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dc.contributor.advisorJol, Harry M.
dc.contributor.authorTopper, Nick
dc.contributor.authorJaeger, Nicholas
dc.contributor.authorCharlton, Brittany
dc.date.accessioned2015-02-09T22:16:15Z
dc.date.available2015-02-09T22:16:15Z
dc.date.issued2014-04
dc.identifier.urihttp://digital.library.wisc.edu/1793/70491
dc.descriptionColor poster with text, images, and photographs.en
dc.description.abstractVisible from aerial imagery, ridge formations can be seen building outward and parallel from the coast in South Westland, New Zealand, near the mouth of the Haast River. These coastal formations are a result of tectonically induced sediment pulses down the Haast River from shifting of the Alpine fault. To better understand the internal stratographic profiles of these coastal features, ground penetrating radar (GPR) was used parallel and perpendicular to dunes. The purpose of this study was the continued investigation of the stratigraphy of these coastal formations using GPR, which will lead to an enhanced understanding of geomorphic processes that affect the coastal processes near Haast, New Zealand, as well as other coastal locations affected by similar processes.en
dc.description.sponsorshipUniversity of Wisconsin--Eau Claire Office of Research and Sponsored Programs.en
dc.language.isoen_USen
dc.relation.ispartofseriesUSGZE AS589en
dc.subjectGround penetrating radaren
dc.subjectStratigraphyen
dc.subjectNew Zealand--Coastal formationsen
dc.subjectGeomorphic processesen
dc.subjectSouth Westland (N.Z.)en
dc.subjectHaast River (N.Z.)en
dc.subjectPostersen
dc.titleInvestigation of the Internal Stratigraphy of Alpine Fault Rupture Induced Coastal Dune Formations in South Westland, New Zealand Using Ground Penetrating Radaren
dc.typePresentationen


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