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dc.contributor.authorBeck, Joseph D.
dc.contributor.authorBergevin, Logan
dc.contributor.authorGuenthner, August
dc.contributor.authorMangin, Matthew
dc.contributor.authorWood, Hunter
dc.contributor.authorJol, Harry M.
dc.contributor.authorGoettl, Martin
dc.descriptionColor poster with text, images, charts, photographs, and graphs.en_US
dc.description.abstractThe Algodones dune field, is located south-east of the Salton Sea in Southern California. The dune field is divided into two sections composed of a protected wilderness area (north) and a larger area of public land (south), which is managed by the Bureau of Land Management. The Algodones Dune field is a highly complex geomorphic and spatially diverse dune system. Dune sediments in the region are derived from aeolian (wind) processes and are remnant sediments from Ancient Lake Cahuilla. On March 5th, a ground penetrating radar (GPR) grid was shot consisting of horizontal and vertical lines on the Eastern Crescentic dune region located in the northeastern portion of the Algodones dune field. Two GPR systems were used in collaboration with San Diego State University.en_US
dc.description.sponsorshipUniversity of Wisconsin--Eau Claire Office of Research and Sponsored Programsen_US
dc.relation.ispartofseriesUSGZE AS589;
dc.subjectDune migrationen_US
dc.subjectStratigraphic nnalysisen_US
dc.subjectGround penetrating radaren_US
dc.titleAlgodones Dune Migration and Strigraphic (sic) Analysis Using Ground Penetrating Radar, Southern Californiaen_US
dc.title.alternativeAlgodones Dune Migration and Stratigraphic Analysis Using Ground Penetrating Radar, Southern Californiaen_US

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