reviewed with the narrative change. See Exhibit 4 4) The adopting ordinance for City Council adoption will repeal any conflicting or duplicate provisions contained in the Municipal Code related to flood hazard provisions. 09-40500004 & 09-40500006 ~ Flood Hazard District Zoning Map Amendment, Special Purpose District Map Amendment, and Development Text Amendment UAPC-Staff Report Page 1 of 10 TÒ UtifcJFtp II. AUTHORITY AND CRITERIA: Sections 4.032, 4.042 and 4.102 of the City of Grants Pass Development Code provide the procedures for initiation of a Special Purpose District Map Amendment and Development Code Text Amendment. The proposed Special Purpose District Map Amendment and Development Code Text Amendment were initiated by the Community Development Director. Sections 2.060, 7.040 and 7.050 authorize the Urban Area Planning Commission to make a recommendation to the City Council and authorize the City Council to make a final decision on a land use matter requiring a Type IV procedure, in accordance with procedures of Section 2.060. The applicable criteria from the Development Code to be met include the following: • Section 4.033 -Zoning Map Amendment Section 4.044 - Special Purpose District Amendment Section 4.103 - Development Code Text Amendment III. APPEAL PROCEDURE: The City Council's final decision may be appealed to the State Land Use Board of Appeals (LUBA) as provided in state statutes. A notice of intent to appeal must be filed with LUBA within twenty-one (21) days of the Council's written decision. IV. BACKGROUND AND DISCUSSION: The City of Grants Pass participates in the National Flood Insurance Program (NFIP). By having ordinances that comply with the NFIP, residents are eligible to obtain flood insurance through the program. FEMA has recently completed the process of updating the Flood Insurance Study (FIS) and Flood Insurance Rate Maps (FIRMsj throughout the country and state, including Josephine County. Both the City of Grants Pass and Josephine County will be adopting the complete FIS and all of the FIRM maps covering Josephine County and the incorporated areas. By doing so, there will not be a need to undertake an additional amendment in the event the Urban Growth Boundary is adjusted in the future. The,purpose of the new FIS is to revise and update information on the existence and severity of flood hazards in the geographic area of Josephine County, to include the Cities of Cave Junction and Grants Pass, The original hydrologic and hydraulic analyses were performed by the U.S. Geological Survey (USGS), and completed in 1979. The countywide updated was performed by WEST Consultants, Inc., and was completed in October 2008. On June 3, 2009, FEMA mailed their "Letter of Final Determination" instructing the City that the new study and maps must be adopted by December 3, 2009, to maintain its 09-40500004 & 09-40500006 ~ Flood Hazard District Page 2 of 10 Zoning Map Amendment, Special Purpose District Map Amendment, and Development Text Amendment UAPC-Staff Report participation in the flood insurance program (See Exhibit 5). The FIS and FIRM maps currently in effect are dated September 27, 1991. The floodway boundary and floodway maps have been incorporated into the new FIRM maps. The existing FIS and FIRM maps will be maintained for historical reference. Failure to adopt the study and maps by December 3 means the City would be suspended from the flood insurance program effective on that date, leaving citizens at risk of flood damage that would not be covered by the National Flood Insurance Program. Adoption of the new FIS and FIRM maps requires that Element 5 of the Comprehensive Plan, specifically the section under Flood Hazard (5.30) be amended to reference the new FIS and FIRM effective December 3, 2009. The revision is à modification to the narrative of the Comprehensive Plan and the change is reviewed as a minor amendment to the database in accordance with Section 13.5.2 of the Comprehensive Community Development Plan Policies document. No criteria are reviewed with the narrative change. In addition to adopting the new FIS and FIRMs, FEMA's "Letter of Final Determination" states additional requirements must be met under Section 1361 of the National Flood Insurance Act of 1968, as amended, within six (6) months of the date of their letter. Specifically, the standards of Paragraph 60.3(d) of the NFIP regulations must be met. The letter goes on to list the following actions in order to be in compliance: • Amend existing regulations to incorporate any additional requirements of Paragraph 60.3(d); • Adopt all standards of Paragraph 60.3(d) into one new, comprehensive set of regulations; or • Show evidence that regulations have previously been adopted that meet ' or exceed the minimum requirements. Thé "Letter of Final Determination" included a "Summary of Map Actions" documenting previous "Letter of Map Change (LOMC) actions (including Letters of Map Amendment and Letters of Map Revision) which will be superseded by the revised FIRM panels.. Many property owners will find little change in the flood information for their property, while others will be required to meet the new elevation requirements for all new structures and substantial improvements to existing structures. An example of the existing and amended maps is provided: 09-40500004 & 09-40500006-Flood Hazard District Page 3 of 10 Zoning Map Amendment, Special Purpose District Map Amendment, and Development Text Amendment UAPC-Staff Report EXISTING FLOOD MAPS 09-40500004 & 09-40500006 ~ Flood Hazard District Page 4 of 10 Zoning Map Amendment, Special Purpose District Map Amendment, and Development Text Amendment UAPC-Staff Report 09-40500004 & 09-40500006 ~ Flood Hazard District Zoning Map Amendment, Special Purpose District Map Amendment, and Development Text Amendment UAPC-Staff Report Page 5 of 10 The summary notes one LOMC for 643/645 SW Balsam Drive, Grants Pass, Oregon, which will be superseded by new detailed flood hazard information based upon revised hydrologic and hydraulic analyses. The property owners were mailed a separate notice concerning the revised FIRMs, but they have not responded as of the date of this report. The existing regulations in Article 13 of the Development Code have been reviewed against Paragraph 60.3 (d) and the State's Model Flood Plain Ordinance for consistency. The additions and changes to Section 13.200 are reflective of the regulations from the above documents. The Municipal Code also includes flood hazard regulations. All flood hazard provisions have been incorporated into Section 13.200 of the Development Code. The final ordinance for approval by the City Council will repeal any old ordinances and existing language that has been incorporated into the Development Code. V. CONFORMANCE WITH APPLICABLE CRITERIA ~ SECTION 4,033 OF THE DEVELOPMENT CODE Criteria for Amendment. The Zoning Map may be amended by the review bodies provided that all the following criteria are met: (1) The proposed use, if any, is consistent with the proposed Zoning District. (2) The proposed Zoning District is consistent with the Comprehensive Plan Land Use Map designation. (3) A demonstration that existing or proposed levels of basic urban services can accommodate the proposed or potential development without adverse impact upon the affected service area or without a change to adopted utility plans. (4) A demonstration that the proposed amendment is consistent with the functions, capacities and performance standards of transportation facilities identified in the Master Transportation Plan. (5) The natural features of the site are conducive to the proposed Zoning District. (6) The proposed zone is consistent with the requirements of all overlay Districts that include the subject property. (7) The timing of the zone change request is appropriate in terms of the efficient provision orupgrading of basic urban services versus the utilization of other buildable lands in similar zoning districts already provided with basic urban services. (8) In the case of rezoning from the Urban Reserve District, that the criteria for conversion are met, as provided in Section 4.034. 09-40500004 & 09-40500006- Flood Hazard District Page 6 of 10 Zoning Map Amendment, Special Purpose District Map Amendment, and Development Text Amendment UAPC-Staff Report Staff Response: Not Applicable. Although the proposed amendments do not related to zoning, it was found that review and acknowledgement of the criteria was important. The adoption of the new FIS and FIRM will result in a map change to the flood hazard, one of the special purpose districts regulated by the City of Grants Pass. The amendment affects properties along the Rogue River and Gilbert Creek. However, the above listed criteria are found not applicable to the amendment. VI. CONFORMANCE WITH APPLICABLE CRITERIA - SECTION 4.044 OF THE DEVELOPMENT CODE (1) The Flood Hazard District map is the Flood Boundary - Floodway Map established by the Federal Emergency Management Agency (FEMA) in the scientific and engineering reports entitled "The Flood Insurance Study for the City of Grants Pass" and the "The Flood Insurance Study for the County of Josephine County, State of Oregon". The flood hazard district map may be amended only by FEMA in the procedure provided for Flood Boundaries - Floodway Maps. (2) Upon receipt of proper authorization from FEMA, the Director shall begin administering the revised Flood Hazard District, as designated by FEMA. Staff Response: Satisfied. As noted above, on June 3, 2009, FEMA mailed their "Letter of Final Determination" instructing the City that the new FIS and FIRM maps must be adopted by December 3, 2009, to maintain its participation in the flood insurance program. Upon adoption, the updated FIS, FIRM and Section 13.200 of the Development Code, will be used to regulate properties in the flood hazard area. VII. CONFORMANCE WITH APPLICABLE CRITERIA - SECTION 4.103 OF THE DEVELOPMENT CODE The text of the Development Code may be recommended for amendment and amended provided that all of the following criteria of Section 4.103 of the Development Code are met. CRITERION 1: The proposed amendment is consistent with the purpose of the subject section and article. Staff Response: Satisfied. The proposal amends Section 13.200 "Flood Hazard District". The purpose statement of Section 13.210 states that the intent of the Flood Hazard District is to designate areas that may be hazardous to development due to flooding. The District is to provide standards that specify how development will minimize public and private losses due to flood conditions in specific areas by provisions designed to: 09-40500004 & 09-40500006 ~ Flood Hazard District Page 7 of 10 Zoning Map Amendment, Special Purpose District Map Amendment, and Development Text Amendment UAPC-Staff Report • Protect human life and health; • Minimize expenditure of public money; • Minimize need for rescue and relief efforts; • Minimize prolonged business interruptions; • Minimize damage to public facilities; • Help maintain a stable tax base; • Notify potential buyers of special flood hazard; and • Ensure those who occupy flood hazard areas accept responsibility for their actions. The proposed amendment is consistent with the purpose statement of Section 13.210 because it brings the Development Code into compliance with regulations of the National Flood Insurance Program (NFIP, Paragraph 60.3(d)) as required under Section 1361 of the National Flood Insurance Act of 1968, as amended. Specifically, the proposed text amendment will: • Consolidate various flood ordinances currently located within the Municipal Code, into one location in the Development Code, • Provide additional terms and definitions for the flood hazard district; and • Brings construction standards for crawlspaces and below-grade , crawlspaces into compliance. CRITERION 2: The proposed amendment is consistent with other provisions of this code. Staff Response: Satisfied. As noted under Section 13.010 of the Development Code, special purpose districts, to include the Flood Hazard District, provide standards intended to mitigate natural hazards, to protect natural features and to mitigate land use conflicts. The standards applicable for the Flood Hazard District are in addition to the standards of the underlying zoning district. Therefore, .the proposed amendment is internally consistent with other provisions of the Development Code. CRITERION 3: The proposed amendment is consistent with the goals and policies of the Comprehensive Plan, and most effectively carries out those goals and policies of all alternatives considered. Staff Response: Satisfied. The proposed amendment is consistent with the goals and policies of the Comprehensive Plan. Section 5.2 of.Element.5 of the Comprehensive Plan Policy document states that the Development Code shall: • Regulate development within the 100-year floodplain and floodway as required to maintain participation in the National Flood Insurance Program; 0940500004 & 09-40500006 ~ Flood Hazard District Page 8 of 10 Zoning Map Amendment, Special Purpose District Map Amendment, and Development Text Amendment . UAPC-Staff Report • Provide methods to determine and appeal the location of the 100- year floodplain and floodway boundaries when there appears to be discrepancies between official mapped boundaries and actual field conditions. ® Facilitate flood hazard policies. The proposed changes to Section 13.200 of the Development Code and the narrative of the Comprehensive Plan help implement the policy statements. As noted above, the narrative of Element 5 of the Comprehensive Plan (Section 5.30 - Flood Hazard) is being modified to reference the new FIS and FIRM effective December 3, 2009. The alternative of not adopting the new FIS, FIRM and Code sections is not a viable option as it would cause suspension with the City's participation in thè NFIP. CRITERION 4: The proposed amendment is consistent with the functions, capacities, and performance standards of transportation facilities identified in the Master Transportation Plan. Staff Response: Not Applicable. The proposed amendments do not pertain to the performance standards of the Master Transportation Plan. VIII. RECOMMENDATION: A. It is recommended that the Urban Area Planning Commission recommend that City Council APPROVE the amendment of the Special Purpose District Map for the Flood Hazard District by adopting the current Flood Insurance Study (FIS) Volumes 1 and 2 and Flood Insurance Rate Maps (FIRM) for Josephine County, Oregon and Incorporated areas effective date December 3, 2009, issued by the Department of Homeland Security's Federal Emergency Management Agency (FEMA). B. It is recommended that the Urban Area Planning Commission recommend that City Council APPROVE the proposed amendment to Section 13.200 (Flood Hazard District) of thé City of Grants Pass Development Code to be consistent with the National Flood Insurance Program (NFIP) and Oregon Model Code Provisions. C. It is recommended that the Urban Area Planning Commission recommend that City Council APPROVE the amendment to update Element 5 of the Comprehensive Plan, specifically the section under Flood Hazard (5.30) to reference the new FIS and FIRM effective December 3, 2009. 09-40500004 & 09-40500006 -Flood Hazard District Page 9 of 10 Zoning Map Amendment, Special Purpose District Map Amendment, and Development Text Amendment UAPC-Staff Report IX. PLANNING COMMISSION ACTION: A. Positive Action: Recommend approval of the request: 1. as submitted. 2. as modified by the Planning Commission (list): B. Negative Action: Recommend denial of the request for the following reasons (list): C. Postponement: Continue item 1. indefinitely. 2. to a time certain. NOTE: The application is not subject to the 120 day requirement per ORS 227.178. X. INDEX TO EXHIBITS: 1. Flood Insurance Study (FIS) for Josephine County, Oregon and Incorporated areas, dated December 3, 2009 (full report is available in the Planning file). 2. Flood Insurance Rate Maps (FIRM) dated December 3, 2009 (full set of maps is available in the Community Development office). 3. Revised Section 13.200 ~ Flood Hazard District Development Code. 4. Revised Element 5, Section 5.30, Flood Hazard located in the Comprehensive Plan 5. FEMA's "Letter of Final Determination" dated June 3, 2009. 09-40500004 & 09-40500006 - Flood Hazard District Page 10 of 10 Zoning Map Amendment, Special Purpose District Map Amendment, and Development Text Amendment UAPC - Staff Report FLOOD INSURANCE STUDY JOSEPHINE COUNTY, OREGON AND INCORPORATED AREAS VOLUME 1 OF 2 COMMUNITY COMMUNITY NAME NUMBER CAVE JUNCTION, CITY OF 410107 GRANTS PASS, CITY OF 410108 JOSEPHINE COUNTY UNINCORPORATED AREAS 415 5 90 Effective: December 3, 2009 Federal Emergency Management Agency Flood Insurance Study Number 41033CV001A i NOTICE TO FLOOD INSURANCE STUDY USERS Communities participating in the National Flood Insurance Program have established repositories of flood hazard data for floodplain management and flood insurance purposes. This Flood Insurance Study (FIS) report may not contain all data available within the Community Map Repository. Please contact the Community Map Repository for any additional data. Selected Flood Insurance Rate Map panels for the community contain information that was previously shown separately on the corresponding Flood Boundary and Floodway Map panels (e.g. floodways, cross sections). In addition, former flood hazard zone designations have been changed as follows: Old Zone New Zone Al through A30 AE VI through V30 VE B X (shaded) C X (unshaded) Part or all of this maybe revised and republished at any time. In addition, part of this FIS may be revised by a Letter of Map Revision process, which does not involve republication or redistribution of the FIS. It is, therefore, the responsibility of the user to consult with community officials and to check the community repository to obtain the most current FIS report components. This FIS report was revised on December 3,2009. User should refer to Section 10.0, Revision Descriptions, for further information. Section 10.0 is intended to present the most up-to-date information for specific portions of this FIS report. Therefore, users of this FIS report should be aware that the information presented in Section 10.0 supersedes information in Sections 1.0 through 9.0 of this FIS report TABLE OF CONTENTS - VOLUME 1 - " Page 1.0 INTRODUCTION 1 1.1 Purpose of Study 1 1.2 Authority and Acknowledgements 1 1.3 Coordination 1 2,0 AREA STUDIED 3 2.1 Scope of Study 3 2.2 Community Description 5 2.3 Principal Flood Problems 7 2.4 Flood Protection Measures 9 3.0 ENGINEERING METHODS 10 3.1 Hydrologie Analyses 10 3.2 Hydraulic Analyses 15 3.3 Vertical Datum 24 4.0 FLOODPLAIN MANAGEMENT APPLICATIONS 24 4.1 Floodplain Boundaries 25 4.2 . Floodways 26 5.0 INSURANCE APPLICATION 47 6.0 FLOOD INSURANCE RATE MAP - 4 7 - 7.0 OTHER STUDIES 48 8.0 LOCATION OF DATA 50 9.0 BIBLIOGRAPHY AND REFERENCES 50 10.0 REVISION DESCRIPTION 53 FIGURES Figure 1 - Flo.odway Schematic 27 TABLES Table ! - Initial, Intermediate, and Final CCO Meetings Table 2 - Flooding Sources Studied by Detailed Methods Table 3 - Flooding Sources Studied by Approximate Methods Table 4 - Summary of Discharges Table 5 - Range of Manning's Roughness Values Table 6 - Floodway Data Table 7 - Flood Insurance Zones Within Each Community Table 8 - Community Map History 2 3 . 4 11 15 28 47 49 TABLES (continued^ Table 9 - Revised Study Descriptions . 53 TABLE OF CONTENTS - VOLUME 2 EXHIBITS Exhibit 1 - Flood Profiles Applegate River Deer Creek Gilbert Creek Illinois River East Fork Illinois River West Fork Illinois River Jumpoff Joe Creek Louse Creek Murphy Creek Rogue Rive- Rogue River Right Overbank Slate Creek Waters Creek • Panels Panels Panels Panels Panels Panels Panels Panels Panels Panels Panel Panels Panels 01P-18P 19P-23P 24P-29P 30P-35P 36P-47P 48P-59P 60P-66P 67P-80P 81P-86P S7P-IÖ0P 101P 102P-108P 109P-U1P PUBLISHED SEPARATELY Flood Insurance Rate Map Index Flood Insurance Rate Map i l FLOOD INSURANCE STUDY JOSEPHINE COUNTY, OREGON AND INCORPORATED AREAS 1.0 INTRODUCTION 1.1 Purpose of Study This Flood Insurance Study revises and updates information on the existence and severity of flood hazards in the geographic area of Josephine County, including the Cities of Cave Junction and Grants Pass; and the unincorporated areas of Josephine County (referred to collectively herein as Josephine County), and aids in the administration of the National Flood Insurance Act of 1968 and the Flood Disaster Protection Act of 1973. This study has developed flood-risk data for various areas of the community that will be used to establish actuarial flood insurance rates and to assist the community in its efforts to promote sound floodplain management. Minimum floodplain management requirements for participation in the National Flood Insurance Program (NFIP) are set forth in the Code of Federal Regulations at 44 CFR, 60.3. In some states or communities, floodplain management criteria or regulations may exist that are more restrictive or comprehensive than the minimum Federal requirements. In such cases, the more restrictive criteria take precedence and the State (or other jurisdictional agency) will be able to explain them. 1.2 Authority and Acknowledgments The sources of authority for this Flood Insurance Study are the National Flood Insurance Act of 1968 and the Flood Disaster Protection Act of 1973. The hydrologic and hydraulic analyses for the studies in Grants Pass and unincorporated Josephine County were performed by the U.S. Geological Survey (USGS) for the Federal Emergency Management Agency (FEMA) under Interagency Agreement No. IAA-H-14-78, Project Order No. 8. The analysis for the City of Cave Junction was performed under Amendment 1-2 of the same contract. Analyses for the City of Cave Junction and unincorporated Josephine County were completed in July 1980. The original analysis for the . City of Grants Pass was completed in July 1979. The restudy of the reach of the Rogue River flowing through Grants Pass was performed by OTÁK, Incorporated. This additional work was completed in December 1989 for FEMA under Contract No. EMW-89-C-2847. The countywide update was performed by WEST Consultants, Inc. for FEMA under ContractNo. EMS-20010-CO-0068.. Updated aerial photography daied 2005 was used in the analysis. Work on the countywide update was completed in October 2008. 1.3 Coordination The dates of the initial, intermediate, and final CCO meetings held for the previous FIS reports for "Josephine County and the incorporated communities within its boundaries are shown in Table 1, "Initial, Intermediate, and Final CCO Meetings". They were attended by representatives of FEMA, the U.S. Geological Survey, the communities, and the study contractor. 1 Table 1. Initial, Intermediate, and Final CCO Meetings Community Initial CCO Date Final CCO Date Cave Junction, City of January 12, 1978 May 12, 1980 June 3, 1981 Grants Pass, City of January 1978 ^ J 9 , 8 ^ " d September 19, 1990 Josephine County, unincorporated areas May 25, 1988 January 12, 1978 May 12, 1980 June3, 1981 Streams requiring detailed study were identified at a meeting held on January 12,1978. In attendance were representatives of the U.S. Geological Survey, FEMA, Josephine County, and the communities of Cave Junction and Grants Pass. The U.S. Army Corps of Engineers (COE) provided hydrologic data for the original Rogue River study, reflecting anticipated flood-control regulation from Lost Creek Dam, located 55.4 miles upstream from the city. Results of the hydrologic analyses were coordinated with the COE. Ending water-surface elevations at Savage Rapids Dam on the Rogue River were consistent with data furnished by the U.S. Geological Survey for the Jackson County Flood Insurance Study (Reference 1), On May 12, 1980, an intermediate meeting reviewing preliminary work done by the study contractor was attended by representatives of the study contractor, FEMA, the City of Cave Junction, and Josephine County. On May 27,1980, the results of the original study for the City of Grants Pass were reviewed at the final community coordination meeting attended by representatives of FEMA, the city, and the study contractor. No problems were raised at die meeting. A final coordination meeting for the City of Cave Junction and Josephine County was held on June 3, 1981. The meeting was attended by representatives of the FEMA, the study contractor, the City of Cave Junction, and Josephine County. All problems raised at the meeting were resolved. Several flooding sources within Grants Pass, including portions of the Rogue and Applegate Rivers, and portions of Louse and Waters Creeks were selected for restudy at a meeting attended by representatives of FEMA, Josephine County, the City of Grants Pass, and the study contractor on May 25,1988. Results of the hydrologic analyses performed by OTAK, Incorporated were coordinated with the COE, USGS, Soil Conservation Service, Oregon Department of Land Conservation and Development, and Josephine County. On September 19, 1990, the results.of the restudy were reviewed at the final community coordination meeting attended by representatives of FEMA, the city, and the study contractor. Countvwide Update An initial community coordination meeting for Josephine County was held on March 6, 2006. This meeting was attended by representatives of the Cities of Grants Pass and Cave Junction, Josephine County, FEMA, and WEST Consultants, Inc. The results of the study were reviewed at the final Consultation Coordination Officer [CCO] meeting held on March 5, 2009, and attended by representatives of the Cities of Cave Junction and Grants Pass, Josephine County, The Oregon Department of Land Conservation and Development and FEMA. All problems raised at that meeting have been addressed in this study. 2 2,0 AREA STUDIED 2.1 Scope of Study This Flood Insurance Study covers the geographic area of Josephine County, Oregon, including the incorporated communities listed in Section 1.1. The flooding sources studied by detailed methods in unincorporated Josephine County and the City of Cave Junction were selected with priority given to all known flood hazards and areas of projected development or proposed construction through 1985. Projected development or proposed construction were considered through 1995 within the City of Grants Pass, The limits of detailed studies in Josephine County were determined by FEMA with community and study contractor consultation at meetings in January 1978 and May 1988. Table 2 lists the flooding sources studied in detail and the included segments. River mileages used in this discussion are based on data published by the Hydrology Committee of the Columbia Basin Inter-Agency Committee (Reference 2), Table 2. Flooding Sources Studied by Detailed Methods Limits of Detailed Study From its confluence with the Rogue River to approximately 4,000 feet upstream of Wildcat Gulch near Murphy. From a point approximately one mile southwest of Selma (RM 3.5) to Crooks Creek. From SW Rogue River Avenue to approximately 875 feet upstream from NW North Hill Drive. From the stream gaging station north ofKerby (near RM 50.0) to the confluence of the East and West Forks of the Illinois River. From its confluence with the Illinois River to approximately 500 feet downstream from Sucker Creek near Cave Junction and from Little Elder Creek (RM 65.6) to Page Creek south of Takilma. From its confluence with the Illinois River to the Redwood Highway bridge and from a noint 870 feet downstream from . Hugo Road at.O'Brien (RM 7.8) to a point approximately 2.4 miles further upstream. From its confluence with the Rogue River to Monument Drive • near Merlin. From its confluence with Jumpoff Joe Greek to Granite Hill Road. From its confluence with the Applegate River to approximately 7,000 feet upstream from its mouth. Flooding Source 1. Applegate River 2. Deer Creek 3. Gilbert Creek 4. Illinois River 5. East Fork Illinois River 6. West Fork Illinois River 7. Jumpoff Joe Creek 8; Louse Creek 9. Murphy Creek 3 Table 2. Flooding Sources Studied by Detailed Methods (continued) 10. Rogue River 11. Rogue River Right Overbank 12. Slate Creek 13. Waters Creek From Maple Creek near Galice (RM 75.2) to the Josephine- Jackson County limits at Savage Rapids Dam.. From its confluence with the main stem of the Rogue River to its divergence from the main stem of the . Rogue River approximately 1,300 feet upstream from Lincoln Avenue. From its confluence with the Applegate River to approximately the intersection of Round Prairie Road and Redwood Highway. From its confluence with Slate Creek to approximately 6,200 feet upstream from its mouth. Flows in Skunk Creek and Blue Gulch are well contained in rectified channels or underground conduits and were not included in the original study. The consultation meetings in January 1978 andMay 1988 further identified flooding sources for which the extent of floodway analysis would be limited or excluded. The Rogue River floodway was determined only from Pass Creek downstream of Grants Pass to the Josephine- Jackson County boundary. Hie Louse Creek floodway analysis was terminated at a point 2,100 feet downstream from the Interstate Highway 5 bridge. The detailed analysis of Murphy Creek did not include a floodway analysis. Floodway delineations were considered unnecessary in the areas already having multiple. Federal, State, and county permit requirements for new construction (such as the area downstream from Pass Creek on the Rogue River). Approximate analyses were used to study flooding sources in areas having a low development potential or minimal flood hazards. The scopes and methods of analysis were proposed to, and agreed upon by FEMA, Josephine County , and the Cities of Cave Junction and Grants Pass. These analyses wete adopted from previously effective flood hazard boundary maps (Reference 3). Table 3 lists the flooding sources, grouped by watershed, which were studied by approximate methods. . Table 3. Flooding Sources Studied by Approximate Methods 1. Rogue River, Grave Creek, Wolf Creek, Coyote Creek, Lirnpy Creek, and Dutcher Creek. 2. Jumpoff Joe Creek, Quartz Creek, Bummer Creek, Bannister Creek, Schoolhouse Creek, and Hairris Creek. 3. Slate Creek, Cheney Creek, Murphy Creek, Williams Creek, Banning Creek, and the East and West Forks of Williams Creek. 4. Deer Creek, Clear Creek, Draper Creek, Davis Creek, McMullin Creek, and Crooks Creek. 5. Illinois River, West Fork Illinois River, MendenhalJ Creek, Rough and Ready Creek, Elk Creek, East Fork Illinois River, Kelly Greek, Tycer Creek, Sucker Creek, Democrat Guleh, Mulvaney Gulch, Althouse Creek, and Althouse Slough. 4 2.2 Community Description Josephine County is located in southwestern Oregon, sharing its southern boundary with the State of California. Established in 1856, the county has an area of 1,625 square miles. Residential land development is present throughout the county due to the moderate climate and recreational features of the region. The estimated population of the county was 52,100 in 1978 (Reference 4). The population as of the 2000 census was 75,726 (Reference 5). The climate of Josephine County is typical of other areas of Oregon west of the Cascade Range. The average July temperature is 71.2°F; in January, the average temperature is 39.9°F. The Klamath Mountain Range to the west provides a minor orographic barrier to winter storms moving inland from the Pacific Ocean. Heavy winter rainfall usually occurs in the interior valleys, and deep snow accumulates at the higher elevations of the Cascade, Siskiyou, and Klamath Mountain Ranges. The average annual rainfall varies from approximately 30 inches in Grants Pass to over 60 inches in the Siskiyou Mountains. The Cascade Range, far to the east, accumulates almost 80 inches of precipitation (Reference 6). Josephine County is drained almost entirely by the Rogue River and its two principal tributaries, the Applegate and Illinois Rivers. Steep, mountainous terrain lends to rapid runoff when mild temperatures and heavy rainfall melt snow at the.higher elevations. The Rogue River originates in the Cascade Range where the highest elevations exceed 8,000 feet. The drainage area of the river as it enters Josephine County at Savage Rapids Dam is 2,430 square miles. As the river flows westerly through the county, flood flows are fairly well contained by both banks until reaching the City of Grants Pass, 5.5 miles downstream of the dam. From Grants Pass to Finely Bend (9.9 miles west of the city), vast areas of low- lying terrain are subject to severe flooding. From Finley Bend, the river meanders north of Jumpoff Joe Creek (8.5 miles downstream). In these reaches, flood flows are subject to natural bank constrictions which result in sizable ponding of water. Beyond Jumpoff Joe Creek, the Rogue River flows northwesterly toward the resort community of Galice. In this reach, flood flows are totally contained by steep canyon walls, especially at Hellgate Canyon and at an unnamed canyon ending at Taylor Creek. In these canyons, flood flows become constricted to a few hundred feet in width. Beyond Galice, the river continues its westward passage through the Klamath Mountain Range until it eventually reaches the Pacific Ocean, The Applegate River originates in the Siskiyou Mountains which form all but the northern boundary of the basin. The summit of the range reaches elevations of over 7,000 feet in some areas. The river enters Josephine County from the southeast at a point 7.5 miles upstream from the small community of Murphy. The drainage area at a discontinued gaging station at the bridge in Murphy, is 663 square miles. Flood flows in a sharply meandering channel inundate wideportions of the floodplain that lie upstream from natural constrictions. Five miles downstream from Murphy, the river passes through a short, narrow eanyon. After leaving the canyon, overbarik flooding is moderate until the river becomes affectedby backwater from the Redwood Highway (U.S. Highway 199) bridge near Wilderville. Here, extensive flooding occurs. Approximately 0.6 miles downstream from the bridge, the Applegate River becomes affected by backwater from the Rogue River. The inundated Applegate River flood plain width exceeds 4,000 feet at its mouth (6.4 miles west of the City of Grants Pass). The eastern boundary of the Illinois River basin is also formed by the Siskiyou Mountains. The southern and western boundaries are formed by the Che.tco Divide of the Kiamath Mountain Range. Summit elevations vary from 4,000 to 6,000 feet. The headwaters of Illinois River consist of two principal tributaries, the East and West Forks. Illinois River. The 5 East Fork Illinois River enters Josephine County from the south at a point 3,9 miles upstream from the community'of Takilma', The drainage area at a gaging station located 0.3 miles north of the county limits is 42.3 square miles. General flooding occurs in most areas near Takilma except in a gorge east of the community. Farther north, extensive flooding occurs in thè wide, flat floòdplain downstream from the Redwood Highway Bridge near Cave Junction. The East Fork Illinois River joins the West Fork Illinois River to form the main stein of the Illinois River at the City of Cave Junction. The West Fork Illinois River also flows northerly into Josephine County at a point 7.1 miles upstream from the community of O'Brien. The drainage area of a gaging station located approximately 4 miles north of the county limits is 42.4 square miles. The most significant flooding in O'Brien occurs at the Redwood Highway Bridge. Overflow inundates portions of the community before re-entering the channel downstream from the bridge. Farther north, near Cave Junction, flooding is much more severe. Wide areas are inundated, especially near the drive-in theater located 2.5 miles south of the community. Below the confluence of its East and West Forks, the Illinois River flows northerly through fertile agricultural areas. Wide floodplains between Cave Junction and Kerby (2 miles to the north) become completely flooded. The flooding north of Kerby is equally severe, eaused in part by a sharp bend in the river as it enters a narrow canyon. Beyond the mouth of the canyon (2.5 miles north of Kerby), the Illinois River continues westward through the Klamath Mountain Range until it meets the Rogue Ri ver at the summer resort community of Agness in Curry County, 50.2 miles downstream. Deer Creek, a tributary of the Illinois River, is located entirely within Josephine County. The creek originates in the Siskiyou Mountain foothills, south of Grants Pass, and flows westerly toward the community of Selma. The drainage area of the stream at a point 3.5 miles upstream from its mouth is 101 square miles. Flood plains in the Selma area are low and flat. Extensive flooding occurs in this agricultural area. City of Cave Junction The City df Cave Junction is in the southwestern portion of Josephine County. The city, surrounded by unincorporated areas of Josephine County ^ is approximately 25 miles southwest of Grants Pass, Oregon, and 12 miles north of the Oregon-California State boundary. Cave Junction, incoiporated in 1948, is the second largest city in thé county, with an estimated 1978 population of over 800. Its population as of the 2000 census was 1,363 (Reference 5). Residential development is present throughout the area due to the moderate climate and recreational features of the region. The climate of Cave Junction is typical of other areas of Oregon west of the Cascade Range. The average July temperature is 71.2°F; in January, 39.3°F. The Klamath Range to the west provides a minor orographic barrier to winter storms moving inland from the Pacific Ocean. Heavy winter rainfall usually occurs in the interior valleys, and deep snow accumulates at higher elevations of the Cascade, Siskiyou, and Klamath Mountain Ranges. (Reference 6). City.of Grants Pass The City of Grants Pass is situated along the Rogue River in eastern Josephine County approximately 25 miles northwest of Medford, Oregon, and 30 miles north of the Oregon- California State boundary. incorporated in 1887, Grants Pass is the county seat and had a population of23,023 as of the 2000 census. The city extends across a 3-mile-wide valley and is bounded by densely wooded hills to the north and south. Fertile lowland areas support a sizable agricultural industry; timber and related byproducts are also important to the economy. Seasonal recreation fishing and character excursion trips on the Rogue River make Grants Pass a very popular tourist center. The Rogue River floodplain within the city has areas of dense residential and commercial development. Aerial photographs show that some small tracts of land are undeveloped, but local land use measures may dictate the type and extent of future development. Gilbert Creek has a very high density of residential development. The drainage area of the Rogue River at the gage in Grants Pass is 2,459 square miles. The river originates in the Cascade Range, where heavily forested slopes reach elevations exceeding 8,000 feet. These steep slopes usually accumulate heavy winter snowfall, and stonn runoff is rapid when mild temperatures and sustained rainfall occur during the passage of a Pacific storm front. An exception to. this general runoff characteristic occurs above an. elevation of 5,000 feet in the vicinity of Crater Lake. Highly permeable pumice soils and lava formations allow much of the rainfall and snowmelt to infiltrate the ground, thus reducing surface runoff (Reference 7). The drainage area of.Gilbert Creek is 5.68 square miles at its mouth. The creek originates in the foothills north of the city, where the highest elevation is approximately 3,100 feet. The channel gradient is very steep until reaching the city, and peak flows usually occur within hours after the passage of a storm front. Topography varies from the steep, forested slopes of Blue Gulch in the northwestern part of the city to the more gently sloping floodplain of the rest of Grants Pass. Elevations range from approximately 900 feet along the Rogue River to over 1,500 feet in the northwestern portion of the city (Reference 8). The average annual temperature is 54°F, with historic extremes ranging from 114°F in 1928 to -1°F in 1972 (Reference 9). Average annual rainfall varies from approximately 30 inches in the vicinity of Grants Pass to almost 80 inches in the extreme northeastern corner of the basin near Crater Lake (Reference 6). 2.3 Principal Flood Problems Abnormally heavy or prolonged rainfall, sometimes combined with snowmelt and frozen or nearly saturated ground, may cause flooding in Josephine County. All streams in Josephine County usually respond to the same storm event, but the (quantitative response ean vary considerably. For example, most steams reached record stages during the devastating floods of December 1964; peak stages on the Applegate River, although high in 1964, were exceeded in January 1974. 7 A comparison of historical floods at gaging stations must consider the possibility of changes that might occur in the stream channels between storm events. The scouring of a stream channel could result in the greater flood having a Lower recorded elevation. Flood flows tend to attenuate as they move downstream due toglie lessening qf the channel gradient and to the storage of water in the flood plains. Gaging-station records collected in the upper part of a basin are, therefore, seldom representative of the runoff characteristics in the lower basin. The largest flood in recent times occurred on the Rogue River on December 23, 1964. A peak flow of 152,000 cubic feet per second (cfs) inundated large residential areas in and around the City of Grants Pass. A storm hydrograph at the Grants Pass gaging station showed the maximum stage was reached within 2 days after the initial raise in stage, and overbank flows remained for almost 4 days after the peak occurred. Antecedent climatologi cai conditions were: 90 inches of snow had accumulated at Crater Lake by December 21, the freezing level rose to 11,000 feet on December 22, and rainfall totaled 8 to 10 inches at several reporting stations on December 21 and 22. The Crater Lake snow depth decreased to 68 inches by December 23 with a loss of 4 to 5 inehes in water content (Reference 10). Downstream from the city to approximately Finley Bend, thousands of acres of productive farmland were under as much as 10 feet of water. Severe erosion and siltation occurred, and extensive irrigation systems were destroyed. It is estimated that 360 residences, 19 commercial establishments, and 2 industries were damaged in this area (Reference 10). Downstream from Finley Bend, the river meanders in and out of deep canyons where development consists of ranches, summer homes, and recreational facilities. In December 1964, it is estimated 70 residences were flooded, and 18 were completely destroyed (Reference 10). Based on 38 years of records collected at a gaging station in Grants Pass, it is estimated that a flood of that magnitude would have occurred on the average of once every 50 years prior to ' the construction of Lost Creek Dam. It would now occur oh the average of once every 120 years with anticipated flood regulation in effect (Reference II). In the past 120 years, the December 1964 flood is believed to have been exceeded twice in Grants Pass. The U.S. Army Corps of Engineers estimates a flood in December 1861 had a discharge of 175,000 cfs; in February 1890, 160,000 cfs (Reference 10). They estimated that, due to upstream storage, discharges of that magnitude would now occur on the average of once every 180 years and 140 years, respectively (Reference 11), Gilbert Creek in Grants Pass is ungaged and quantitative historical high-flow data are unknown. Residents living adjacent to the channel have observed road overflow at various culverts throughout the city. There is-severe channel encroachment in many areas due, in part, to vertical retaining walls built at the edge of the low-water channel. A house on L Street spans the channel and will obstruct high flows. On the Applegate River, the largest peak recorded at a gaging station located 1.8 miles southeast of the Town of Applegate in Jackson County occurred on January 15, 1974. A peak discharge of37,200 cfs exceeded the December22,1964 peak of2,500 cfs. Extremely unstable channel conditions make an exact comparison of instantaneous peak flows impossible, and revisions of previously published data have been necessary. Flood damage to agricultural lands was extensive, but most of the damage occurred in areas 8 upstream from theTown-of Murphy.-' It is estimated that 2900 acres òfproductive farmland were inundated (Reference 12). Most of the residential damage occurred downstream from Murphy when the river scoured a sharp bend and inundated almost 200 acres, Based on 38 years of data collected at the Applegate gaging station, it is estimated that a flood of the magnitude of the 1974 peak would reoccur on the average of once every 20 years. Now that the Applegate Reservoir is completed, the recurrence interval has been lengthened. The largest flood on Slate Creek occurred on December 22,1964. A peak flow of4,650 cfs was recorded at a gaging station located 3.6 miles upstream from the community of Wilderville. Flood damage was not extensive because of the sparse population at that time. Based on 19 years of data collected at the gage, a flood of this magnitude would reoccur on the average of once every 8 years. The largest flood recorded in the Illinois River basin occurred on December 22,1964. Two gaging stations located in the upper basin near Takilma and O'Brien indicated unit runoff values of approximately 380 cfs per square mile. Instantaneous peak flows were 15,700 cfs near Takilma and 16,100 cfs near O'Brien. A gaging station located in the lower part of the basin near Kerby had a peak flow of 92,200 cfs and a unit runoff of approximately 240 cfs per square mile. The above unit runoff values are the highest ever recorded in Josephine County. Because of the sparse population at the time, flood damage primarily involved highway bridges and agricultural land. Water depths of over 15 feet covered the Redwood Highway north of Kerby. Some homes were observed floating away from their foundations during the flood. Based on 15 years of records collected at the gaging station on Illinois River near Kerby, it is estimated a flood of this magnitude would occur on the average of once every 150 years. In the upper basin where the flood runoff was more intense, the recurrence interval is estimated to be 500 years at Takilma and 300 years at O'Brien. The Takilma gaging station has 39 years of record; O'Brien, 22 years. Extensive flood damage also occurred in the small tributary basins of Josephine County. Deer Crede, Jumpoff Joe Creek, and Louse Creek, although ungaged, had the highest flows ever observed during the December 1964 storm. Many drainage structures were damaged, resulting in the disruption of traffic. Farmland on the narrow terraces of the valleys suffered erosion and silt accumu 1 ations. Without streamflow data, it is not possible to derive statistical flow data for this flood. 2.4 Flood Protection Measures There are two functioning flood-control reservoirs in the basin. Lost Creek Dam, located 55.4 miles upstream from the gage in Grants Pass, will reduce, the magnitude of peak-flow ' events. It is estimated that a flood of the magnitude of the 1964 Rouge River flood would have occurred approximately once every 50 years prior to the construction of Lost Creek Dam. It should now occur on the average of approximately once every 120 years with existing flood regulation in effect. Due to upstream storage, discharges of the magnitude of the 1861 and 1890 Rogue Riyer floods would now occur approximately once every 180 years and 140 years, respectively (Reference 13). Applegate Reservoir on Applegate River 9 is also located in Jackson County, 33.6 miles upstream from the community of Murphy. Construction of Elk Creek Dam began in 1986 and ceased in 1988. The completed portion of the dam was subsequently breached beginning in July 2008. No flood control isprovided by the remaining structure. There are no extensive levee systems in the county. Some private interests have constructed dikes adjacent to their property; their capability of withstanding sizable flood events is unknown. ENGINEERING METHODS For the flooding sources studied by detailed methods in the community, standard hydrologic and hydraulic study methods were used to determine the flood-hazard data required for this study. Flood events of a magnitude that are expected to be equaled or exceeded once on the average during any 10-, 50-, 100-, or 500-year period (recurrence interval) have been selected as haying special significance for floodplain management and for flood insurance rates. These events, commonly termed the 10-, 50-, 100-, and 500-year floods, have a 10-, 2-, I-, and 0.2-percent chance, respectively, of being equaled or exceeded during any year. Although the recurrence interval represents the long-term, average period between floods of a specific magnitude, rare floods could occur at short intervals or even within the same year. The risk of experiencing a rare flood increases when periods greater than 1 year are considered. For example, the risk of having a flood that equals or exceeds the 100-year flood (1-percent chance of annual exceedence) in any 50-year period is approximately 40 percent (4 in 10); for any 90-year period, the risk increases to approximately 60 percent (6 in 10). The analyses reported herein reflect flooding potentials based on conditions existing in the community at the time of completion of this study. Maps and flood elevations will be amended periodically to refleet future changes. 3.1 Hydrologic Analyses Hydrologic analyses were carried out to establish peak discharge-frequency relationships for each flooding source studied by detailed methods affecting the community. Federal Emergency Management Agency standards require Flood Insurance Studies in adjacent areas to use consistent hydrologic analyses. Accordingly, the hydrology of the Rogue River in Josephine County is identical to that used in the Jackson County Flood Insurance Study (Reference 1). The U.S. Army Corps of Engineers has since revised that hydrology (Reference 11) as shown in the following table (discharges are in cfs). Discharges Flood Event Josephine County Revised Hydrology 10-percent-annuaI-chance 73,000 70,000 2-percent-annuaI- chance 128,000 120,000 1-percent-annual-chance 144,000 153,000 ' 0.2-p ercent-annual-chance 260,000 280,000 Both sets of data are based on 38 years of stream flow records collected at Grants Pass gaging s tation (1939-1976). The discharges are adjusted for expected probability and include anticipated flood-control regulation from Lost Creek Dam. The revised values are still within the 90 percent confidence limits of the original values. The regulating effect of the proposed Elk Creek Dam currently in development by the COE has been evaluated. 10 • s xi O rt a Ci ed O .O . O O O O-O • o- O Ö o o CD o o CD o oo vo oo «n oo CN oC m CM tN i—i: •—1' o o o o o o o oo xr •o" C?\ m rs i— i—. o o m jn m cN o o o o o o a^ rn CD o" en" o\ ^ o\ co M .a o o o o o o o o o o o o ( N VO O I O CD ''TF- oo" C-í VO n o\ vT vo" —1 o o o o m CM oo CM ^ tn en" of CM" 3 1 I •8 I Ö P O 2 § ° S » VD O OO VO rs rs 0\ o\ o o o o o o o o VO ^ 0\ NO o o í o o " C4 1—I 1 I o o o o m vo os t^ -en ^ r-^ oC oo Vo m" o vo o o ^ .o <=> l^N I V es m "S- o Ö H CM • t—< v i ^ FFV V] VI o oo' no en en ^ i—i o o o 0\ "a, ex, < ! ! -M • « Pi ö a fi 5 •S S :§ * ri o t s § u o o P¿ O -t-> +j < Construction of Elk Creek Dam.ceased in 1988. The completed portion of the dam was subsequently breached beginning in July 2008. No flood control is provided by the remaining structure. However, since the regulated discharges, including the anticipated benefit of the Elk Creek facility, were found by OTAIC," Inc. to fall within the 90 percent confidence interval of the unregulated discharges (i.e., without the Lost Creek and Elk Creek facilities), no changes were made to the discharges shown in the Summary of Discharges (Table 4). The U.S. Army Corps of Engineers also provided concordant flood control from both Lost Creek and Applegate Reservoirs. The Applegate River data were based on records collected over an 18-year period at a discontinued gaging station near Wilderville. The magnitude of the design floods on Slate Creek, and Illinois, East Fork Illinois, and West Fork Illinois Rivers was derived by using a log-Pearson Type III probability distribution (Reference 14) of the gaging station data referred to in Section 2.3, A generalized skew coefficient was determined from U.S. Water Resources Council Bulletin 17 (Reference 15). Discharges at sites within 5 to 25 percent of the gaging station drainage area were estimated using the following transfer formula: Qu = Q g ( A „ / A g ) n Where "Qg" and "Ag" are the discharge and drainage area at the gage, "Qu" and "An" are the discharge and drainage area at the ungaged location, and the exponent "n" is an exponent derived from regional flood-frequency equations published in the U.S. Geological Survey Flood-Frequency Analysis for Western Oregon (Reference 16). Design floods at all other ungaged sites were determined using the flood-frequency equations included in the western Oregon analysis. The 0.2-percent-annual-chance flood equation for the Rogue River basin, not included in that report, is: QO:002(500) = 1 0 5 A ° ' 9 1 ( S T + 1 ) " U 6 1 1 , 0 4 Where "A" is drainage area in square miles, "ST" is the area of lakes and ponds (in percent), and "I" is the rainfall intensity (2-year, 24-hour) in inches. The Gilbert Creek hydrology is based on 25 years of peak-flow data collected at a gaging station on Jones Creek, a small basin east of the the City of Grants Pass with headwaters adjoining Gilbert Creek. Jones Creek has. a drainage area of 7.41 square miles at a gaging station located at the culvert entrance on Interstate Highway 5. The discharges.used in this study were computed using a direct drainage area ratio of the two basins even though runoff in the urban areas of Gilbert Creek may differ from the rural runoff in the Jones Creek basin. If was beyond the scope of this study to conduct a detailed study of the effects ofthe storm- sewer inflows within the city. In order to determine the magnitude of the design floods on Jones Creek, the 25 years of peak data were used in a log-Pearson Type III probability distribution, with a generalized skew coefficient determined from the U.S. Water Resources Council Bulletin 17 (Reference 15). The USGS computer program J-407 (Reference 14) detected no low outliers, and the discharges were not adjusted for expected probability. 14 The Gilbert Creek drainage area was determined on the basis of drainage maps provided by tWc City of Grants Pass (Reference 17) and by a USGS topographic map (Reference 8). The 1989 OTAK, Inc. analysis computed flows for Lause Creek and Waters Creek using the USGS equations in the publication entitled "Magnitude and Frequency of Floods of Western Oregon" (Reference 16). The 0.2-percent-annuaI-chance Q equation, describe above, was also used. Salt Creek enters Waters Creek approximately one-half mile upstream of Waters Creek mouth. The hydrologic analyses for the upper portion of the Applegate River were conducted using records from the 42-year period of unregulated flow (i.e., 1939-1980) at the USGS gaging station near Applegate (No. 143 66000) and the regulated flow curves provided by the COE. The accepted regulated discharges (i.e., regulation due to the Applegate Dam) were projected to additional locations of interest upstream of Wildcat Gulch near Murphy using the flow transfer formula described above. Peak discharge information was provided for the 10-, 2-, 1-, and 0.2-percent-annual-chance floods on the Applegate River, although only the 1 -percent-annual chance flood profile was computed. Hydraulic Analyses Analyses of the hydraulic characteristics of flooding from the sources studied were carried out to provide estimates of the elevations of floods of the selected recurrence intervals.Users should be aware that flood elevations shown on the Flood Insurance Rate Map (FIRM) represent rounded whole-foot elevations and may not exactly reflect the elevations shown on the Flood Profiles or in the Floodway Data tables in the FIS report. Flood elevations shown on the FIRM are primarily intended for flood insurance rating purposes. For construction and/or floodplain management purposes, users are cautioned to use the flood elevation data presented in this FIS report in conjunction with the data shown on the FIRM. Water-surface elevations were estimated at all cross sections by a computer program that computes energy losses between sections, using conservation-of-energy equations (step- backwater analysis). This hydraulic model requires accurate measurements of channel cross sections, bridge and dam geometries, and a proper evaluation of the roughnéss of the main channel and floodplains. The water-surface elevations at each cross section were determined by using the U.S. Geological Survey computer program E-431 (Reference 18). Locations of selected cross sections used in the hydraulic analyses are shown on the Flood Profiles (Exhibit 1). For stream segments for which a floodway was computed (Section 4.2); selected cross section locations are also shown on the FIRM. Channel and cross section properties were determined by photogrammetry based on aerial photographs taken September. 30, 1978 (Reference 19). Bridge geometries and the underwater portion of the cross sections were surveyed in January 1979. Roughness coefficients (Manning's "n") were based on field observation and aerial photographs. The range of roughness values used for all floods is shown in Table 5. Flood Source Applegate River Deer Creek Gilbert Creek Table 5. Range of Manning's Roughness Values Main Channel Flood Plain 0.032-0.042 0.034-0.045 0.032-0.055 0.032-0.080 Ó.035-0.080 0.035-0.085 r 15 Table 5. Range of Manning's Roughness Values (continued) Illinois River canyons near ICerby Sours Flat area near Pomeroy Dam 0.038-0.065 0.045-0.050 0.038-0.042 0.050-0.065 .0.040-0.045 0.035-0,055 0.045-0.060 0.034-0.080 0.034-0.080 0 .^034-0.080 0.034-0.080 0.034-0.080 0.035-0.080 0.050-0.080. gravel & roek areas. East Fork Illinois River West Fork Illinois River overflow reach near 0.035-0.070 0.040-0.080 Lone Mountain Road Jumpoff Joe Creek Louse Creek Murphy Creek Rogue River through Grants Pass Slate Creek Waters Creek 0.032-0.055 0.033-0.048 0.045-0,050 0.030-0.065 0.031-0.038 0.032-0.055 0.030-Ö.070 0.032-0.100 0.035-0.080 0.045-0.080 0.032-0.09Ó 0.031-0.200 0.038-0.150 0.038-0.110 The initial water-surface elevations for the flood profiles on the Rogue River were derived from a step-backwater convergence study made through a five-section reach ending at cross section A (Reference 20), Profile convergence was attained for each of the prescribed flows by using the U.S. Geological Survey computer program E-431. The computation procedure requires a uniform change in channel conveyance between cross sections. Also, in rapidly expanding reaches, the program assumes 50 percent of the energy is recovered between sections (due to uncertain eddy losses). Program E-431 became invalid at the outlet of two narrow canyons where chute flows and hydraulic jumps occurred (cross sections R and AB). Therefore; water-surface profiles through these canyons were estimated, and the hydraulic model was reset at the canyon entrances using elevations derived by slope-conveyance studies. Both Hellgate and Robertson bridges are built well above the 0.2-percent-annual-chance flood levels, and neither would constrict the flows. The main channel varied from long calm reaches of silt, interlaced with boulders, to the bedrock outcrops of Hellgate Canyon. Flood plain vegetation varied from smooth, after- harvest hop fields to dense, forests. The Rogue River floodway analysis began at cross section BU. The initial 1 -percent-annual- chance flood elevation for the floodway was taken directly from the normal profile computed for the cross seetion. Because encroachment was not allowed downstream from cross section BU, no surcharge was computed for that cross section. The hydraulic analyses of the reach of the Rogue River in Grants Pass began at a point approximately 2.3 miles downstream of the city, where the overbank flow breakout returns to the channel. Photographs of the 1964 flood revealed that there was divided flow downstream of the city. The December 1964 flood discharges in Grants Pass (152,000cfs) closely approximated the published 1-percent-annual-chance discharge of 144,000 cfs. This 16 discharge resulted in well-defined overflows at the sewage treatment plant and at the RogueHa Mobile Home Park. The initial hydraulic analyses were conducted to identify the various flow behaviors. Three distinct flow patterns occurred: 1. The 10-percent-annual-chance flow was contained in the channel. 2. The 2- and 1-percent-annual-chance floods caused overflows on the right bank. 3. The 0.2-percent-annual-chance flood completely inundated the floodplain. An iterative hydraulic analysis for divided flows around the islands was undertaken to determine the flow distribution. In order to assess the significance of the overflows, survey data were collected to describe the control section over which these overflows would occur. These data were subsequently incorporated into the hydraulic model using the HEC-2 divided flow option. The hydraulic analyses required flow and watcr-surface elevation balances between the main stem and the north overbank at three different locations. The results of the analysis were then compared with the 1964 flood photographs. It was identified that overbank flow returned to the channel at a point located approximately 2.3 miles downstream of the sewage treatment plant. Surveys of typical cross sections for both the channel and the north overbanks were conducted and then compared to data used in die existing Flood Insurance Study hydraulic model of July 1980. It was determined that the variations between the old cross sections and the recently surveyed cross sectio'ns were less then one foot. Therefore the existing cross sectional data were retained for profile computations. Water-surface elevations of floods of the selected recurrence intervals were computed through use of the COE HEC-2 step- backwater computer program (Reference 21). The 1-percent-annual-chance profile on the.Rogue River agreed favorably with many 1964 high-water marks found throughout the study area. However, an exact comparison of profiles is impossible in the lower reaches because of ungaged tributary inflow during the 1964 flood.. There was a small disagreement on the Rogue River between the computed profile elevations and elevations determined from a stage-discharge relation at a gaging station in Grants Pass. A minor adjustment was, therefore, prorated from die gage to the Seventh Street bridge, 0.6 mile downstream. The 1989 restudy of the Rogue River analyzed the reach from a point approximately 3.5 miles downstream of the South 6th Street Bridge in Grants Pass to apoiht 2.2 miles upstream of the South 6th Street Bridge. The restudy included the proposed Redwood Highway crossing. The hydraulic study was conducted by the Oregon Department of Transportation's Hydraulic-Division and was provided by FEMA to OTAK, Inc. Hie restudy used discharge values based on the original values used in the Josephine County Flood Insurance Study of December U 1981, which included die regulating effect of the proposed Elk Creek. Dam, soon to be completed by the COE. The regulated discharges include most of the anticipated benefit for the Elk Creek facility and weirs found to fall within the 90 percent confidence interval of the unregulated discharges (i.e., without the Lost Creek and Elk Creek facilities). The original cross sectional geometry and roughness 17 coefficients for the Rogue River restudy were retained from the original modeling for the restudy computations. Known elevations from the effective modeling were used for the starting water surface elevations of the restudy reach. The selected recurrence intervals were computed using of the COE HËC-2 step-backwater computer program (Reference 21). Photographs of the 1964 flood of the Rogue River at the City of Grants Pass revealed divided flows around the islands located just downstream of thCcity. To determine the flow distribution, thé split-flow option of HEC-2 was used. It was identified that the right ' overbank flow; returned to the channel approximately 2.3 miles downstream of the municipal sewage treatment plant. The resulting water surface elevations matched within 0.2 feet of those published previously. The flood way analysis for the Rogue River restudy was computed using the full 1 -percent- annual-flood discharge assuming no breakout flows. Flood profiles for Gilbert Creek began at the culvert on Rogue River Avenue, the first point where energy controls would not be influenced by backwater from the Rogue River. The initial water-surface elevations were determined from composite stage-discharge relation computed at the culvert entrance. A composite stage-discharge relation is a graphic presentation that combines the amount of water flowing through the culvert with the amount flowing over the road, then relates the total flows to an upstream water-surface elevation. Flows through 23 Gilbert Creek culverts were computed using USGS computer programs E-431 and A-526 (Reference 18 and 22). Most road overflow situations involved flat street surfaces where flow direction was difficult to determine. Where unconfined overflow occurred, the effective width was based on either the upstream channel geometry or the location of houses and garages in the approach section. In all cases, the amount of road overflow was computed using coefficients published in the USGS Techniques of Water-Resources Investigations (Reference 23). Storm-sewer inflows were estimated at West B Street and at Hillcrest Drive using outlet pipe diameters and by assuming the pipe gradient was equal to the ground slope to the nearest manhole structure. Resultant discharges were derived from the Manning equation for pipe flow as given in King's Handbook of Hydraulics (Reference 24). Both Gilbert Creek and Jones Creek have a trans-basin irrigation canal iii the upper basin. The Tokay Canal diversion from the Rogue River is at a pumping station at Savage Rapids Dam, located 6.1 miles, upstream from the Grants Pass gaging station. The canal contribution to flood flows is uncertain because some flows can enter the basin as spillage from the; canal. The ditch capacity at the pumping plant is 47 cfs, but the capacity upstream from Hawthorne Avenue is only 27 cfs. This study assumes ditch flows are negligible during peak events. Flood profiles were drawn showing computed water-surface elevations to an accuracy of 0.5 foot for floods of the selected recurrence intervals (Exhibit 1). Initial water-surface elevations for the profiles on Jumpoff Joe Creek reflected concordant flows of the Rogue River. The 1 -percent-annual-chance flood elevations on Rogue River extended 2.2 miles up the Jumpoff Joe Creek channel. The initial water-surface elevation used for the floodway analysis was estimated from a slope-conveyance study that did not consider concordant flow or backwater. The Jumpoff Joe Creek profiles continued uninterrupted pasttheconfluenceofLouse Creek inMerlin. An increase in channel gradient 18 upstream from Merlin made it necessary to establish additional crosssectidtis. These cross sections were estimated by interpolating between the geometries of the two nearest cross sections, and by using a map having 4 foot contour intervals (Reference 19). Supercritical flow situations were encountered at three cross sections. Each situation required a resetting of the model using critical-depth elevations for each of the prescribed flows. . - ' At Russell Road, the 0.2-percent-annual-chance flood overflowed the highway at a point 800 feet south of the bridge. A composite flow situation could not be computed because the flow in the main channel and flow in the overflow section did not share a common headwater elevation. Road overflow was estimated. The main channel consisted of gravel and small boulders and the overbank areas varied from pastures to dense forests. The initial water-surface elevations for profiles on Louse Creek were headwater elevations computed for the railroad bridge in Merlin.- The headwater elevations were manually computed from a critical-depth section at the outlet of the bridge. Exact discharge values could not be determined because of unknown inflow from Harris Creek, a large tributary with a bridge 450 feet north of the Louse Creek channel. There is an exchange of flow between the two channels via a large ditch at the toe of the railroad embankment. An apportionment of flow through each structure could not be made because there is no common headwater elevation due to the lateral slope of the terrain. For the purpose of this study, it was assumed no peak flow exchange occurs during flooding. The 1-percent-annual-chance flood on Louse Creek was found to be contained within the main channel except at the railroad bridge in Merlin and at a bridge on Monument Drive. A portion of the Louse Creek floodplain, downstream of Monument Drive, was found to be susceptible to 1-percent-annual-chance sheet flow, a condition of overland flow where elevations and directions of flow are difficult to determine. Small embayments at the mouths of tributaries also wouid experience flooding. A flood way was designed to occupy the entire width of the 1 -percent-annual-chance floodplain because any encroachment on the main channel would increase the stream velocities and aggravate bank erosion. Supercritical flow occurred at 18. cross sections in this reach. Because of the steep channel gradient, 21 additional cross sections were needed to define a continuous profile. The additional cross sections were estimated as described in the Jumpoff Joe Creek discussion. Approximately 30 percent of the 1-percent-annual-chance flood flow on Louse Creek bypasses the bridge at Monument Drive at a point 600 feet north of the channel. The flow capacity of the bridge would not allow any encroachment on the flood plain, and a floodway analysis was not attempted. The channel consisted of gravel and cobbles, with some overhanging brush, and overbank values ranged from pasture grass to dense forest. The. 1989 study by OTAK, Inc. extended the portion of detailed study for Louse Creek by adding a reach extending from approximately 470 feet downstream of Monument Drive upstream to its crossing of Granite Hill Road, a distance of 2.9 miles. The starting water 19 surface elevation for the extended reach was based on known elevations from'the effective modeling. Channel and cross section properties were surveyed between February and June of 1989. Water-surface elevations of floods of the selected recurrence intervals were computed through use of the COEHEC-2steip-backwater computer program (Reference 21). The average fall of Louse Creek throughout the study reach was approximately 90 feet per mile. This steep slope resulted in many supercritical flow conditions even though surveyed cross sections were taken at an Average interval of 600 feet along the creek. Because of the steep channel gradient; 24 additional cross sections were added to the hydraulic model. Overall, the 1 -percent-annual-chance floodplain width on the upper Louse Creek varied from 50 feet to 1,000 feet. Because of the steep channel gradient for Louse Creek, the equal conveyance encroachment option that operates on the energy gradeline was used for the floodway analysis. This method is suggested for steep waterways since it will not allow unreasonable encroachments. The resulting floodway widths varied from 30 feet to 230 feet. The flood profiles for Applegate River began at its confluence with the Rogue River. Initial water-surface elevations were based on concordant flows where backwater extended 1,180 feet up the Applegate River channel. The initial water-surface elevation for the floodway analysis was determined from a stage-discharge relation established at cross section BZ on Rogue River and does not consider concordant flow or backwater. A natural constriction at cross section Z caused a supercritical flow situation for the 0.2- percent-annual-chance flood. The change in the state of flow eaused an unrealistic shape in the stage-discharge relation, and the 0.2-percent-annual-chance elevation was, therefore, estimated by extrapolating the rating curve. Supercritical flows were also encountered at a low diversion dam at the mouth of Murphy Creek. The hydraulic model was reset using elevations derived by critical-depth computations. A direct weir formula could not be used because of excessive bypass flow around the ends of the dam. The bed material of Applegate River varies from areas of unstable gravel and rock deposits to bedrock outcrops overlain by boulders and gravel. Much of the reach is subject to change due to scour and filling of bed material and to gravel mining, Floodplain vegetation varied from pasture grass to dense deciduous brush, On the south bank at cross section AE, an upstream bank projection would cause a portion of the cross section to become ineffective for transmitting flows due tp a large eddy current. An unrealistically high "n" value was therefore assigned to reduce the conveyance in that portion of the cross section. The 1989 OTAK, Inc. analysis extended the Applegate River study from the previous upstream limit of detailed study to the Josephine-Jackson County line, an addition of approximately 5.6 miles. Known water surface elevations from the effective modeling were used as the downstream boundary for the extended modeling. Cross section properties were surveyed between Februaiy and June of 1989. Water-surface elevations of floods of the selected recurrence intervals were computed through use of the COE HEC-2 step-backwater computer program (Reference 21). No floodway was computed as a part of the 1989 analysis due to the lack of development pressure. The average fall of the Applegate River throughout the 1989 study area was approximately 17 feet per mile. With surveyed cross sections taken at an average interval of one every 3,000 feet, many critical depth statements were encountered during the initial hydraulic 20 simulations. This problem was solved by using the interpolated cross sections option of the IIEC-2 model. Approximately 21 cross sections were automatically inserted by the hydraulic model throughout this reach of the Applegate. Overall, the 1-percent-annual- chance floodplain width on the limited detail study portion of the Applegate varied from 1,200.feet to 2,700 fèet. " ' ' Initial water-surface elevations for profiles on Slate Creek reflect concordant flows of Applegate River. Backwater extended 5,500 feet up the Slate Creek channel. The initial elevation for the Slate Creek floodway analysis was determined by a slope-conveyance study through the first five cross sections of the reach (to cross section C). Concordant flow with backwater was not a consideration for the floodway analysis. Main channel bed material consisted of areas of rock and gravel deposits interlaced with boulders. The upper reach consisted of bedrock outcrops and boulders. Floodplain vegetation varied from moderate to extremely dense brush and tree growth. Waters Creek, a small tributary to Slate Creek, was studied by OTAK, Inc. in 1989 from its confluence with Slate Creek upstream for a length of approximately 1 mile. The starting water-surface elevation was computed using the slope-area method. The backwater elevations from Slate Creek at the confluence were computed based on a normal depth approximation for Slate Creek using a discharge computed from the flow/area transfer formula (Reference 16). The Waters Creek confluence is located approximately 3 miles upstream of the confluence of Hound Prairie Creek. Channel and cross section properties were surveyed between February and June of 1989. Water-surface elevations of floods of the selected recurrence intervals were computed through use of the COE HEC-2 step- backwater computer program (Reference 21). The average fall of Waters Creek throughout the study reach was approximately 50 feet per mile. This steep slope resulted in many supercritical flow conditions, even though surveyed cross sections were taken at an average interval of 300 feet along the creek. Because of the steep channel gradient, 17 additional cross sections were added to the hydraulic model. Overall, the 1-percent-annual-chance floodplain varied from 80 feet to 420 feet. Because of the steep channel gradient for Waters Creek, the equal conveyancc encroachment option that operates on the energy gradeline was used for the floodway analysis. This method is suggested for steep waterways since it will not allow unreasonable encroachments. The resulting floodway widths varied from 30 feet to 100 feet. Initial elevations for the. design-flood profiles for Murphy Creek were determined from a slope-conveyance study in the lower reach where all but the 0.2-percent-annual-chance flood were well contained in a rectified channel. A floodway analysis was not required on Muiphy Creek. Headwater elevations at the Southside Road bridge were computed using the U.S Geological Survey computer program A-526 (Reference 22). Supercritical flows were encountered at two cross sections (E and I), and the model was reset using critical-depth elevations at each cross section. The.0.2-percent-annual-chance flood overflows Southside Road near the intersection of Williams Highway. Bypass flows then merge with Applegate River and do not re-enter the Murphy Creek channel. Thè extent of road overflow was estimated because a composite stage-discharge relation could not be established at the bridge. Murphy Creek main-channel bed material consisted of loose rocks and boulders, and floodplain vegetation consisted of areas of unimproved pasturelànd, and moderate to dense brush and tree growth. 21 The flood profiles for the Illinois River began at a point 300 feet downstream from a gaging station near Kerby (No. 14377100). The stage-discharge relation developed at the gage was used to determine initial elevations. The velocity distribution in a vast pondiiig of water at Sauers Flat, upstream from the gage, is uncertain due to eddy currents and slack water. The limits of the effective velocities were then estimated until upstream.profile elevations agreed with a stage-discharge relation established at a discontinued gaging station (No. 1437000) located at the Finch Road bridge in Kerby, 3.6 miles upstream from the.initial cross section. A low diversion dam near Cave Junction (Poineroy Dam) was completely submerged by all flows and did not affect profile elevations. As previously mentioned, the computation of flood profiles continued uninterrupted up East Fork Illinois River to Sucker Creek. As the Illinois and East Fork Illinois Rivers were treated as essentially one river, cross section locations on the East Fork Illinois River refer to the starting point of the profiles, Illinois River Mile 50.0, approximately 6.4 miles downstream from the conflucnce of the Illinois, East Fork Illinois, and West Fork Illinois Rivers. Cross section data for Illinois and East Fork Illinois Rivers were obtained from photogrammetry based on aerial photographs taken on September 30,1978 (Reference 19). Bridge geometry and underwater portions of the cross sections were surveyed in January 1979. There was a wide range in main-channel bed material throughout this study reach. In the canyon area north of Kerby, bed material consisted of boulders and bedrock outcrops. In the ponded reaches of Souers Flat, bed material consisted of soft bottom material with brushy banks. ' Floodplain vegetation consisted of pastureland grass, cultivated farm lands (oftenbare during flood season), moderate to heavy brush and tree growth, and dense, deciduous brush and tree growth. Effective velocities at Sauers Flat were estimated by assigning high "n" values to reduce the conveyance in thenoncontributing areas of the floodplain. This technique was also used on East Fork Illinois River, upstream from the Redwood Highway. Extensive areas of shallow flooding were judged noncontributing because of the bank configuration upstream from eross sections M and N. . Initial water-surface elevations for the second segment of the East Fork Illinois River were determined by using the converging profile technique through five cross sections ending at cross section A. The effective channel at cross sections A and B was adjusted to exclude the embayment at the mouth of Little Elder Creek. Supercritical flows were encountered at a narrow canyon near cross section J. The hydraulic model was reset using a critical depth elevation, and the profiles continued uninterrupted through the remainder of the reach. Bed material in the commonly braided main channel consisted of large areas of unstable rock and gravel deposits. There are bedrock outcroppings and large, rounded boulders in the narrow confines of the canyons, but, generally, the entire reach appears subject to considerable movement of bed material. Flood plain vegetation consisted of some areas of pastureland, but moderate to heavy brush and trees predominated. 22 Flood profiles for the first segment of the West Fork Illinois River began at its mouth and reflect concordant flow conditions from the main stem of the Illinois River. Backwater from a 1 -percent-annual-Chance flood would extend 4,460 feet lip the West Fork Illinois River channel. The initïâfconcordant flow (or backwater) and was derived by modeling the base flood from Pomeroy Dam to the initial section at the mouth. The effective velocities at the west bank of cross section J were uncertain due to the configuration of the upstream channel. The cross section width was therefore arbitrarily reduced to exclude an eddy flow situation. The main-channel bed material consisted of large areas of irregular bedrock outcropping overlain in places by loose sand and gravel deposits. Wide gravel bars are evident where the low-water channel is deeply entrenched near one of the banks. Flood plain vegetation consisted of moderate to dense brush and tree growth. Initial water-surface elevations for the second segment of the West Fork Illinois River profiles were derived by a convergence run through a reach (five cross sections) ending at cross section A. Flow was tranquil throughout the reach; the only problem encountered was a bypass-flow situation at the Redwood Highway bridge in O'Brien. The low north bank of the ehannel upstream from the bridge allows water to flow toward the intersection of Lone Mountain Road and Redwood Highway, located 1,800 feet north of the channel. It is possible that some of the water overflows the intersection and bypasses the entire reaeh downstream from the bridge. For. the purpose of this study, it was assumed that the entire road overflow was limited to 850 feet of roadway immediately north of the bridge. This limitation was based on the position of the upstream berm which contains all flow at the approach cross section (cross section L). Main channel bed material consisted of gravel bars at sharp channel curvatures, bedrock outcrops that formed deep low-flow pools and boulder-strewn reaches that appear unstable. Floodplâin vegetation varied from pastureland grass to areas of dense brush and trees. The initial elevations for the flood profiles on Deer Creek were estimated by a convergence run through a reach with six cross sections ending at cross section A. McMullin and Thompson Greeks are tributaries that parallel Deer Creek throughout much of the central portion of this study reach. Although there is an exchange of peak flows near cross section R, it was assumed most inflow occurred at cross section P. Main channel bed material consisted of sizable areas of rock and gravel deposits which are subject to considerable movement during flood stages. Floodplain vegetation varied from pasture grass to dense brush and tree growth. Large acreages of cultivated farmland also occupy the floodplains. Flood profiles were drawn showing computed water-surfacé elevations to an accuracy of 0.5 foot for floods of the selected recurrence intervals (Exhibit 1). The hydraulic analysés for this study were based on unobstructed flow conditions. The flood elevations, thus derived are considered valid only if there are no significant changes made to the existing drainage structures or to other physical features of die channels (such as changes 23 in alignment and vegetation). 3.3 Vertical Datum " "" All F1S reports and FIRMS are referenced to a specific vertical datum.. The vertical datum provides a starting point against which flood, ground, and structure elevations can be referenced and compared. Until recently, thestandard vertical datum used for newly created or revised FIS reports and FIRMs was the National Geodetic Vertical Datum of 1929 (NGVD 29). With the completion of the North American Vertical Datum of 1988 (NAVD 88), many FIS reports and FIRMs are now prepared using ÑÁVD 88 as the referenced vertical datum. Flood elevations shown in this FIS report and on the FIRMs are referenced to NAVD 88. These flood elevations must be compared to structure and ground elevations referenced to the same vertical datum. For information regarding conversion between the NGVD and the NAVD, visit the National Geodetic Survey website at www.ngs.noaa.gov, or contact the National Geodetic Survey at the following address: NGS Information Services NOAA, N/NGS12 National Geodetic Survey ' SSMC-3, #9202 1315 East-West Highway Silver Spring, Maryland 20910-3282 (301)713-3242 (301) 713-4172 (fax) The conversion factor from NGVD to NAVD for all flooding sources in this report is +3.36 feet. Temporaiy vertical monuments are often established during the preparation of a flood hazard analysis for the purpose of establishing local vertical control. Although these monuments are not shown on the FIRM, they may be found in the Technical Support Data Notebook associated with the FIS report and the FIRMs for this community. Interested individuals may contact FÉMA to access these data. To obtain current elevation, description and/or location information for benchmarks shown on the FIRMs, please contact information services Branch of the NGS at (301) 713-3242, or visit their website at www.ngs.noaa.gov. FLOODPLAIN MANAGEMENT APPLICATIONS TheNFIP encourages State and local governments to adopt sound floodplainmanagement programs. To assist in this endeavor, each FIS report provides 1-percent annual-chance floodplain data, which may include a combination of the following: 10-, 2-, l- , and 0.2-percent-annual-chance flood elevations; delineations of the 1 -percent-annual-chance and 0.2-percent-annual-chance floodplains; and I-percent-annual-chance floodway. This information is presented on the FIRM and in many components of the FIS report, including Flood Profiles, Floodway Data tables sind Summary of Stillwater Elevation tables. Users should reference the data presented in the FIS report as well as 24 additional information that may be available at the local Community map repository before making flood elevation and/or floodplain boundary determinations. 4.1 Floodplain Boundaries To provide a national standard without regional discrimination, the 1-percent annual chance (100-year) flood has been adopted by FEMA as the base flood for floodplain management purposes. The 0.2-percent-annual-chance (500-year) flood is employed to indicate additional areas of flood risk in the community. For each stream studied by detailed methods, the 1- and 0.2-percent-annual-ehance floodplain boundaries have been delineated using the flood elevations determined at each cross section. Between cross sections, the boundaries were interpolated using topographic maps at scales of 1:2,400, 1: 4,800, and 1:62,500, with contour intervals of 2 ,4 , and 80 feet, respectively (References 8, 17, and 19). Gilbert Creek boundaries were determined on the basis of random topographic elevations taken during the field surveys. They may, therefore, not show local variations of either higher or lower terrain between points of definition. For streams studied by approximate methods, the boundary of the 1-percent-annual-chance flood were taken from the Flood Hazard Boundary Map (Reference 3). The 1- and 0.2-percent-annual-chance floodplain boundaries are shown on the Flood Insurance Rate Map. On this map, the 1-percent-annual-chance floodplain boundary corresponds to the boundary of the areas of special flood hazards (Zones A and AE), and the . 0.2-percent-annual-chance floodplain boundary corresponds to the boundary of areas of moderate flood hazards. In cases where the 1- and 0.2-percent-annual-chance floodplain boundaries are close together, only the 1-percent-annual-chance floodplain boundary has been shown: Small areas within the floodplain boundaries may lie above the flood elevations but cannot be shown due to limitations of the map scale atid/or lack of detailed, topographic data. For the streams studied by approximate methods, only the 1-percent-annual-chance floodplain boundary is shown on the Flood Insurance Rate Map. Countywide Update As part of the countywide update, floodplain boundaries were digitized from the effective FIRM and Floodway panels. USGS topographic maps (Reference 25) and aerial photography (Reference 26) were used to adjust floodplain and floodway boundaries where appropriate. The 1- and 0.2-percent-annual-chance floods were redelineated on Gilbert Creek and portions of the Rogue River using new topography with a one-foot contour interval provided by the City of Grants Pass (Reference 27). The cross section locations were digitized from the effective Floodway panels or work maps. Elevations used for the redelineation were taken from the effective floodway data tables and adjusted to the NAVD88 vertical datum. The redelineation along Gilbert Creek extended from SW Rogue River Avenue to just upstream of NW Windsor Drive, a distance of approximately 2.5 miles. Redelineation along the Rogue River extended from approximately river station 111,810 (cross section CD) to river station 158,250 (cross section D J). 25 In accordance with FEMA Procedure Memorandum 36 (Reference 28), profile baselines have been included in all areas of detailed study. Profile baselines are shown in the location of the original stream centerline or original profile baseline without regard to the adjusted floodplain position on the new base map. This was done to maintain the relationship of distances between cross sections along the profile baseline between the hydraulic models, flood profiles and floodway data tables. Floodways Encroachment on floodplains, such as structures and fill, reduces flood-carrying capacity, increases flood heights and velocities, and increases flood hazards in areas beyond the encroachment itself. One aspect of floodplain management involves balancing the economic gain from floodplain development against the resulting increase in flood hazard. For purposes of the NFIP, a floodway is used as a tool to assist local communities in this aspect of floodplain management. Under this concept, the area of the 1-percent-annual-chance floodplain is divided into a floodway and a floodway fringe. The floodway is the channel of a stream, plus any adjacent floodplain areas, that must be kept free of encroachment so that the 1-percent-annual-chance flood can be carried without substantial increases in flood heights. Minimum Federal standards limit such increases to 1 foot, provided that hazardous velocities are not produced. The iloodways in this study are presented to local agencies as minimum standards that can be adopted directly or that can be used as a basis for additional floodway studies. The iloodways presented in this study were computed for certain stream segments on the basis of equal-conveyance reduction from each side of the floodplain. Floodway widths were computed at cross sections, Between cross sections^ the floodway boundaries were interpolated. The results of the floodway computations are tabulated for selected cross sections (see Table 6). In cases where the floodway and 1-percent-annual-chanee floodplain boundaries are either close together or collinear, only the floodway boundary is shown. For the purpose of developing the 1-percent-annual-chance floodway for the Rogue River, all of the flow was assumed to be confined to the main stem channel and its immediately adjacent overbank. As agreed upon by county representatives and FEMA, the computation of iloodways on the Rogue River, downstream of Pass Creek, on Murphy Creek, and on Gilbert Creek were not a requirement of this study. The area between the floodway and 1-percent-annual-chance floodplam boundaries is termed the floodway fringe. The floodway fringe encompasses the portion of the floodplain that could be "completely obstructed without increasing the water-surface elevation of the 1- percent-annual-chance flood more than 1 foot at any point. Typical relationships between the floodway and the floodway fringe and their significance to floodplain development are shown in Figure 1. 26 1-PefiCÉNT-AAINUÂL-CHANCE RGQOPUMN AffiÂOf FUOOOPLAIN THATCOUÜ> SÉ UtfO fOR WYÉLOPMENTiriUtfWGROUND FLOOD ÉLÉVATION BEFORE ÏNCROACHMEWT ON FWOOPIAIN UNEA3ffTOER000£l£VATK>« ftfOftE ïftCROACHMENT. UX£ CD IS THE aOOO ELEVATtótí AFTíR ENCROACH MENT, . •JUttHAltGEK NOTTO ÉXCEED1 .OfOOT ÍFti REQUtí(ÉMeHT)ORÍ£SSE«AMaUNTÍ«PIC(FIEC>íy5TATE- Figure 1. FIqodway Seheraátíe 27 0£ Hl H 0 D O 3 IL Hl O z < X _[ < z> z •i <0 III o DC 111 >- I Q O o III o DC o <0 ö z 5 o o LU (0 Sin et UJ ü t >• o i l l h Q Z ölü ¡Ii | § S j U. IL S t tu i s e l e 8K FO 0 w 01 w w Ol o z ff w o z o K o UJ CO CO CO o tt u •«i r? o q -f o o o o o m o o T-" o CD en co m oo o c\j O T- T-' o o d o o ^ o ö ci <\{ -«foco in e^ N n d f f l r - ' n o i d ^ S f f l f f l f f l m r i N t f i m f f l O T - i r i ^ « cvi to w s » oi S i; (0 00 «i » o> ~ , CM CM M 0)0 )0 )0 )0 )0 )0 ) _ . n *- coN 00 «0 O) O) 0 ) 0 ) 0 ) 0 ) 0 ob "to 6 * n in ifl rt o) s ^ ri s o) r . • r -i i / i ra o l o »— flfl _ . . _ . — -- — . — — ^ di BJ T N M Ol 0 ) 0 0 0 O T- r- t- N PI A ^ ^ In «i wj uj uj c0 00 c000<7)0>0>0>0)0)00>0)0)0)0)0)0)0)0)0) . M Q) O) 5) O) £ * »" V in IO p * N J2 CT) c o © 8 © o o - o £ S 5 2 « o « - o * r » . - i o < Q < 0 i « e o c i « ( D S i n h t t d t n M d Q N N N A r . l O O a i r ^ Ol (0 O) CQ a - o o o o o o O O O O O O O O O O O O o W K" ° N J U) N CO 5 O O O CT) CO CO - § a o o _J LL Ol UJ > 01 UJ b-< o U1 -J n 0. < oh TABLE 6 Di 111 f-< a O O IL III o z < X o _J < z z <£ h-z UJ o cc UJ CL > 0 a o o IL Iii o a: o CO o z Q O o u. LU CO ~ < h-LU 111- A : LU o t >; D x l | I - D 2 5 8 t I i LU U. LL I i i ¡ 8 t a Q e s DC — H- LU < O W ¡ 3 b Hl LU > LL s < E 7 UJ F O o w ui w S lu 5 t o 6 Ui CO CO to o a: o o o o o o o o o o o o o o o o o o Ol •f O) o O) Q a> b N n o ^ ® o! w (o in o w N (\i n o N n oi oi m oi ri in «i N N — r M N o n f ' i f i o i n i n i D i D . ¿ j 0 a o o o o o o o o o o o o o o o in in cvj co tvi (D 00 I"-. B N 131 in (O N r; O 't W O (Ö <9 CO (vi in' w' ri N (vi (D oi CO* M o w t ^ ^ i n i f l i o f f l C D i D N O) ~ o o o o o_ o. o o o o o o o o o o ci cj d ei ro « (vi uj od o n w d d io ^ m • J i; „ w MM ^ - a> o o O co o O o O o o o o o o o o o o o o CD CM p o> p CO o (O CM Cvl o o CO in in co CO 00 n- o> a> CO m CO 00 r- CVI 00 -t" to" o" to" co" eo" co" r- (D in CD" o" CD in Ol CO - in m O) (o ° ™ eo m O in N Z M to : 0 rvi ir» /ri ~ i/^ K i n O O O o o o o o o o o o o o o o P) E n ^ N N Tt h- I O r N N r r P J I ^ CO v-_ LO_ LO LQ in CO 00 CO cq_ in T* if IO N Ol' r N Ol Ol" O* o" r P) Ifl «O in a in m K) (o (o to to to h- f*- f- f- f- o o O N 00 oo S O) N Tf h- N M «O 2 IT s i * * t s EL < M < CD ü D Ul -IL Ü I ^ -J ii N < < < < < < < < < < < -j s z o q. o a: < < < < < < < o < h -< Q > - g G O O LL o z UI 3 I-z UJ £ UJ • 3 z < £ O z UI o £ ui S ui t UJ a UJ u. TABLE 6 en tu I - I D O o u. UJ O z < X O T < z z < I - Z HI O a: UJ D _ >- I Q O o U . M o or R > o to CD z O o o "HI V) — < H UJ Hi I T l l i U t 2 > Q 5 > E l S 5 g t uj LL U- i l l < Z i LU LL LL > O : Q O > VI) LL al — S o w ¡ S t u UI HI > U- ä < & O M 2 LLI > LU 2 O § to CO £0 O A o o r-- o o RT " fi fi t o > t o o . a o ( M c o M O O o Q o r - o _ m « o ^ o o a > o i r ) o a i e o a a t - o o w o T - ' « t n n n i n n i n i n ' t N i n w - o i c o i n w t - ' t i n o o o o o o o o Oi *-^ CO_ CM CD Ifi »- co co" co* xi" CM o o o o o o o " l O I D N n i f l N N M M (D N N N N "C> O) O o o o a o O «5 O Cs| CJ CO en to O CM ifl 5 , X ' > < I -< Q > - < Q o u - J LL >- o z UI a < z 11) s UI a < § 2 o z LU <5 OL UJ s UJ UI a tu LL TABLE 6 ai LU H I Q O ¿ o Ui 0 2 < 1 O _J < D 2 2 < H 2 UI O OC Ui C L I O o Ui o OC D O O) (D Z • o Ö L L LU Ui ^ < I- LU LU o : U J o t > Q Í > I - Q 2 ÇOI- O LU y tu U- U- . ¡8b O í Q til U_ X — 7 rlll rfOS gsfc U J LU > U . s (OiOt t j roo lOlcOOlOONNNNNCOIDNCIt o o o o o o o o o o o o o o o o o o o o o o • ^ N M ^ N O i n o i n i o o o i n ' o o N r a n ^ o j c D i D ^ T - T - M io io io ininv) ininio io io io inino in in>ni f l i 0 in i0 (D(Di0 (D(aNNiN C M C N I C M C M C M C M C M C N I C M C \ I C \ I C \ I C \ I C \ I C M C M C \ I C \ I C M C N < C M C \ I C \ I C M Tf r r N (O « ® « ® o N ^ n 00 O) (1 q W 'î 00 I D N ri ri rt ri- ri ri ri Tf U I to to ^ N T- . « J to to W ^ « a i o¿ o"; F a O W UJ v CO Q U J U J o z Í to Q O I -O U J « to. to o o; o T F O O O C O T O T - R ^ M O O O J R ^ T M T D T D Í - N R ^ - 0 ) ( f l ( p o o N < j i o o i n ( ( i i n o i ( D " U m OT OO O O OJ OJ CO CS IO LÍL O ™ ri" CM" J C ri • TÍ" ri ri . T f T f ( f l ( < ) a o a o o g g g r i o o i o i o i S H S o o n J" to' § x < H < a > - § a o o —i LL or UJ H < O o 3 Z ¡ R O uj 5 S S gl i j V UJ D O H Z IU o a: UJ a. < o o o u_ UJ 8 O £0 U> z D O O -J u. LU CO < I- LU LLI a: l u o b. i S p P D Z 5 8 B U UJ LL Li. . >" Q 111 Ü B U , LL. KO- >" O 7 b UJ < o w S o g S LU U J > U . < Z W o pa o w LU W S U J in o 2 £ a o H O UJ w w w o oc a c- r- to o d d ^ m (OWN CO 00 oo CM CM CM CO CO CO CM CM CM -tf r- CD CO 00 <§ CM CM CM N N fl o> CO $ 2 P I S £Ö O l S s g a> co o O N N <0 00 3 CO 00 CO n T3 a) OL 0) o e-£ c o I < a >- 1 o O _1 5 Z LU 3 6 E. IU o. >• o z Ui O a LU -E U J U J a I U u. TABLE 6 LU DC if) < H 111 ' H < ' LU lil t;j CO CO q q in q en q q o CM q o lO . Ol (D q o> o> q q 00 UJ o St d d d d d d d d O o o d d d q o O O LL O >- Q <- > s i s co Ol O "t CO CM oq CM CM CD xj- CM in q co CM q q T-J CM h-* CM co" co" OÍ ib" —- in r^ O i oo" CO co". fJ •t d co* co co* co' B S g u j O) O) O) O o o O T- T— CM CM CM co CO xj- CO in CO CT) Ol o T— CM CM CM_ CM_ CM_ CO co_ CO co_ T" CO CD CO co__ co_ co__ co_ CO (O co_ co_ in in in W) _l UJ LL fcb 'l111 i< —1 II ¡ 1 1 CM M- "t. CO CM CO CO CM CM o xj- CM q q r^ q ^ CM d c\i CO Cvi co in oo' d tf d *i r^ d co K co" r^ co d lO co CM CM* CO o Ol Ol O o o O T— CM CM CM co CO co xj- V in oo Ol CT) o CM CM CM_ CM_ c i co_ co_ co_ CO CO cö CO CO CO co co_ co_ co_ in lO in in fe O W <1 _J LU LL U. T~ T" T-" " " " ^ T~ V H Z LU O >- ~ OL Q or 111 O > h- < M; ,_ CM M; Nf 00 CM cq oo CM CM q tr CM o q q h; CM d CM to cvi co* in co' d d tr d co CO T—' co" d Cfj co CM CM CO 0_ o O) O) O o o o T™ CM CM CM co co co s xf in CO Ol Ol o T— CM CM CM_ (N CNI_ CO CO co_ co co_ co_ CO co CO co CO co P) CO xr in in in in T" ©Ö LU LI OL — O 1- LU < u w _ O ID CM •t a) oo CM "J; Ol Ol CM ^ in tr r-. r- CD q CO q co CM LÚOh 5 _i UJ UJ LU M-* €0* CM CO CO •t* CO lO r- CD CD in cd ui in in r-* h-* UÍ 00* in CM in > LL >* < < a _ 5 < t¡ 7 UJ 18 ,3 82 ID • t o c a 18 ,3 82 to CO h-* to co" r-" a> CO r-T oo co" oo" r-" in CM co" T- co" CM T- LL u w LU "" . w N«o CD in r- o o o o a o o in o oo CO CM D CO o CO o o o CO o o o> o CM Q fu > bb. M ai_ r-(O co in CO fc o a> o a> o o CO co o co co in TT TT CM <0 O) CO O) t co-co CM CM t OO in UJ ' UJ U o o o o o o o o o o o o O o o o o O o O o o o o o z a> oo Ol r- r- T—• r-~ CO CO in •«r- •o h- co m CO Ol o Ol CM O) h-O ff - t M; o> o CC r-" oo" o> o o co" í " in K oo" Ca o" CM* co" s in" CO* CM s t* TT CO w to co CO - t •<* - t t X}- in in in m in 00 oo oo co 00 CO n o o <0 CD z z o • fc" £ o UJ o 11 CC o LL (0 w 8 1 OT ra LU tA o < ca o a UJ U. O X )xL •J S Z O a. a OL CO H t) > ? X >- K o OL < H < Q > - % Q O o - J LL >-o Z Iii o Z " 1LI <3 OL 111 £ Ui t ui a ui LL TABLE 6 oc UJ I -< o o S z ¡r o iu j- S í < X o < p *f ÍO h- z Ui o o: UJ o. >-I Q O •3 LL UJ ü OC Z3 O <0 (¡) z Q O O ai w f-, < r-LLJ UJ kUJ o > o xí¡ H Q Z §8 tí ZÍUJ u. u. ¡ | S 1 8 Í S ¿ _J LU U. U- CCQ o 5 UJ ui Di ^ b uj UJ UI l e í- d o to tu ^ w S ui > u. UJ o. z ? w Q o H o UJ to to to o et o q o o o o d o o CO (O o o co 01 o 0 0 0 ' - ^ o» r-, o o N O N N N M œ O © r N (i) 10 r « O W (fl q in w N m 10 ri N in N o o N 't it ri oi o N c o c o c o ^ w c o r - w c o o j o t - c M c o c o i n i « i o i n i n i n i n m i n w w i o ( û ( D ( D < û ( O B i D (M (o co co ri ri co" in n n n it m M m LO œ m N ri io in in IO N m in m o> o in T-' « N CO CO O m in in T- CT> cq in u ) \ t S m o n m <**-u)orocM'r->o>c? r-n i f M o t o i f t o o o i n o i s i f o i o i M * — r " ivi ' - - - - - - - ~ co O) CM xt CO T - 1 - -CM n f l i s o u o i N O ) CO CM O CM O co CM S (O N W (D CO r o i j - i n o o o i f u a o o w i n o i N ^ r o c o n a CMcocotocMCMCMCMinin Í < Q I O O - i LL > 0 0 0 0 0 0 0 0 0 0 0 0 S ? 9 2 - CO CO CSI_ (O CO o O, o o_ o o <*> ® .—~ n R —JT I r t tis KJ* «C RT»* #FT O T- CM CM co co o) o r N ^ co <0 00 oï o cd o m co n co oí di Ol O) Ol Ol O) O) o o o o .¡¡><0 o o C 3 u . Ä M o iSîv Q UI LL CD < < < < 3 ^ ^ S z < < < < < 5! r £ UI Y-< £ Q O ¿ o o < z > < X o _ J < z z H Z UJ o 0É UJ Q. I Q O o UJ o CC o to o z a o o ¡S&¡ BS. - I I H D Z s g t i ¿m 3 5 < o g s ¡ 8 1 5 I J LU > ~ a a CD uj m u. en ~ y b LU 1 OÎG 2 LU LU > U . I S P O o OT LU *-' W Q UJ Ui o Z g LU « t/ï W O Oí O o) o O) q q q q 10 10 q q O t • d o r- oo t- q -3- co o q d a d d 0 0 d d a ci CD co CD 00 O) O) CM CM CM (O (O q " f r ; 10 ci t 5 X a LU o É < D >- Î Û O O u . tL UJ > 0¿ <0 o z a: o ii_ I -O) LU 5 FL O O D W A Y D A T A W ES T FO R K IL LI N O IS R IV ER 1- P E R C E N T- A N N U A L- C H A N C E F LO O D W A TE R I SU R FA C E E LE V A TI O N ' IN C R E A S E ! (F EE T) I N O to in d o d o 1 F ee t A bo ve C on flu en ce w ith Il lin oi s an d E as t F or k Illi no is R iv er s FL O O D W A Y D A T A W ES T FO R K IL LI N O IS R IV ER 1- P E R C E N T- A N N U A L- C H A N C E F LO O D W A TE R I SU R FA C E E LE V A TI O N ' W IT H FL O O D W AY (F EE T N A V D ) 1. 43 2. 5 1. 43 7. 6 1 >4 42 .4 1, 44 8. 6 1 F ee t A bo ve C on flu en ce w ith Il lin oi s an d E as t F or k Illi no is R iv er s FL O O D W A Y D A T A W ES T FO R K IL LI N O IS R IV ER 1- P E R C E N T- A N N U A L- C H A N C E F LO O D W A TE R I SU R FA C E E LE V A TI O N ' W IT H O U T FL O O D W AY (F EE T N A V D ) 1, 43 1. 8 1, 43 7. 6 1, 44 2. 1 1, 44 8. 1 1 F ee t A bo ve C on flu en ce w ith Il lin oi s an d E as t F or k Illi no is R iv er s FL O O D W A Y D A T A W ES T FO R K IL LI N O IS R IV ER 1- P E R C E N T- A N N U A L- C H A N C E F LO O D W A TE R I SU R FA C E E LE V A TI O N ' > ^ CCQ 3 £ ö i ö 1 ,4 31 .8 I 1, 43 7. 6 1, 44 2, 1 1, 44 8. 1 1 F ee t A bo ve C on flu en ce w ith Il lin oi s an d E as t F or k Illi no is R iv er s FL O O D W A Y D A T A W ES T FO R K IL LI N O IS R IV ER FL O O D W A Y M EA N VE LO C IT Y (F EE T/ SE C ) S (0 t r O ci evi 1 F ee t A bo ve C on flu en ce w ith Il lin oi s an d E as t F or k Illi no is R iv er s FL O O D W A Y D A T A W ES T FO R K IL LI N O IS R IV ER FL O O D W A Y SE C TI O N A R EA (S Q . FE ET ) 17 26 1, 44 1 1, 48 6 1, 30 8 1 F ee t A bo ve C on flu en ce w ith Il lin oi s an d E as t F or k Illi no is R iv er s FL O O D W A Y D A T A W ES T FO R K IL LI N O IS R IV ER FL O O D W A Y , W ID TH (F EE T) O O Q *-® O O to r- CM T- 1 F ee t A bo ve C on flu en ce w ith Il lin oi s an d E as t F or k Illi no is R iv er s FE D ER AL E M ER G EN C Y M A N A G E M E N T A G E N C Y JO S E P H IN E C O U N T Y , O R E G O N A N D IN C O R P O R A TE D A R E A S FL O O D IN G S O U R C E D IS TA N C E1 51 ,6 00 . 52 ,2 30 52 ,9 20 53 ,6 60 1 F ee t A bo ve C on flu en ce w ith Il lin oi s an d E as t F or k Illi no is R iv er s FE D ER AL E M ER G EN C Y M A N A G E M E N T A G E N C Y JO S E P H IN E C O U N T Y , O R E G O N A N D IN C O R P O R A TE D A R E A S FL O O D IN G S O U R C E C R O S S S EC TI O N W es t F or k Illi no is R ive r (c on tin ue d) Y 2 A A A B • 1 F ee t A bo ve C on flu en ce w ith Il lin oi s an d E as t F or k Illi no is R iv er s FE D ER AL E M ER G EN C Y M A N A G E M E N T A G E N C Y JO S E P H IN E C O U N T Y , O R E G O N A N D IN C O R P O R A TE D A R E A S TABLE 6 a: UJ H-< o o UJ H o .< < X Ü t < Z) z z i z ill Ü £ UJ Q. >- i a o o UJ Ü ct Z>-o CO - Q 5 > H O Z O W Zi UJ o i l I S t D I— LU ¡ S t ] 55 < tD III F a O OT UJ W D UJ > UL Z O I--O UJ CO to CO O cn o o o o o o c M r ^ c o i o r - - o O P ) ( M ! D I N O O ) ( 1 W E O V T O ' I o o a o o a o o o a o a a o o o o o o a o o a a o to (c n to cn u) N o ^ o o co ra a si o) o r- f- f- f- f- co « N t N t o c o m n W « ! « co ai CO CT) N (O cn co in ui i n N M i f o n i o ^ n o r - T - T - N N n n r ) ^ i n i n ( 0 ( D < D N N N Mcococococococowcocococococococooooo OoDIOff lcONNON r- r- r^ r- f-- co m (D N in _ co' co' co co R cq CM CO c- CM 00 CO CO co co in co* Ol" CO r-' CO v-T id co" CO in to" co CO •«I- in m CO co CD c- t- N 00 00 CO CO 00 00 00 00 00 00 00 CM CM CM CM CM CM CM CM CM CM CM to CD CM 00 CM 00 CO cq co co in Ö Ö Ö o o o o d d d d d d co' O) CO* cd T—" in oo* CO in in CO CO co CO CO CO CO CO CO CO CO co co CO CO CO Tf in in CO CO CO c- r--CO CO «o CO CO CO CO co co co CO 00 oo 00 00 CO OO oo 00 CO CO CO 00 00 CO co" cn O) O) cn in co' CO O) co co cn o o O o o o o o o o o o o o o o o O o o o :o o o a cn CM m Ol o CM o M- co in CM CO CO r- co 00 r- ^— CO in TT •»f CM co o co CM. r-. in co_ O cn co. CM 00. i-. cq in CO co_ CM~ «T- CM" Tt-' * * T- CM o T - CM CM CM ^ r*- CM i n ^ n n o i N W t f f l N r t ' - o i c o o i O N N ^ I D N » N ( 0 0 ( \ | i n n ( \ | T - t S C O r N C O r O N i - N T - r H r O N ' - T - T - T - W N N O O O O O O O O C P O *tffl(OfflCOOlM< > O < H < Q > i Q O O —I LL UJ £ IU 3 z < S > 0 z UJ a oz 1 UJ TABLE 6 LLf cn ^ a: < Lil H < CO q co q q CO q q T— q CO q CM T— q CO o q q CN < cu w ü t z o o ó Ó d d d o d d o d d O O d d d d d d d D O >- O í > ÜL O i 5 < CO CO q CM q q co T— co CO CM co q q cn CM CM q CN O) q ÜJ H h- Q ^ cri cd 00 •f' co" iri W CN" r--' d iO O CM d cn r»-' O) CO CO ai O) ^ o ti _J LU r- oo 00 Ol o o o T— T- CM CM co co in in co co r- r- r- 00 O < oo oo oo 00 O) O) cn cr> O) O) O) O) O) cn O) O) cn a> cn cn cn cn cn Ol Z > < 3 güJ LL LL _J w i s BIS q cq q CM IO q •>t co r- °í r-; O) q ca cq oq CM t in CM r-- CN O) cd CQ -í" cd ui r-" CM r-' CO* d d d O) CO* oo" cd r-' ai cn ¿ O h r- 00 00 Oí o o o T* T— CM CM co co rí- in in co CO r- r- r- 00 «í « t oQ¡ oo 00 00 00 O) O) O) O) cn O» O) cn O) O) en O) cn CO cn cn cn cn cn cn § _J LU iL LL H Z UI o a: •o> UJ o cq (O CM IO q i- co_ T- O) co q CO CM M; in CN r- CM Q_ O) cd CQ >t e> iri h-' CM" T" co* d s d d cn* CO* CO co r^ ai cn | r- CO 00 O) o o O T— T— CM t CM cn oo CM co CM LÜOh _i LU LU LU r--° oí h-" cd r-" f-" d od oí tó oo CM CM 00 oo cn r-' CO cn r^ co" > LL >- < < LJ _ Q o: H < LU z!V o is o CO o OJ oo m 00 rt o O h-. 00 o co •Sí xl- O) «1 h- in co cn 00 If) O o": CO CM m T - o> h» co to O) O h- xj- co o CM cn ^ CM in o cn 00 ^— r-- Oí O) h- 00 r- O) O) CO, CO cn r- 00 cn h- oo Tj- CD O p q LL U UJ LU in x p o eo o o co o (O O) o t O) CM . to CO 00 CO 00 co r- in in xt cn CO O aíu g LL 00 o oo o f- O) >í VO co to to 3 s CO 00 o o h- o 00 r- to o < o 1— CM T- IO IO T- tí» co IO co v- CM oo o T— in T— in cn o D¿ P cm" co* rf IO* co" co" N co" oT ef o" T- cm" CM a> Z O Q J-o O í? d) O O LL UJ W ifi w O oí a> o 3 c N < m O a UJ ü. o X < 3 i¿ Z O CL a on to t-n > Í 3 ifc O CL E "c o o < < < < < < < < < < < < < < < < < < < < O -J < Q < a r \ VJ LL >-u 2 LU £3 ffi s in ¿ LU a ui ai LU a: ü LJU O ~3 Ü. U. 0 01 O w O < ULI UJ QÉ QÍ O < t i ES O Ou O o 1 5 Q UJ g MU- TABLE 6 ' FL O O D W A Y D A TA JU M PO FF J O E C R EE K 1- P E R C E N T- A N N U A L- C H A N C E F LO O D W A TE R S U R FA C E E LE V A TI O N IN C R EA SE (F EE T) 01 o o d o d o 1 Fe et A bo ve C on flu en ce w ith R og ue R ive r ' FL O O D W A Y D A TA JU M PO FF J O E C R EE K 1- P E R C E N T- A N N U A L- C H A N C E F LO O D W A TE R S U R FA C E E LE V A TI O N W IT H FL O O D W AY (F EE T N AV D ) 99 2. 6 99 4. 5 1, 00 0. 1 1, 00 4. 4 1 Fe et A bo ve C on flu en ce w ith R og ue R ive r ' FL O O D W A Y D A TA JU M PO FF J O E C R EE K 1- P E R C E N T- A N N U A L- C H A N C E F LO O D W A TE R S U R FA C E E LE V A TI O N W IT H O U T FL O O D W AY (F EE T N AV D ) •9 91 .7 99 3. 8 1, 00 0. 1 1, 00 4. 4 - 1 Fe et A bo ve C on flu en ce w ith R og ue R ive r ' FL O O D W A Y D A TA JU M PO FF J O E C R EE K 1- P E R C E N T- A N N U A L- C H A N C E F LO O D W A TE R S U R FA C E E LE V A TI O N R EG U LA TO R Y (F EE T N A V D ) 99 1. 7 99 3. 8 1, 00 0. 1 1, 00 4. 4 1 Fe et A bo ve C on flu en ce w ith R og ue R ive r ' FL O O D W A Y D A TA JU M PO FF J O E C R EE K FL O O D W A Y M EA N VE LO C IT Y (F EE T/ SE C ) 10 .0 12 .4 10 .8 14 .2 1 Fe et A bo ve C on flu en ce w ith R og ue R ive r ' FL O O D W A Y D A TA JU M PO FF J O E C R EE K FL O O D W A Y SE C TI O N A R EA (S Q . F EE T) 65 4 • 52 8 60 4 46 0 1 Fe et A bo ve C on flu en ce w ith R og ue R ive r ' FL O O D W A Y D A TA JU M PO FF J O E C R EE K FL O O D W A Y f E O L1J § fe 2 w (o o ° M í (D . 1 Fe et A bo ve C on flu en ce w ith R og ue R ive r FE D ER A L EM ER G EN C Y M A N A G EM EN T A G EN C Y JO SE PH IN E CO UN TY , O RE G O N A N D IN C O R P O R A TE D A R E A S FL O O D IN G S O U R C E D IS TA N C E1 O O o Ï 'O) (O oo lí) 00 z z <: 1— z Ui o oc Ui 0. >- I o o o UI o cn o CO o z o o O LÜ w ^ < H LU LU tz LU D t Z £ Q < > I- Q Z 5 o UJ Zl UJ , >- Q g g f l § f c j 5 _ I LU U_ LU O > I i —) Ml ü UJ tu Ll-ti ^ 5 o 2 o £ b U J U J > U- < & UJ o": F a o UJ Q UJ UJ O z £ Q z O B tu « CO to O a: o o o o o o o o o o o o o o o ö o o o o o o o o 0 o 0 ö o d o d o d d o d d 0 0 0 d o d d o d ' d d d d I D in in ^ r-* cö O T- T- CM O O O O T-; r- 0 Ol CD O cq T-; 0 O co in 00* O) V CO CT) CM ir? d in co' CM* in CO CM 0 O 0 • T— CM co co M- öl- m m CD co N co cn cn o> cn 01 CT) Ol CD Ol cn Ol en cn Ol Ol CT» Ol CT) cn r- 0 CT) CD 0 CO t- 0 r- T- T- 0 CO • cn o> o> Ol 0 cn cn o> cn cn o> Ol Ol O cn Ol CD Tf r- CDU") in ^ cri co tri CM' CO' O O O R - T - CM o o o 0 0 0 Ol CO 0 CD 1- 0 T— r- 0 co in 00' o> cd Ol CM in o" in V 00 CM* K in co CN 0 0 O T— CM co CO tn Kl iß so ü> O) o> cn CT) cn cn o> cn cr> O) cn o> o> o> cn Ol CT) 0 Tf -r- cq in in d o (d ei N N n XL r- 01 CM ™ 1 01 Ol T-f->* cri r-omcOT-OTj-ior-i~~mcotocDCTiintocDKiNO X >- < H < Q > 1 Q O o - J LL >-o z UJ ö < z UJ s UI 0 1 o 2 UJ ö flC UJ E UJ w a UJ u. TABLE 6 FL O O D W A Y D A T A | LO U SE C R EE K 1- P E R C E N T- A N N U A L- C H A N C E F LO O D W A TE R S U R FA C E E LE V A TI O N IN C R E A S E (F EE T) i q o o q q q o q q q q q q q q O T - < 0 < \ | o o o ^ q q 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 FL O O D W A Y D A T A | LO U SE C R EE K 1- P E R C E N T- A N N U A L- C H A N C E F LO O D W A TE R S U R FA C E E LE V A TI O N W IT H FL O O D W AY (F EE T N A V D ) 1. 03 0. 8 1. 03 9. 0 1, 04 4. 4 1, 05 1. 8 1. 05 5. 8 1. 05 9. 7 1. 06 4. 1 1, 07 0. 4 1. 07 6. 3 1, 08 1. 0 1, 08 5. 0 1. 09 0. 2 1. 09 4. 4 1, 09 9. 0 1. 10 5. 9 1, 11 1. 0 1. 11 7. 8 1. 12 5. 3 1. 12 8. 5 1, 13 2. 0 1. 13 7. 9 1, 13 9. 9 1, 14 2. 5 1. 14 5. 5 1. 15 4. 6 1 Fe et A bo ve C on flu en ce w ith J um po ff Jo e C re ek FL O O D W A Y D A T A | LO U SE C R EE K 1- P E R C E N T- A N N U A L- C H A N C E F LO O D W A TE R S U R FA C E E LE V A TI O N W IT H O U T FL O O D W AY (F EE T N AV D ) 1, 03 0. 8 1. 03 9. 0 1, 04 4. 4 1, 05 1. 8 1. 05 5. 8 1, 05 9. 7 1. 06 4. 1 1, 07 0. 4 1. 07 6. 3 1, 08 1. 0 1, 08 5. 0 1. 09 0. 2 1. 09 4. 4 1, 09 9. 0 1. 10 5. 9 1, 11 1. 0 1, 11 7. 7 1, 12 4. 7 1. 12 8. 3 1, 13 2. 0 1, 13 7. 9 1, 13 9. 9 1. 14 2. 4 1. 14 5. 5 1. 15 4. 6 1 Fe et A bo ve C on flu en ce w ith J um po ff Jo e C re ek FL O O D W A Y D A T A | LO U SE C R EE K 1- P E R C E N T- A N N U A L- C H A N C E F LO O D W A TE R S U R FA C E E LE V A TI O N R EG U LA TO R Y (F EE T N AV D ) 1, 03 0. 8 1. 03 9. 0 1, 04 4. 4 1, 05 1. 8 1. 05 5. 8 1, 05 9. 7 1. 06 4. 1 1, 07 0. 4 1. 07 6. 3 1, 06 1. 0 • 1, 08 5, 0 1. 09 0. 2 1. 09 4. 4 1, 09 9. 0 1. 10 5. 9 1, 11 1. 0 1, 11 7. 7 1, 12 4. 7 1. 12 8. 3 i 1, 13 2. 0 1, 13 7. 9 1, 13 9. 9 1. 14 2. 4 1. 14 5. 5 i 1, 15 4. 6 1 Fe et A bo ve C on flu en ce w ith J um po ff Jo e C re ek FL O O D W A Y D A T A | LO U SE C R EE K FL O O D W A Y M EA N VE LO C IT Y (F EE T/ SE C ) 7. 0 I 10 .5 9. 4 10 .7 9. 4 10 .3 7. 2 9. 5 6. 4 10 .9 8. 7 11 .4 7. 6 10 .5 8. 0, 7. 3 I 11 .1 7. 8 9. 9 9. 1 11 .8 13 .9 10 .4 8. 8 11 .9 1 Fe et A bo ve C on flu en ce w ith J um po ff Jo e C re ek FL O O D W A Y D A T A | LO U SE C R EE K FL O O D W A Y . SE C TI O N A R E A (S Q . F EE T) 60 0 40 0 44 6 39 3 45 0 41 0 58 0 44 3 55 0 32 4 40 7 31 0 46 3 33 5 44 0 48 1 31 7 45 2 35 8 , 3 87 29 9 25 4 33 8 40 3 29 7 1 Fe et A bo ve C on flu en ce w ith J um po ff Jo e C re ek FL O O D W A Y D A T A | LO U SE C R EE K FL O O D W A Y W ID TH ' (F EE T) 1 Fe et A bo ve C on flu en ce w ith J um po ff Jo e C re ek FE D ER A L EM ER G EN C Y M A N A G EM EN T A G EN C Y JO SE PH IN E CO UN TY , O RE GO N A N D I N C O R P O R A TE D A R E A S Hi 0 01 Zi o co LU O z- É CO O 12 ,8 40 13 ,5 80 14 ,0 00 14 ,4 50 14 ,8 60 15 ,2 90 15 ,6 80 16 ,2 00 16 ,6 40 17 ,0 10 17 ,3 50 . 17 ,8 00 18 ,1 10 18 ,5 60 18 ,9 10 19 ,3 30 19 ,7 62 20 ,1 76 . 20 ,5 42 20 ,8 22 21 ,3 84 21 ,5 70 21 ,6 98 ' 21 ,8 57 22 ,8 42 1 Fe et A bo ve C on flu en ce w ith J um po ff Jo e C re ek FE D ER A L EM ER G EN C Y M A N A G EM EN T A G EN C Y JO SE PH IN E CO UN TY , O RE GO N A N D I N C O R P O R A TE D A R E A S o z a O O —i l i . C R O S S S EC TI O N Ü £ Al ü c N < a i u ú i J j i i ( D i ¡ ¡ T 5 í J g z o a o i i : w i - 3 > | ) < ® » N 3 < < < < < < < < < e < < < < < < < < < < < < 5 « ¿ p 1 Fe et A bo ve C on flu en ce w ith J um po ff Jo e C re ek FE D ER A L EM ER G EN C Y M A N A G EM EN T A G EN C Y JO SE PH IN E CO UN TY , O RE GO N A N D I N C O R P O R A TE D A R E A S TABLE 6 UJ 5 o o ¿ o Uit- If IT P t-z UJ Ui a 1 a o 3 u. UJ 8 O CO Ü z a o 3 u. ¡5 p „ LU E m o t z IS gtD ill CD LU a t f i = p a o 111 ro gui f i b UJ 0 1 5 § P o ai w 8-o a: o 0 0 0 0 0 0 0 6 T- in CM o_ in crj CM co ai co" r-' CO co r- 00 00 01 T— x— co "t T-_ r-_ CM CM CM_ CM T-" 1- T-" r-" T- T- T-" O C O O O O C M O O O O ö ö d 0° 0 d 0 d d o N in (o CM" IN •t (ß (D X-; in CM a in ^ O ) ai N O ) in ci T - O O C O C M O O O J I O I - T - O O J C O ^ I - L O R - O F ß H I I I I N M O T D O I I F L O W K I O I F L I F L 5 S f f ^ «3 to CM CM CM CM CM a. a) i j £ 0 Ü c > - N < t t i ü Q U J U . O I = T ! i : J 5 <£D CQ CO £0 m £0 CD CO 03 CO CD CO Q] a 0 1 § aJ a> u. i < a I a o o Ö z UJ (!) < £ UI I z UI g UI s UJ • Ui u. TABLE 6 £ LU H < o o 3 * 9. UJ H O < z > X o UJ UJ o ¡ ä p <• CO UJ o a: UJ CL >- 0 Q O O UJ o a: O CO (3 z a o O u_ UJ w < I- UJ UJ et tu Q ib- > Q < > i 5 < 1- Q 2 §815 ¿K! I I S i 8 In 5 - 1 ÜJ LL LL > _ DC Q P S J 111 O UJ UJ UL cc — >- o t LU | S ID. • t v r N N N o ^ i O N f f l n o o n a o i i o w w i q f f l q o o o o o d o o o o a o o d o o a d o o o o ' — T— T- Tf CM CO iq oq O cq f-. cn cn iq 10 CM 01 co CM O co co a cn q CO Tf Tf 10 id co CD T- 10' r^ 0 ^ CO W" cn CM CO CO to" to f- f- f- f- f- f- r- R-» H- R-» 00 00 00 01 cn 01 cn cn O 0 0 T" *— t- 00 00 ca 00 CO 00 00 00 00 00 CO 00 CO 00 00 ca 00 CO O) cn cn O) O) o> OJ Tf 0 CM CO q co q f-; CM 0 CM TO- cr> Tf 00 q q q T-; q OJ o> co' Tf -F" Tf -F* id id CD ^ id co cn CM CO 00 0" CM" co" V r- f- f- f- f- r- CO 00 00 00 O) O) O) cn 0 O O T— V f 00 00 00 OO 00 00 «0 CO 00 CO CO 00 CO 00 CO CO CO 00 cn O) cn Ol OJ O) O) 0 CM CO to q q r-: CM 0 CM f-; q to 00 q q x- cn O) co -t id id co id CO O) CM ^ 00 00* 0" CM" co" T- R- f- F-- t- 00 CO CO 00 o> cn cn cn O O 0 •X— ^ ^— 00 CO CO 00 00 CO CO c o 00 CO CO 00 00 00 00 00 00 CO <71 <71 cn O) cn O) a; R; ¡ 0 © IN ¡ 0 N CO l*-" M-* - ° JT oi oi Ol- I B P a o M -UJ ~ GO Q UJ 0 t-o UJ w M 60 O cc o 0 0 O O 0 0 0 O 0 O O O O O CO 0 00 CO CM CD 00 IO M-0 0 O O 0 0 0 O 0 O O O O O CM t- O CO T— O) CO cn co CO 10 Cft CD_ O CO CM CD CD CM. CM Tf in CD O CO o_ CO co" T—" T- co" co" co" 00 co" CM CO 10" r-" OO" O) 00 0 CM" CM" 0" co" CM" co" •T" CO CO IO IO 10 •0 CD CO CO CM t- T™ T- t— T- o o i o m o i o o i o i O i o i o o o o o „ f ^ _ . „ o o „, . ( D f f l Q t c n n ^ o o N t i o n o f w S i i i ' H W c o ^ ^ N . t w n O) ocog § x > 2j m m m m m cn o oc a < I Q U D 1 U I L ( ! ) X ^ O ^ - I 5 Z O L Ö K W O. O O O O O O O ^ O O O o O O O 0 0 0 £ < Q > - I Q o o —I LL >• o z UJ • o z Ul -I O o o Ui o oc o CO o z 5 o 3 UJ 9 er ¡st q O Ol CO in in q in in q q q in - Q $ > O o CO q q CM co iq CO CM Ol T-CO Ol Ol Ol Ol Ol Ol CT) Ol Ol Ol Ol Ol Ol CD Ol Ol Ol Ol Ol Ol Ol Ol Ol Ii. Lu i_ > Q t: <> o o r» C\| r; ^ " f r CM CO Ol * q « - xf v- r^ in O o CN CM q r» q cd r»' r»' CO CM CO lö CD CO o" co" CO co CM* co in oi cri co ^ if" d fgfc 5 Mw T- \— T— CM CM CM CM CM CM co CO CO CO co t if- m CO CO co r» Ol Ol Ol Ol Ol Ol Ol Ol Ol CD CD cn Ol cn Ol Ol CD CD Ol Ol Ol Ol CD Ol cn CD LL u. > -Ol o o> 1- < o o I-. CM T- r^ ^ CM CO CD M; <— O) T— if T- ^ vn q q CM CM O v- Q <0 N ed rj m !0 CO CO oo r^ ri CO cd h-- CM* CO m" O) O) cd T-I •»t d f- ^—' %— ^— ^— CM CM C4 CM CM CM CO co CO co co M" m CO co CO r--3 Ui Ol Ol Ol CD Ol Ol CD Ol CD Ol Ol CD CD Ol O) Ol Ol Ol Ol CD Ol Ol Ol CD UJ Ol LL D: — 7 hw Tt q. CO o co vn Ol CD oa q oq o CO in CM UJ CO f- co 00 CO o Ol CM CO CO oi Ol* o CM T" ^ cö CM*-T-' co f-' CO T-' in d •5 _J UJ ^ t—' T— T— — T— t— \—1 TT" T— >— r- T- ^— < — T" T- T UJ UI > ü, ä < tu ^ Ol CO CM O co o CD CM CO o ö o o o O o o o o o o a — UJ in C m o in 'S- in Ol co in o CM CO. o o o o o o o s q o o o S o o^ t- a K u_ oo Ol fc o oo 5 in: CM co CO TJ- m CM o CO f f CO in CO m in W> co t CO m CO t •f. m tj- UJ o 00 00 Ol CO oo CO Jt O co o Ol o o o .o o a o o o o o o Q o o CO h» CO CM co o t^ to CO CO T- CO Ol vCO oo in h-CO fc t CO 00 "t o o £ « CJ (O^ CO CD Ol Ol Ol CD cn. cn o CM 5 X > N < OQ O a UJ LL CD X S z O Q. a ql 00 «o o Ii u O o o o O Q Q Q Q Q Q O a o Q Q o a Q a Q a a Q o Q1 •—• OL O < < Q < Q O O LL o 5 z Ol s H Z UI E UJ o < z < >-o z UJ o cc UJ £ UJ * ui o UJ Li_ Q£ UJ > a: Ui Z) o o 2 S w o < Ui UJ £ Di o< ¡fS H H op ü f e UI § Z o I S 0- Q UJ y CO < o ^ TABLE 6 a: U J H < O O S* E O S ¡ X Ü 0 a o o L L L U ë O « (D z Û o O - I ' - L L UJ CO ~ < I - UJ LU OL LU O > O ^ > ElS rí uj ¡8ln g y LU LL LL d a UJ T I Di — >-o -, h LU < O W Isti l i PO o w LU CO S UJ U J o Ë -o UJ co w « o Di O CD TO q q O CM CD o d d ò ö o d- OCOCJlh-OCNCOO COCnh-h- o o o o o o o o o o o co q O CM CD R-" M CM R- Q O T- r- CT) OO O Q Q Q CM q q cd d CM cri r- O ^ T-T 03 CM CO d CO od I—• CM CN CN cM CO co "T co IO co co r-O) O) O) CT) O) CT) CT) CT) O) O) en CT) en CT) CT) f^ q q CM cd f"- O) CM o o O 1-o> o> o> CT) q T ^ q q c N C N q q f ^ q ^ c o • w ra co ai ^ T- o N r to oi N i N i N M N W ' f ^ ^ i f i i n i n OlOioioicnœcDaicnoicna) q oo 00 r- CO T- O q CM CM oo q r- q q q q d d TJ CM CD d CN CD co CT) V co" T— co O) r-Y— T— ^— 1— CM CM CM CM CN co TT TT TT CD in CD CD h-O) en CD en CT) CT) CT) en O) en O) en en en e» O) O) en en (D 00 N R TF N O N T •«t -rí t^ pi ° co* cd cd if ° q CM q oò co O) o LO o o O o o o m i n c o c o j r o ) » - o ) C M « ï < g o O M r h S r i t N N N p N ^ CM" CM" 0 0 R-" ^ ^ ^ ^ ^ 3 a co co io T-T M If O) O) (û - S O) O) co io o ' r f ^ n i N t o o a ) L o i o c N i ^ c o q t n t n h --t «o CM CM CM co N u i n ^ o o ^ ^ « O O O O C J C J O O O O O O H» (FL ( D O 1 ) N Q ( Í if 0)_ O) 00 q. CM Tf c CM" CO" CO "»T U) CO S N 0 0 O ) O ) o o o o o o o o T - O) T -o K io io" co •T T- * - ' • Ç\L CO T}- w < F F L Ü Ü U J I I C ) I - - > I ¿ - I 5 Z O Ú . A D Í W O O O £ flj ^ <¡) CL < l-< Q > - Î Q O o Li. * U J U J Cd o U J H < a: HI H I Q o o LL 111 o z < X % << iS I Q O 3 u. LU 2 O « o z 5 o o _ J u. UJ 60 — < t-LU LU a: UJ o t > Q x l 1 58C JUJ g i i 1 s t 5 - J LU LL LL I I £ ° ¡J LU ? Li . U J O z: g Q UJ W O or o q in qtD o iq q o d o' o" o d d o o n d o N N r - i q o d o d d "I ^ t ^ h ^ "1 t "R r. m m i J O M p i o d ^ i r i i i i N d p ) R- T - T - N t M n ^ T F ^ i f ^ l o i o inf--CMinr---'fincoinT);T-;ococo ' in in b pi pi' d o rt' in in n o T - t - T - N w f l i f T f t - j f i r i n 8 N N t- in R-; CM U> R-t- iri in ^ K l f l K l i t r O n l l ) O O * - T - T " T- T~ J w' pi n ri d - r- « w co !? 3 3 (O N m to leaving natural vegetation in place • reducing surface water run-off with vegetative planting and keeping natural water retention areas. Shrink-swell and road building hazards can be safe-guarded with adequate design and site preparation. An important task is to ensure that builders and developers are made aware of the soil properties of the site or area before planning, and construction begin. The soil mapping and inventory of this section should serve as adequate generalized information regarding the hazards of soils within tile UGB area. Site specific analysis of the soils should be encouraged in sensitive areas where soils are exposed to weathering and/or where slopes are steeper than 35% percent. The relationship between steep topography, soils and natural vegetation becomes increasingly delicate as the percentage of slope increases. This delicate balance is strongly affected by human actions in developing or preparing sites for development. Extensive excavations for cut and fills, premature removal of natural vegetation and the additional load placed on a hillside by development can lead to earth movement in the form of slope erosion or mass movement. Grants Pass & Urbanizing Area Comprehensive Plan Last Revision: 11/4/2009 Page 5 - 12 EXHIBIT^ 5.30 FLOOD HAZARD PURPOSE The purpose of this section is to describe the history of flooding in the urban growth boundary area, identify the flood-prone areas, evaluate the degree of hazard, and describe the appropriate safeguards from flooding. HISTORY OF FLOODING The earliest recorded flood in Josephine County occurred in 1861. Since no subsequent flood has surpassed the magnitude of that flood, it has been chosen to represent the "100 year flood." (Army Corps of Engineers) Flood magnitudes are rated by their chance of annual occurrence. A "100 year flood" is assumed to have a 1% chance of occurring each year. A" 1 year flood" is assumed to have a 100% chance of occurring each year. These are mathematical relationships that ignore the natural variables which affect the weather. Table 5.30.1 depicts the major floods of the Rogue River at Grants Pass during the last 120 years. TABLE 5.3.1 Major Floods of the Rogue River at Grants Pass Nov. - Dec., 1861 175,000 cfs ("100 year") Feb., 1890 160,000 cfs Feb., 1907 60,500 cfs Nov., 1909 . 70,000 cfs Feb., 1927 138,000 cfs Dec., 1942 54,400 cfs Dec., 1945 70,000 cfs Jan., 1948 59,900 cfs Oct., 1950 65,400 cfs Jan., 1953 77,000 cfs Dec., 1955 135,000 cfs Dec,, 1964 152,000 cfs ("50 year") Dec., 1972. 82,500 cfs Dec., 1974 96,400 cfs Grants Pass & Urbanizing Area Comprehensive Plan Last Revision: 11/4/2009 Page 5 - 13 The table reveals that there is little mathematical order to the occurrence of floods. Floods of similar magnitude can occur within a few years of each other, such as the Februaiy 1907 and November 1909 floods and the October 1950 and January 1953 floods. Floods of relatively great magnitude can occur within a decade of each other, such as the December 1955 and December 1964 floods. The long range forecasting of flood occurrences would seem able to predict only that floods will occur at random intervals and at varying magnitudes. FLOODPRONE AREAS The Rogue River flows through the approximate center of the Urban Growth Boundary area. There are five confluent creeks that discharge into the Rogue River within the UGB. Map 5.30.3 shows the UGB and the floodprone areas (shaded). The actual areas of special flood hazard are identified by the Federal Emergency Management Agency in a scientific and engineering report titled "Flood Insurance Study" with the accompanying Flood Insurance Rate Maps for Josephine County and Incorporated areas effective date December 3,2009, and any revision. These areas were subject to flooding during the 1964 flood. Note that flood levels protruded into the channels of Gilbert and Allen Creeks. This phenomenon occurs because the flood level of the river is at a high elevation and the flood waters of the creeks are effectively "dammed" by river water. Water always seeks mean sea level and, therefore, is always flowing to the ocean. When the creeks are dammed by the river, then they overflow their banks upstream and water flows in sheets over the surface of the land in its relentless search for sea level. Therefore, the confluent creeks of the UGB area are also prone to a flood hazard relative to the magnitude of the river flooding. DEGREE OF FLOOD HAZARD The degree of flood hazard is measured in terms of loss of life and property. No deaths from flooding in the Grants Pass area are noted in the literature. Flood warnings usually occur in time to prevent loss of life^ as people are able to move out of the floodprone areas. However, real property and improvements such as buildings are subject to the forces of flooding water. A quote from the Postflood Report. December 1964 Flood (Army Corps of Engineers) can dramatically relate the damages to property by flooding. "One of the major factors causing excessive damages during this flood was the enormous quantity of debris brought into the channel from every source. This debris collected behind bridges resulting in the complete destruction of several, and major damage to nearly ever other bridge across the main stream. It also contributed to residential damage all along the river, knocking buildings from their foundations or smashing into walls." Within the UGB area, residential areas on both sides of the river were flooded up to 8 feet. (Postflood Report, 1964. Army Corps of Engineers). The city sewage treatment plant sustained damages estimated at about $65,000. The Postflood Report did not summarize the value of residential damage but did state the values of the home flooded to be between $30,000 and $50,000 per home and estimated the average residential damage to be $900 per residence. Exhibit 5.30.2 shows an aerial view of the flooding of 1964. Grants Pass & Urbanizing Area Comprehensive Plan Last Revision: 11/4/2009 Page 5 - 14 EXHIBIT 5.30.2 Aerial View of 1964 Flood Grants Pass & Urbanizing Area Comprehensive Plan Last Revision: 11/4/2009 Page 5 - 15 SAFEGUARDS FROM FLOODING Safeguards from flooding that can be implemented at the local level are warning systems, land use regulations and the Federal Flood Insurance Program. Warning Systems The Army Corps of Engineers operates a computer simulation model for the hydrological characteristics of all the significant water drainage basins in Oregon. That simulation model can predict fairly accurately when a flooding river system will "crest", or reach its highest flooding elevation, and what the elevation will be at the "crest." That information is provided to all radio stations and local emergency units like the police and national guard. If elevations of floodprone areas are known by recognized landmarks, then people and mobile property can be removed from the anticipated flooding area. An emergency evacuation program that employs local police, fire department and other civic groups can help facilitate the relocation of persons and property from a floodprone area. Land Use Regulations The City and/or County can regulate the use of land within known floodprone areas. The regulations can range from allowing no development in floodprone areas to allowing any type of development in conjunction with federal floodplain laws. The regulations can also selectively designate floodprone areas as public open space for parks, wildlife areas and floodways. Public open spaces would allow active public use of the land and enhance the attractiveness and livability of the Urban Growth Boundary Area, while reducing future potential losses of life and property from flooding. Land use regulations can also be used to set aside land areas for the detention of storm water. Those lands, such as wetlands, grassed waterways, and woodlands, may reduce flood elevations of the frequent small floods, and prevent future increases in flood heights of these frequent floods. Flood heights have the potential for increase in proportion to the increases in urban level development in the Boundary area. Urban development increases the amount of storm water runoff by increasing the area of impervious surfaces such as streets, driveways, parking lots, and rooftops. If the natural storm water detention areas of the UGB area are converted to impervious surfaces by urban development, then the storm water runoff will flow more rapidly over the surface, into stormdrains and on to the creeks and the river, thereby increasing the elevation of the flood and/or decreasing the elapsed time between the beginning of the flood and the flood "crest". Land use regulations can provide equitable transfers of land use intensities for each land use type from the floodprone areas and storm water detention areas to other less sensitive areas. For example, a proposed residential development in an area with potential for storm water detention may be encouraged to preserve the detention area through incentives encouraging the transfer of density. The potential number of dwelling units that can be built on the detention area may be transferred to the remaining buildable area of the land that has less potential for detention. In this way, the developer retains the revenue potential of the development, and may even reduce the costs Grants Pass & Urbanizing Area Comprehensive Plan Last Revision: 11/4/2009 Page 5 - 16 of development by clustering. The community retains an open space and a storm water detention area, reducing the hazard of flood, and reducing the size and cost of storm drain lines. Federal Flood Insurance Program The catastrophic nature of flooding and the relatively localized effect of intermittent floods caused the insurance industry to find it financially unfeasible to provide flood insurance at reasonable rates. Increasingly, the federal government was requested to act to protect and safeguard private property. Legislation was passed in 1956, but money was never appropriated to implement the program. Further studies resulted in Title XIII, National Flood Insurance, part of the Housing and Urban Development Act of 1968 (Public Law 90-448) and the Flood Disaster Protection Act of 1973. Together these acts created an enormous federal subsidy in an effort to provide reasonable flood insurance at affordable rates. In effect, the federal government underwrites private insurance companies and subsidizes insurance premiums by paying the difference between the "affordable" premium which is charged to the policyholder, and the actuarial or "true cost" premium. The actuarial premium would be the rate charged to the policy holder if the insurance policy were written based on the statistical likelihood of flooding combined with the potential losses resulting from flood damage. In exchange for the reduced rate, property owners, through state and local governments, agree to adopt appropriate land use control measures to bring the risk of public and private losses to acceptable levels. In 1979, work was completed on the Flood Insurance Study for the City of Grants Pass. A similar study was completed for Josephine County in 1980. Initial use of this information will be to convert Grants Pass and Josephine County to the regular flood insurance program of the Federal Insurance Administration. Streams in the area requiring detailed study were identified at informal meetings held in January 1978, between the U.S. Geological survey, the Federal Insurance Administration and the City of Grants Pass. The Rogue River and Gilbert Creek were studied by detailed methods. Although the Gilbert Creek flood plain is quite small, the density and intensity of streamside development justified establishing the flood zones by detailed methods. Most recently, the Federal Emergency Management Agency completed a new Flood Insurance Study for Josephine County and Incorporated Areas dated December 3,2009. A primary purpose of the National Flood Insurance Program is to encourage state and local governments to adopt and enforce land use practices within flood prone areas to the degree necessary to reduce the risk to acceptable levels as set forth in the program. Each Flood Insurance Study therefore includes a map which delineates the extent and location of areas subject to periodic inundation and differentiates between the floodway and 1 00-year and the 500-year flood boundaries. In order to provide a national standard without regional discrepancies, the 100-year flood has been adopted by the Federal Insurance Administration as the base flood for flood management and insurance purposes. The 500-year flood is indicated simply to make communities aware of additional areas in the community with perceivable levels of flood risk. Map 5.30.3 illustrates the approximate location of the floodway, the 100-year and 500-year flood boundaries. The actual areas of special flood hazard are identified by the Federal Emergency Management Agency in a scientific and engineering report titled "Flood Insurance Study" with the accompanying Flood Insurance Rate Maps for Josephine County and Incorporated areas effective date Grants Pass & Urbanizing Area Comprehensive Plan Last Revision: 11/4/2009 Page 5 - 17 December 3, 2009, and any revision. The principal result of the Flood Insurance Study is the Flood Insurance Rate Map. This map contains the official delineation of flood elevation lines. The level of flood risk and therefore insurance premiums are determined from this map. Grants Pass & Urbanizing Area Comprehensive Plan Last Revision: 11/4/2009 Page 5 - 18 MAP 5.30.3 Floodway and 100-Year Flood Plain for Grants Pass Urban Growth Boundary Grants Pass & Urbanizing Area Comprehensive Plan Last Revision: 11/4/2009 Page 5 - 19 The National Flood Insurance Program divides the area of the 100-year flood into a floodway and floodway fringe. The floodway is the actual channel of a stream or river plus any adjacent flood plain areas that must be free of encroachment to allow the 100-year flood to flow freely without substantial increases in flood heights. Maximum federal standards establish a limit for flood height increases of one foot, provided that hazardous velocities are not produced. The area between the floodway and the boundary of the 100-year flood are termed the floodway fringe. Exhibit 5.30.4 depicts the relationship among the stream channel, floodway, floodway fringe and 100-year floodplain. EXHIBIT 5.30.4 Floodway-Flood Plain Schematic Floodway fdnge Flo Encroachment- 100-year flood plaitt v- Stream channel s >d .e l eva i i o ß w 11 irt M Miigfe: B|rçroacl inerït - a ;. y* o A-reä òfiflòod p l & . ^ ^ ¿ ^ S j ' j o n before- for d o v e i ^ p m m ^ m w H \ ^ o^.flood; plain Line C D is {hc^h.oodilovàLÎion àiierïMcroàçii.înOîif " Jïpno Insurance rates are based on the degree of flood risk. In order to establish actuarial insurance rates, the Federal Insurance Administration has developed a process to transform the data depicted in the floodway schematic drawing, into flood insurance criteria. That process includes the determination of flood hazard factors and flood insurance zone designations for each flooding river or creek. The city has adopted a floodplain development ordinance that is in compliance with the National Flood Insurance Program. The city ordinance identifies buildable land within the 100-year floodplain as the floodway fringe. The floodway is not considered buildable.. Development on the buildable land (floodway fringe) must be constructed so that the first floor level of the building is a minimum of one foot above the 100-year flood elevation. This regulation anticipates that once the floodway fringe is fully encroached upon by development, the actual flood elevation will be raised one foot above the 100-year flood level. Development in the floodway must demonstrate that encroachment will not raise the flood elevation beyond the one foot maximum above the 100-year Grants Pass & Urbanizing Area Comprehensive Plan Last Revision: 11/4/2009 Page 5 - 20 flood elevation. The federal regulations require that a qualified surveyor determine the degree of displacement. The displacement of floodway water by the proposed floodway development may adversely affect other development on the adjacent floodway fringe, which usually precludes floodway development in an urban area. Grants Pass & Urbanizing Area Comprehensive Plan Last Revision: 11/4/2009 Page 5 - 21 Federal Emergency Management Agency Washington, D.C. 20472 RECEIVED JUNO 9 2009 CERTIFIED MAIL IN REPLY REFER TO: RETURN RECEIPT REQUESTED 19P-N CITY OF GRANTS PASS June 3, 2009 The Honorable Len Holzinger Mayor, City of Grants Pass 101 NW A Streeel Grants Pass, Oregon 97526 Dear Mayor Holzinger: Community: City cf Grants Pass, Oregon Community No.; 410108 Map Panels Affected: See FIRM Index This is to formally notify you of the final flood hazard determination for your community in compliance with Title 44, Chapter I, Part 67, Code of FederalRegulations, On September 27, 1991, the Department of Homeland Security's Federal Emergency Management Agency (FEMA) issued a Flood Insurance Rate Map (FIRM) that identified the Special Flood Hazard Areas (SFHAs).the areas subject to inundation by the tiase (1 -percent-annual-chance) flood in the City of Grants Pass, Josephine County, Oregon. Recently, FEMA completed a re-evaluation of flood hazards in your community. On January 23t 2009, FEMA provided you with t*r6liminmy copies of the Flood Insurance Study (FIS) report and FJRM thai identify existing flood; hazards In your community. FEMA has addressed all comments received on the Preliminary copies of the FIS report and FIRM. Accordingly, the FIS report ¡and FIRM for your community will become effective on December 3,2009. Before the effective date, FEMA will send you final printed copies of the FIS report and FIRM. Becausc the FIS for your community has been completed, certain additional requirements must be met date of this letter. Prior to December 3,2009, your community is required, as a condition of continued eligibility in the National Flood Insurance Program (NFIP), to adopt or show evidence of adoption of standards are the minimum requirements and d o ^ S s u f ^ S ^ S y S S ! o r local requirements of a more stringent nature. It must.be emphasized that all the standards specified in Paragraph 60.3(d) of the NFIP regu lations must be enacted inaiegallyenfbrcea b le document. Th is incl Udes adoption o fthe current effective FIS report and FERM to which the regulations apply and the other modifications made by this map revision. Some of the standards should already have been enacted by your community in order to establish eligibility in the NFIP. Any additional requirements-can be met by taking one of the following.actions: Amending existing regulations to incorporate any additional requirements o EXHIBIT 2 Communities thai fail to enact the necessary floodplain management regulations will be suspended from participation in the NFIP and subject to tlie prohibitions contained in Section 202(a) of the Flood Disaster Protection A c t o f l 9 7 3 as amended. In addition to your community using the FiS report and FIRM to manage development In the floodplain, FEMA will use the FIS report to establish appropriate flood insurance rates. On the effective date of the revised FIRM, actuarial rates for flood insurance will be charged for all new structures and substantial improvements to existing structurés located in the identified SFIIAs, These rates may be higher if structures are not built in compliance with the floodplain management standards of the NFIP. The actuarial flood insurance rates increase as the lowest elevations (including basement) of new structures decrease in relation to the Base Flood Elevations established for your community. This is an important consideration for new construction because building at a higher elevation can greatly reduce the cost of flood insurance. To assist your community in maintaining the FIRM, we have enclosed a Summary of Map A étions to document previous Letter of Map Change (LOMC) actions (i.e., Letters of Map Amendment, Letters of Map Revision) that will be superseded when the revised FIRM panels referenced above become effeetive. Information on LOMCs is presented in the following four categories: (1 ) LOMCs for which results have been înc/udçd on the revised FIRM panels- (2) LOMCs for which results could not be shown on the revised FIRM panels because of scale limitations or because the LOMC issued had determined that the lots or structures involved were outside the SFHA as shown on the.FIRM; (3) LOMCs for which results have not been included on the revised FIRM panels because the flood hazard information on which the original ' déterminations were based is being superseded by new flood hazard information; and (4) LOMCs issued for multiple lots or structures where the determination for one or more of the lots or structures cannot be revalidated through an administrative process like the LOMCs in Category 2 above. LOMCs in Category 2 will be revalidated through a single letter that reaffirms the validity'of a previously, issued'LOMC; the letter will be sent to your community shortly before the effective date of the revised FIRM and wili become effective 1 day after the revised FIRM becomes effective. For the.LOMCs listed in Category A, we will review the data previously submitted for the LOMA or LOMR request and issue a new determination for the affected properties after the revised FIRM beeomes effective. The FIRM and FIS report for your community have been prepared in our countywidc format, which means that flood hazard information for all jurisdictions within Josephine County has been combined into otie FIRM and FIS report. When the FIRM and FIS report are printed and distributed, your community will receive only those panels that present flood hazard information for your community. We will provide complete sets of the FIRM panels to county officials, where they will be available for review by your community The FIRM panels have been computer-generated. Once the FIRM and FIS report are printed and distributed, the digital files containing the flood hazard data for the entire county can he provided to your community for use in a computer mapping system. These files can be used in conjunction with other thematic data for floodplain management purposes, insurance purchase and rating requirements, and many " other planning appfations^Qopies ofthe digital f lesj>r papejeppjeso fthe FIRM panels may be obtained by c a H i n ^ ^ ^ ^ ^ ^ ^ ^ ^ ^ ^ ^ É l ^ f e ^ ^ M ^ ^ ^ ^ B l n addition, yoiir community may be eligible for additional credits undèr our Community Rating System if you implement your activities using digital mapping files. 3 If your community is encountering difficulties in enacting the necessary floodplain management measures, we urg&you to call the Director, Federal Insurance and Mitigation Division of FEMA in Bothell, Washington, at (425) 487-4682 for assistance. If you have any questions concerning mapping issues in general or the enclosed Summary of Map Actions, please call our Map Assistance Center, loll free, at 1- 877-FEMA MAP (1-877-336-262-7). Additional information and resources your community may find helpful regarding the NFIP and floodplain management, such as The National Flood Insurance Program Code of Federal Regulations, Answers to Questions About the National Flood Insurance Program, Frequently Asked Questions Regarding the Effects that Revised Flood Hazards have on Existing Structure, Use of Flood Insurance Study (FIS) Data as Available Data, and National Flood Insurance Program Elevation Certificate and Instructions, can be found on our website at http://www.noodmaps, fema.gov/lfd. Paper copies of these documents, may also, be" obtained by calling our Map Assistance Center. Sincerely, William R. Blanton Jr., CFM, Chief Engineering Management Branch Mitigation Directorate Enclosure: Final Summary of Map Actions cc: Community Map Repository Mr. Tom Schauer. Senior Planner, City of Grants Pass FINAL SUMMARY OF MAP ACTIONS SOMA-2 Community: GRANTS PASS, CITY OF Community No: 410108 To assist your community in maintaining the Flood Insurance Rate Map (FIRM), we have summarized below the previously issued Letter of Map Change (LOMC) actions (i.e., Letters of Map Revision (LOMRs) and Letters of Map Amendment (LOMAs)) that will be affected when the revised FIRM becomes effective on December 3, 2009. 1. LOMCs Incorporated The modifications effected by the LOMCs fisted below wiff be reflected on the revised FIRM, in addition, these LOMCs will remain in effect until the revised FIRM becomes effective. LOMC Case No. Date • Issued Project Identifier Old Panel New Panel NO CASES RECORDED 2. LOiViCs Not incorporated The modifications effected by the LOMCs listed below will not be reflected on the revised FIRM panels because of scale limitations or because the LOMC issued had determined that the lof(s) or structure (&) involved we re. outside-the Special Flood Hazard Area, as shown on the FIRM. These LOMCs will remain in effect until the revised FIRM becomes effective. These LOMCs will be revalidated free of charge 1 day after the revised FIRM becomes effective-through a single revalidation letter that reaffirms the validity of the previous LOMCs. LOMC Case No. Date Issued „ Project Identifier Old Panel New Panel LOMA 97-10-389A 10/24/1997 \S£RDEEN.SUHOIV, BLOCK D. LOT 4- 1714 SW 3ROWNELL 41Ò1060003C 41033C0511E LOMA 98-1Q-086A 02/06/1998 l375,fVW PROSPECT AVENUE " TAX LOT 801, »ORTION OF SECTION.7, T36S, R5W.W.M. \ 4101Û6QÛÛ2C 41033C0504E LOMA 00-10-056A - 12/15/1999 • • /VESTGATH SUaOlV. BLOCK1, LOTS Ö26 COTTONWOOD STREET 4101080003C 41033C0511E LOMA O2-10-129A 01/09/2002 .OWER RIVER MEAJDOWS SU8QIV PHASE 2, JOT 68-2156 CHAMBERS LANG 4155900237D 41Q33C0S11E LOMA 03-10-0134 A 01/09/2003 3AROEM VALLEY ESTATES SUBDIV, LOT 11 - MOB GARDEN VALLEY WAY 4155900237D 41033C0511E LOMA • 03-10-0141Ä 03/13/2003 • 1436 SE ROGUE DRIVE - PORTION OF GOVT -0*4, SECTION 21. TMS. R5W. WJll. 4101080004C 41033C0516E LOMA 03-10-043QA 05/01/2003 7371 NORTH APPLEGATEflOAD - PORTION PF SECTION 20, T37S, RSW 4155900329B 41033C0702E. LOMA 04-10-0474X 04/14/2004 aARKSI DE ESTATES, LOT 4 — 1126 SW- JNCOLNROAO . .41Q10B0003C 41Ó33C0511E •": ' - " ; - - '¿ - - • 5/21/2Û09 Page 1 of 2 SOMA-2 FINAL SUMMARY OF MAP ACTIONS Community: GRANTS PASS, CITY OF Community No: 410108 LOMC Case No. Date issued Project Identifier Old Panel New Panel LOMR-F 04-1Q-0627A 10/13/2004 A/EE WILLOW SUBDIV, LOTS Z-3 - 1215 4 1211 RONWOOD DRIVE 4155900237D 41Q33C0511E LOMA 05-10-0849A 11/10/2005 1111 LUZON LANE \ 4101080004C 41033C0512E LOMA 08-10-0194A 04/03/2008 EAST PARK SUBDIVISION, BLOCK A. LOT 0 - i 174 ACACIA LANE 4101Q80004C 41033C0512E LOMA 08-10-0014A 35B DONEEN LANE - Sac 24, T3flS, RfiW, W.M. 41559002370 41033C0511E 3. LOMCs Superseded The modifications effected by the LOMCs listed below have not been reflected on the Final revised FIRM panels because they are being superseded by new detailed flood hazard information or the Information available was not sufficient to make a determination. The reason each is being : superseded is noted below. These LOMCs will no longer be in effect when the revised FIRM becomes effective. LOMC Case No. Date Issued Project Identifier Reason Determination Will be Superseded LOMA 02-10-047A " 11/28/2001" 643/645 BALSAM ROAD - PARTIUON PLAT 1996-015, PARCEL 1; LOWER RIVER MEADOWS SUSOIV, LOT 4 2 - 6 4 " A 1. Insufficient information available to make a determination. 2. Lowest Adjacent Grade and Lowes! Finished Floor are below Ihe proposed Base Flood Elevation. 3. Lowest Ground Elevation is below the proposed Base Flood Elevation. A. Revised hydrologie and hydraulic analyses. 5. Revised topographic information. 4. LOMCs To Be Redetermined The LOMCs in Category 2 above will be revalidated through a single revalidation letter that reaffirms the validity of the determination in the previously issued LOMC. For LOMCs issued for multiple lots or structures where the determination for one or more of the lots or structures has changed, the LOMC cannot be revalidated through this administrative process, Therefore, we will review the data previously submitted for the LOMC requests listed below and issue a new determination for the affected properties after the effective date of the revised FIRM. LOMC Case No. 1 Date • Issued .. Project Identifier Old Panel - New Panel i NO CASES RECORDED !• • - V - — — — .5/21/2009'- URBAN AREA PLANNING COMMISSION September 23,2009 6:00 PM Council Chambers 1. ROLL CALL The Urban Area Planning Commission met in regular session on the above date with Chair Berlant presiding. Commissioners Arthur, Kellenbeck, Fitzgerald, Richardson/Fowler and Fedosky were present. Also present and representing the City was Interim Community Development Director Angeli Paladino, Senior Planner Schauer, and Associate Planner Glover. 2. 1T£MS FROM PUBLIC: None. 3. CONSENT AGENDA a. IMPUTES i. ^Minutes of September 9, 2009 Commissioner Kellenbeck stated, I'm abstaining from one of those. Do you want to break it out or do you want me to just vote with the group and aOctain from the one? Chair Berlant stated, why don't w ^ o ahead and break that out. That was the Twisted Pines, so moving the second Findings of Fact Twisiea Pines p h a s ^ . Let's.deal with all the other matters on the consent agenda. Commissioner Fitzgerald stated, on p a g ^ O of our packet tonight, in the discourse that we talked about on the text amendment, I found no reference to the que^ion of notification to the Commissioners, yet 1 asked that question, "Had the Commissioners been notified?" I do n^d my response about it, but I don't find the question on the record. Interim Community Development Director AngelPPaladino did state that they had been mailed twice, and this doesn't appear in here either. So, I'm wondering why that aWn't show up. Chair Berlant stated, why don't you just make an amendment to it to add that to it and then that will complete it. Commissioner Fitzgerald stated, actually page 48, where aoNwt midway through it says that I stated according to Commissioner Ellis, they have not seen this and didn't know anything about it as of this evening. Well, that's the answer, but the question is missing. So the question was, "Have^te Commissioners been notified about this text amendment and Interim Community Development Director Angeli-Peladino stated that they had been mailed it twice. The answer there, as I was saying... that change 1 would like to see pbi in. Board of County commissioners, yeah. Commissioner Richardson asked, you did not consider the statement by cN sufficient? Where she says, "I was wondering if the County Commissioners crosscheck won't happen? Was there addition to that question? Commissioner Fitzgerald stated, yes there was. 1 made a specific point as to whetHNc the text amendment had been notified and I asked the question, "Had it been notified to the County Board of Comml^ioners so that they were aware of what was being taken up." ^ ^ Commissioner Richardson stated, I understand, but isn't that what the crosscheck included^V Commissioner Fitzgerald stated, no, it wasn't because the text amendment dealt with the res idem« requirement being changed from the Urban Growth Boundary and so that was what was part of it. Chair Berlant stated, so, I suggest that if you ask that the minutes be amended to insert the question thaW>u asked then that would cure that. Commissioner Fitzgerald stated, that's what I'm saying is, it needs to be amended to include the question whicrSwas, "Had the Board of County Commissioners been notified of the text amendment changes that were proceeding a n a ^ r. Urban Area Planning Commission September 23^2009 ' missioner Kellenbeck ahead of that as d at least been noticed that the EXHIBITS 7d UAVtlpnP characteristica^ased on the shape of the parent parcel, natural features, including trees. Condition A (2) not applicable, conation A (3) for the reasons stated in subsection (b) which is better achieve the public purpose allowing a lot arrangementTNat represents a more efficient use of land. Criterion 4, satisfied based on the section that says... based on purpose. ItlSjks about accomplishing the same purpose and so I would relate that back to 3 (b) for the purpose of achieving a ofetter public purpose and design. (She asked another Commissioner off microphone about combining and the conversion was inaudible) I'll combine that with a motion to approve the tentative pian for the subdivision. On item 15, for t n ^ h e d building on proposed lot 2, to allow that to remain until the time of building permits for that building only but tkleave the condition the same for the building that would otherwise split the property line between lots 3 and 4, chqd to add to that condition on the shop for parcel 2 that the standard code language that we've seen in the past afcout "if no building permit is pulled, then a demolition permit and removal of lhat building would be necessary within tñtó given timeframe so that there isn't an accessory building with no residence after a certain number of years wrKch I believe is... is it 3 years? Does that sound right? Two or three years? The revision to condition 1 (b) about th^CUE being allowed to go directly straight through the hammerhead. Commissioner Fitzgerald seconded the motion. ChatoTterlant asked for further discussion. Commissioner Fedosky stated, chair Berlant, I agree wittvyou on your recent reflections on needing to have flexibility in these areas but I guess my expectation is that there woulcNae at least one or two of these that jump out as being close to being satisfied. The drawings here for me contrast cleaKy, the not satisfied nature of these 3, that there are alternatives, and it can be developed, and there's nothing unique rMhe shape of these lots. It's just a better idea, and the lots will sell better, and a tree is saved. 1 agree with you but not tcSthe degree that everything in front of us is stretched on so far. I think that begins to deviate from our purpose a n d \ j r scope as a body. Just my opinion Commissioner Kellenbeck stated, I have one amendment to my motion and thaNtfas to include a condition that require an on-site turnaround for vehicles exiting a garage on parcel 4. Commissioner Fitzgerald stated, 1 amend the second. Chair Berlant asked for further discussion. Seeing none, he called for a vote. ^ ^ MOTION ded and tedosky Commissioner Kellenbeck moved and Commissioner Fitzgerald seconded a mot ion as ar the vote resulted as fo l lows: "AYES": Berlant, Arthur, Kellenbeck, Fowler, and Fitzgerald. "NAYS' and Richardson. Abstain: None. The mot ion carries. ii. 09-40500004 & 09-40500006: Flood Hazard District - Special Purpose District Map Amendment and Development Code Text Amendment Proposal: Special Purpose District Map Amendment and Development Code Text Amendment to adopt the new Flood Insurance Study (FIS) and Flood Insurance . Rate Maps (FIRM) issued by the Federal Emergency Management Agency (FEMA) dated December 3, 2009. The proposal amends Article 13 of the Development Code related to the flood hazard district. In addition, the narrative in Element 5 of the Comprehensive Plan is updated to reflect the new FIS and FIRM maps. Applicant: City of Grants Pass Planner: Lora Glover Chair Berlant stated, at this time we will begin the hearing with a Staff report followed by a presentation by- the applicant, statements from persons in favor of the applicant, statements by persons in opposition to the application, and an opportunity for additional comments by the applicant and Staff. Once that has occurred, the public comment portion will be closed and the matter will be discussed and acted upon by the Commission. Chair Berlant asked if there is anyone present who wishes to challenge the authority of the Commission to hear this matter. Seeing none, Chair Berlant asks if there are any Commissioners who wish to abstain from participating in the hearing or declare a conflict or a potential conflict of interest. Urban Area Planning Commission .September 23, 2009 16 [Commissioner Arthur made a comment off microphone. The comments were inaudible] Chair Berlant stated, I would say that certainly I received notice that my property might be affected by this amendment. In reviewing it, actually, I don't think this amendment has any effect on my property so I don't think there is any either actual or potential conflict for me. Commissioner Arthur stated, and I have the same thing. I also received a notice and being up on the hill behind here I don't think I'm in any imminent danger of anything. Are there any Commissioners who wish to disclose discussions, contacts, or other ex parte information they have received prior to this meeting regarding the application. Seeing none, Chair Berlant states that in this hearing the decision of the Commission will be based upon specific criteria which are set forth in the Development Code, all testimony given which apply in this case are noted in the Staff Report. If anyone would like a copy of the Staff Report, please write that in a note to me and one will be provided to you. It is important to remember that if you fail to raise an issue with enough detail to afford the Council and the parties an opportunity to respond to the issue, you will not be able to appeal to the Land Use Board of Appeals (LUBA) based on that issue. Chair Berlant states the hearing will now proceed with a report from Staff. Associate Planner Glover stated, good evening again. As we start tonight there is a lot of information in the packet and I'll try to guide us through it. We are doing several parts to this. There are various components. We're looking at the Flood Hazard District Zoning Map Amendment, the Special-Purpose District Map Amendment, and the Development Code Text Amendment. This procedure is a type IV. That is a Planning Commission recommendation forwarded to the City Council for their'final decision, and that hearing is set for November 4,1 believe it is. It will be at six o'clock. Tonight this is a recommendation decision, it is not a final decision for you. The proposal again includes amending the purpose of the Special-Purpose District Map for the flood hazard to adopt the flood insurance study volume 22. Those are referenced throughout the material as the FSI, and the flood insurance rate map, the FIRMs for Josephine County. The amendment also includes adopting a new section 13.200, the flood hazard district as the Development Code, and then also to update Element 5 of the Comprehensive Plan referencing the new FIS and FIRM with an effective date of December 3, 2009. The City of Grants Pass as you "know participates in the National Flood Insurance Program. By doing so our residents are able to obtain flood insurance from this program. The Federal Emergency Management Agency which is FEMA has recently completed the process of updating our current 1991 FIS and FIRM maps. The purpose of the new FIS is to revise and update the information on the existence and severity of flood hazards in Josephine County to include the incorporated areas of Cave Junction and the City of Grants Pass. The County is also in the process of adopting the City map, they are not separate maps anymore. So as we gó through any expansions later on to the City we will have already adopted those maps. We won't have to go through the process again to pick up small segment along the way. I'll mention this again but, the flood hazard areas are for the Rogue River and also for Gilbert Creek so Commissioner Arthur that's probably why you picked up that notice. It was off of Gilbert Creek. On June 23, 2009, this was in sense a sudden notice, we've been working through this process but we knew the study was happening, but on June 3, 2009 FEMA mailed their letter of final determination instructing the City that the new maps and study must be adopted to maintain our participation in the flood insurance program by no later than December 3, 2009. Adoption of the FIS and FIRM requires that the Element 5, the Comprehensive Plan, be updated; All of these documents are interrelated. So what one references, we all need to blend it together, and so with the new FIS and FIRMs we need to make sure we're referring to the December 3, 2009 version. In addition, the new FIS requires the update of the Development Code, specifically standards of paragraph 60.3d of the National Flood Insurance Program Regulations. Most of this pertains to the crawl space requirements and how those are constructed. This is an example. I'm not sure how well the audience can see. On the left is the existing FIRM map showing the light blue as the flood plain and then the floodway in the dark blue. Vou can see on the new maps there is a difference... we're looking at the Webster-Lincoln road area around the All Sports Park also. The floodway fringe or the floodplain as a lot of folks noticed there is an elevated area in the center that is still clear. It's outside of that hazard, and the floodway stays pretty close to the existing. This is just one example. We are finding a lot of areas where the impacts are (ess on property owners though there are few areas that they have little bit moré of a flood hazard noted on them. I would encourage at this point... I do not have air of the maps available on the computer here, down here at this office, hut you aré welcome to come into our office and we can print out a map for you of your Urban Area Planning Commission .September 23, 2009 17 specific lot to compare. We do have the large maps here tonight. Commissioner Richardson stated, the question is I guess, in the old version of the existing flood maps everybody in the blue area and everybody in the pale yellow area was required to have flood insurance in the old map or the existing one, and now in the new one people that used to have to have flood insurance don't need it but these people in floodway fringe are now going to be required to have flood insurance. Is that the basic impact of this? Associate Planner Glover stated, required... generally it will be coming to their lender. If they have a loan on their property their lender would require it. Part of the difference to is, again we're showing a lot of area in the new map that is now outside of that flood hazard, so based on these maps, the lenders for those home sites would not necessarily require the flood insurance. It also gives an opportunity now for people that may not have been reflected in the flood hazard under the old map that maybe now are reflected in it, they can get the insurance today under today's standards, which those might change if they have to prove elevation later on. So it gives an opportunity for those folks to cut their insurance people. Commissioner Richardson stated, right. 1 guess what I'm saying is, at this point people who have mortgages based on this new one, are likely to get a notice from their lender that says, "You're going to have to have and pay for flood insurance." If you own a house in this that you own free and clear, you need to go think about purchasing flood insurance. So we've sent out notices... Associate Planner Glover stated, we sent out over 1000 notices to people within the flood hazard or Rogue River and Gilbert Creek. But again, even under the existing maps those folks within the flood hazard, their insurance providers more than likely require them to have flood coverage. So it's not having flood coverage is a new requirement, it's just some people may need it now but didn't before or now in this particular map, there's probably quite a few... some of these new subdivisions off of Lincoln area that no longer require it based upon these maps. So the requirement to have flood insurance is not a new requirement. Commissioner Richardson stated, right, I understand that. Just that in looking at them there is a dramatic difference between those two before and after. Associate Planner Glover stated, it's much better in this example for most of the people in the middle that are outside of that flood hazard now Commissioner Richardson interrupted, exactly. It's the folks that are now in the floodway fringe who thought they were secure, who possibly have an issue. Associate Planner Glover stated, we can overlay these maps in the office and this is what I was trying to show too. It's little bit hard, I keep losing my arrow. As you come up to this area, that's about the same area that's here. This scale is a little bit off. So this floodway fringe has not moved dramatically. Most the time it has reduced down. It's just that it's reduced down here in the center. All of this center is out, where before it was inside. So we're finding that on the majority, the impact is less severe for most properties. But again I would encourage people to come to the office, and we can show them the before and after. I just thought it would be a little bit too much color to lay them on top tonight. I did want to give you a little perspective though. I got these copies of these maps in 1964 courtesy of the County. This is Webster and Lower River Road area. You can see the Water and how it inundated the land through that area in and crossed over onto South River road side. This is West Park street. Actually this is East Park street. This Is East Park Street running down through here and then West Park Street there. This is Rogue River Highway and then you can see M Street. The next one is my favorite map. This is my mother's house off of Rogue Drive. This is the Portola area, down in the corner. This is Herrick coming down, and then Lela coming through. So we have one of my neighbors here that didn't have water in his house in the 1964 flood. So the NFIP , the National Insurance Program has been in existence since the passage of the National Flood Insurance Act of 1968. We have over 700 communities in the Pacific Northwest participating in the program. In 1973 flood insurance became mandatory as a condition of any federal or federally related assistant. This generally related to... for the loans. FEMA conducts hydrologic and hydraulic analysis and prepares the flood plain maps and provides those to the participating communities. The combination of insurance and mitigation through floodplain management provides a powerful combination to help safeguard our residents. The plane managing and via ordinances and development standards is a mitigation vice because insurance cannot do the work alone. Participation in the NFIP brings a number of benefits to the community. Residents are able to purchase and renew their flood insurance policy. Urban Area Planning Commission .September 23, 2009 18 The City of Grants Pass participates in the community rating system, it's a voluntary rating system that qualifies our residence for lower flood insurance premiums as a result of education outreach and measures to reduce flood losses. FEMA will also come through and inspect our records and we report to them, I believe on an annual basis of the information we provide. NFIP insurance provides an additional $30,000 from FEMA for reconstruction to meet current standards. This is specifically helpful on older homes that may have built to code originally. If we are suspended from the program, we face the following consequences: Existing policies will not be renewed. No federal grants or loans for building may be made in identified flood hazard areas. Federally backed mortgages such as Fannie Mae, Freddie Mac, or FHA also require NFIB insurance. So that could limit our housing industry. No federal disaster assistance may be provided to repair any buildings located in the flood hazard areas unless we are participating in the program. In addition, if we are suspended and then go back to get reacted again, there is a 30 day waiting period for flood insurance. This could be critical if we don't respond in time... December 3. It would be into January or February possibly before we would have flood insurance again and that's normally our bad season, our wet season. Non-NFIB insurance companies will not cover more than one claim for disaster. Non-FIP providers are hard or difficult to find and are often very expensive such as Lloyd's of London. They had a very small high risk pool with high premiums. As we go through this with the different amendments we have to address the criteria for us, and this is how the development code for zone map amendments... Section 4.033 of the development code is specific to zone map amendments. We needed to acknowledge this though we did not feel it was applicable because it's not related to a specific zone, however the adoption of the new FIS and FIRM maps will result in a map change to the flood hazard. A special district. As you are aware we have several Special-Purpose Districts in the Development Code. Again the amendments affect properties along Gilbert Creek and the Rogue River. Section 4.044 of the development code, flood hazard district map; this is satisfied. The flood boundary floodway is established by FEMA. The flood hazard district map may be amended only by FEMA. Upon receipt of authorization from FEMA the Director shall begin administering the flood hazard district as designated by FEMA. Back again to our directive on June 3, 2009, we received or were mailed their letter of final determination instructing the City to adopt the new FIS and FIRM maps by December 3, 2009. Section 4.103 of the Development Code Proposed Amendment is consistent with the purpose of the section and article. This criteria is determined be satisfied. The proposal amends section 13.200, the flood hazard district, and is consistent with the purpose statement. The amendment will consolidate various flood ordinances in the municipal code and the development code. It will provide additional terms and definitions for the flood hazard, bring construction standards for crawlspaces and below grade crawlspaces into compliance. One of the goals of this amendment will bring the municipal code and various resolutions and ordinances that have been passed over the years will consolidate all of that into the development code so we don't have various documents to research through, or that may have conflicting or outdated language in. So it will all be rolled into this amendment.. The final packet before the City Council will have a draft ordinance available for them noting which documents are going to be updated or canceled at that point. I'm losing the word that I wanted. So, at this point, it's Staff recommendation that you make three motions recommending approval to the City Council. The first is to amend the Special Purpose District Map for the Flood Hazard District by adopting the current insurance study, the FIS volumes 1 and 2, and the Flood Insurance Rate Maps, the FIRMs for Josephine County and incorporated areas effective date December 3, 2009, issued by the Department Homeland Security's Federal Emergency Management Agency (FEMA). The next motion would be the Urban Area Planning Commission recommend that the City Council approve the proposed amendment section 13.200, the flood hazard district of the City of Grants Pass development code to be consistent with the National Flood Insurance Program and the Oregon Model Code Provision. Finally, the third motion be the Urban Area Planning Commission recommend that City Council approve the amendment to update Element 5, the Comprehensive Plan, specifically section flood hazard 5.30, to reference the new FIS and FIRM maps effective December 3, 2009. I'll jump back up real quick because we didn't really discuss it in the Staff Report, the Oregon Model Code Provisions. This is just kind of the guide that was developed via the department DLCD. It consolidated all the federal and state regulations into kind of a checklist for us to go through to make sure that we had all the parts that we needed to do which is what was rolled into the amendment for article 13. After that I'll open it up to questions for you. Chair Berlant asked if anyone wanted to speak to this issue. Seeing none he closed the public hearing portion and turned it over to the Commissioners. Urban Area Planning Commission .September 23, 2009 19 Commissioner Richardson stated, when we just taik about Gilbert Creek and the Rogue River obviously we have left out other of the major feeders of the Rogue River. I'm thinking of Sand Creek and Allen Creek and all of the rest of them, and those folks in Atlanta that are seeing this traffic flooding. I know in many places flooding happens someplace else and it can be a perfectly sunshiny day where you are and melting in and around the Crater Lake that can cause flooding to occur here in Grants Pass. Is that the only kind of situation that FEMA deals with or do they deal in just addressing these areas with an idea of a sudden downpour that is so severe that literally the ground cannot handle it? Interim Community Development Director Angeli-Paladino stated, I don't know that we know that answer. Associate Planner Glover stated, I do know flood insurance is available to all of us in a sense because flooding happens. It could be an example like that, or an erosion or drainage problem. So the flood insurance program... and if we do this part of it, it still provides the opportunity for all of our residents to achieve flood insurance. Commissioner Richardson stated, right, I guess though as far as FEMA is concerned, it's to handle a flood event in the rivers as opposed to a.... What is it? Atlanta got, 24 inches of rain in just a matter of 4 or 5 hours -- a tremendous downpour — so they had flooding in places that they had never had flooding before. Chair Berlant stated, I'm not sure but 1 think FEMA covers all of those and this is just trying to look at the most likely areas and more mandate that there'll be coverage or at least protect themselves if they're going to. Commissioner Fitzgerald stated, this is the concerns of the federal agencies that will require like FHA and all of the programs, Rural Housing programs and others that all fall under FHA guidelines in the secondary market which is Fannie Mae and Freddie Mac, all of them will require these be applied and that's why it really is a perfunctory type of administrative deal. If we don't have... the City does not adopt them, those programs are not available to our citizens. It's just that simple. Commissioner Fowler asked, and am I to understand that even if you're not living in one of the designated shaded areas you're still eligible for the federal subsidiary or whatever the group insurance is? Associate Planner Glover stated, yes you can still obtain federal insurance. The studied areas is... when again like a lender would come through and say, "You are in a designated flood area, you have to have it if you want our loan.", but otherwise they obviously recommend a lot of times that people that are concerned or on a smaller tributary should have the flood insurance. Commissioner Fitzgerald stated, it doesn't change the flood certs that you can obtain from a surveyor which will give you 1 foot... the bottom of the being 1 foot above the flood stage. So anybody that has those flood certs will have to make sure that nothing is changed on the new maps. So I would think it would.... Is there something that we are going to send out as a City? A website or something that alerts people to the fact of having those flood certs perhaps reevaluated to make sure they are okay with the new maps? Associate Planner Glover stated, well, we will be sending out another notice on this application — I believe a decision notice with more information there and their contacts information too. Again, we sent out over 1000 notices for all along that hazard area along the Rogue River. We'll be noticing the insurance companies. A lot of them are already aware of it. They're getting their new maps on their own and they have started calling and also on this. Commissioner Fitzgerald stated, I was just wondering about the flood certifications. A lot of times homeowners don't realize they have them. Especially if they bought a new home that was done by the developer who built the homes, put that in and had all of the crawjspaces flood certified like I did at Schaeffer's. We flood certified every one of those because of it. We should perhaps put something in there to have them contact the person that did that if they have a flood certification to make sure it hasn't changed. It would be a terrible shame if they had a flood certification they thought, and with this new map it's not exactly correct or doesn't work for them just to have them check it. Not that we are trying to inherit.some liability but it might be a good idea just to tell them if they had a flood certification that they should have it reestablished or rechecked to make sure it's still effective- Commissioner Richardson stated, you know it seems to me that the monthly newsletter that comes out with the sewer news would be a wonderful opportunity to remind everybody to have it checked. Urban Area Planning Commission .September 23, 2009 20 Chair Berlant stated, and it looks like you want 3 separate motions on this Associate Planner Glover? Commissioner Fitzgerald stated, I'll make those motions if you want Commissioner Berlant. Associate Planner Glover stated, you can do it separately or if you're going to approve all of them then 1, 2, and 3 of those items... Commissioner Fitzgerald interrupted, do you want them separate Associate Planner Glover? (Associate Planner Glover stated, if you just at least reference those) Do you want me to read a, b and c? (Associate Planner Glover stated, that's fine) I make a motion that we would first recommend that the Urban Area Planning Commission recommend to the City Council to approve the amendment of the Special-Purpose District Map of the flood hazard district by adopting the current flood insurance study FIS volumes 1 and 2, and flood insurance rate maps (FIRM) for Josephine County Oregon and incorporated areas, effective date December 3, 2009 issued by the Department of Homeland Security's Federal Emergency Management Agency (FEMA). Do you want me to do all of them? Okay. B. It is recommended that the Urban Area Planning Commission, I would make a motion that we would recommend the City Council approve the proposed amendment to section 13.200 Flood Hazard District of the City of Grants Pass development code to be consistent with the National Flood Insurance Program (NFIP) and the Oregon Model Code provisions. C. I make a motion that the Urban Area Planning Commission recommend that the City Council approve the amendment to update Element 5 of the Comprehensive Plan; specifically the section under Flood Hazard 5.30 to reference the new FIS and FIRM effective December 3, 2009. Chair Berlant called for a vote. MOTION Commissioner Fitzgerald moved and Commissioner Richardson seconded the mot ion to recommend approval for the above noted amendments (A, B, and C) as stated and the vote resulted as fo l lows: "AYES": Berlant, Arthur, Kellenbeck, Fedosky, Fowler, and Richardson. "NAYS": None. Abstain: None. The mot ion carries. iii. 09*40500002: Comprehensive Plan Text Amendment Propo&qh - Proposed amendment to the Comprehensive Plan adopting a new Urbanization Element Applicant: >viCity of Grants Pass Planner: senior Planner Schauer Chair Berlant stated, at this time we wilh^egin the hearing with a Staff report followed by a presentation by the applicant, statements from persons in favoSqf the applicant, statements by persons in opposition to the application, and an opportunity for additional comments b^t^e applicant and Staff. Once that has occurred, the public comment portion will be closed and the matter will be discussed and acted upon by the Commission. Chair Berlant asked if there is anyone present who wisn^to challenge the authority of the Commission to hear this matter. Seeing none; Chair Berlant asks if there are any CoKjmissioners who wish to abstain from participating in the hearing or declare a conflict or a potential conflict of interest. Sb^ing none, are any Commissioners who wish to disclose discussions, contacts, or other ex parte information they ra^e received prior to this meeting regarding the application. Seeing none, Chair Berlant states that in this hearing thetiecision of the Commission will be based upon specific criteria which are set forth in the Development Code, all testimon^iven which apply in this case are noted in the Staff Report. If anyone would like a copy of the Staff Report, please writNbat in a note to me and one will be provided to you. It is important to remember that if you fail to raise an issue witfissnough detail to afford the Council and the parties an opportunity to respond to the issue, you will not be able to appeaNo the Land Use Board of Appeals (LUBA) based on that issue. Chair Berlant states the hearing will now proceecN(ith a report from Staff. Senior Planner Schauer stated, I'll talk in a minute on procedural things for this are little bit difhs^nt so I'll talk about that as part of the presentation in terms of appeals. This is a continuation of the hearing on the Uhs^inization Element Urban Area Planning Commission .September 23, 2009 21 before the Planning Commission and poreqtially sooner. The room will probably be a little fuller than the floodplain tonight. 8. • ADJOURNMENT There being no further business to come before the Commission, Chair Berlant adjourned the meeting at 9:30 p.m. Gary Berlant, Chair Urban Area Planning Commission Date ' These minutes were prepared by contract minute taker, Wendy Hain Urban Area Planning Commission .September 23, 2009 35 ö • GO O on on O 2 > _ I t-t ^ Ö î ^ d o 9 n ë a m r o Q (T> Ö BS: 9 on O S " n O P Í? O O C/ì i er «TÖ O) p * S- I B- £ 8 a . EP s Pb O íü o 3 O.. 5 er ß " B Ü 3 • o •n a ff Eh cn tù co 5 tù t/3 ai cr n> 3 n> P- O p hd O p Q- P N> Cu n VI ET pi U p H tr crq" t=: o rî p cr p tî» p n> H n n O o a-B" O A - cr ta tr p N ^ A - W 1' O ^ P H A - S l/l r+ H O & n> g'- ^ n> i-t w B. O r+ P B-n> C s- 3 p O O O- w o a p a- D o o X FÙ s a a n o E 3 H B 0 a> 1 r+ PT > o p c r n T n p. H) H r 2-3 CT fî rt « n «» O tí" 3 m A OÛ O hT CL n P í I. Ci. cg ^ n> tt. O F Ht O o O- 0 l-t p p n a> O h3Í O p O O p t d a O n cyi n o p en n • ë O) P o p . > c 33-TJ fl) ¡33 § > mCD 1 , 1 Q] S Ss 2 « CO"D ÍTT, £ 7 X m 3 CD cd 3 O a g i o S o 2 . = Oc o co' (D3C « Q cl-q O C D > c T J Q ) ¡ E N O > .^OJ zrmg 01 — 3" O ' O CD gioSI" OCQ W a o g o m 3 m 3 = « 3 I . 0} -n CD if) 3 tf^ M tt 3 3 "DnC-i ( Û q O GOq O ® Q] o uïï- 3 g- foo CL™ O^ V ^ C K (Q O C O O O 3 • O d o S « X -r&k CD 03 S . Q . I p f l i l m® g c S ¡$¡D <5 - « CD Q.ZT -n UJ _ j 3 £ CQ Q]^ 3 O Ol g o 3 Q] m 3 «a -n° o — 3 . C D 5 - C L C Q ^ O (QCD ° a Q-a 03 q-OO Q O Q3 o c 3. 7T* J ^ - * • ~ , . , , ^y— J^ ... Gïr^yejnâmen-i- S^c-4'on * 2 i 2cQ ^lood •i-ir: V /-I J • .L ! \ .'J A , ™ n Art S\ } i ¡KO. i M L u r i  i o r • n i r , [ J f r . ^ / o f - o a r 'yeu U ) e , ^ a u e , h o d hfflr9> S i n a i . - ¿ k l U o m e ( A ^ f t S G-pr"' L 1 W / _qjc¿ c é í & J ^ c j u j L l cÇu I h r a IqvO u n C f W L f , h o t ^ H 4 s h r u . U S b A / a / ? ( . rt / • ^ / O l ' / U f « — _ f W aH t , r i n c o r n i v.S û v i m o n n f o W I 4 : |A o ; U fl h c C u d ú M í d . T-P ^ K i s firA^gftU, d i o r n ^ S ôUf propel fe™. A l l i e d J h . _ C L J m u f ï k ' T J L Ö ; H i n „ , _ , f . ^ / ^ VH ( t o x r e i - X I t u « H fee n u e < " ^ J ^ j È û ô à i X i t o A ö f Q ^ o r ^ j X I i W - / J ^ n Tâ ôt sué ~4!ft-r _ _ — — „ - f b h c o ^ H / a h u ¿ t h k i £ h s q r a n a , . ¡ h j L m ^ Ljrs (Aß U n ^ bup.d CAJ^ kUn -i-cfi Ö4 - k e Panics f$-tl>\L noir rn ôur Oft/x. (\)e are q ^ U , ^Qnœ^ Ikil UJOJLM. c \qQS»L U À Q t v t f d s l x i p . ~P(/Xsz p,