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dc.contributor.advisorJol, Harry M.
dc.contributor.authorHilgendorf, Zach
dc.contributor.authorMorrison, Sean
dc.contributor.authorAdams, Hannah
dc.date.accessioned2016-03-23T20:08:39Z
dc.date.available2016-03-23T20:08:39Z
dc.date.issued2015-04
dc.identifier.urihttp://digital.library.wisc.edu/1793/74436
dc.descriptionColor poster with text, maps, images, and charts.en
dc.description.abstractLake Superior has undergone a number of lake level phases that have resulted in the formation of beach ridges. One beach ridge that corresponds with the Nipissing phase of Lake Superior is located 0.5 km inland from the present southern Lake Superior shore within the Huron Mountains, MI. Two parallel, low frequency ground penetrating radar (GPR) transects were collected over the ridge to better understand the subsurface stratigraphy. Preliminary results indicate that lakeward dipping reflections on top of horizontal to subhorizontal reflection patterns which indicate an aggradational and progradational coastal environment.en
dc.description.sponsorshipSummer Research Experience for Undergraduates (SREU); University of Wisconsin--Eau Claire Office of Research and Sponsored Programs.en
dc.language.isoen_USen
dc.relation.ispartofseriesUSGZE AS589en
dc.subjectNippising Beach Ridge (Huron Mountains, MI)en
dc.subjectHigh-frequency GPRen
dc.subjectGround penetrating radar (GPR)en
dc.subjectPostersen
dc.titleLow Frequency (50, 100, 200 MHz) Ground Penetrating Radar Analysis of the Nipissing Beach Ridge, Huron Mountains, MIen
dc.typePresentationen


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