Re-examining Shoreline Elevations at Ancient Lake Chewaucan in Central Oregon, USA

dc.contributor.authorKendrick, Brianna
dc.date.accessioned2019-06-28T18:07:03Z
dc.date.available2019-06-28T18:07:03Z
dc.date.issued2019-06
dc.description40 pagesen_US
dc.description.abstractThe Chewaucan Basin in Eastern Oregon provides a unique environment for pluvial lake geomorphology research, as lake oscillations in the last 30,000 years have formed shoreline features that wrap around the basin. Over the last century, multiple scholars have published works describing shorelines of the ancient lakes using various elevation data collection methods, including USGS topographic maps, Digital Elevation Models, and survey equipment. By revisiting accessible shoreline sites and measuring elevations using a TopCon RTK GPS I found that topographic maps vary between 0.2 and 11 meters off and Digital Elevation Models, which are developed using the historical topographic maps, vary in accuracy between 2.5 and 12.25 meters, when compared to the TopCon measurements. These discrepancies reveal that historical elevation data needs to be evaluated when studying the geomorphology and other issues in the basin.en_US
dc.identifier.urihttps://hdl.handle.net/1794/24747
dc.language.isoenen_US
dc.rightsCreative Commons BY-NC-ND 4.0-USen_US
dc.subjectPaleogeomorphologyen_US
dc.subjectGreat Basinen_US
dc.subjectUSGSen_US
dc.subjectGeographyen_US
dc.titleRe-examining Shoreline Elevations at Ancient Lake Chewaucan in Central Oregon, USAen_US
dc.typeThesis / Dissertationen_US

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