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dc.contributor.advisorKrissek, Lawrence
dc.creatorHibbard, Shannon
dc.date.accessioned2014-05-13T13:19:53Z
dc.date.available2014-05-13T13:19:53Z
dc.date.issued2014-05
dc.identifier.urihttp://hdl.handle.net/1811/60443
dc.description.abstractProglacial environments, the settings in front of glaciers, are increasingly targeted for study as global climate change affects many of the world’s glaciers. This study focuses on a proglacial environment in Kaunertal, Austria, located in the drainage basin of the Gepatschferner Glacier, one of the biggest glaciers in Austria (Baewert and Morche, 2013). Effects of transport in proglacial drainage systems like this one are hypothesized to influence the distribution patterns of different rock types supplied by glacial erosion. The main goals of this project are to: 1) describe the composition of gravel-sized clasts along an ~4 km length of the Fagge River, the proglacial stream that drains the Gepatschferner Glacier in order to test the results presented in similar research; and 2) interpret the spatial changes in gravel composition in terms of the distribution of bedrock types in the area and the effects of transport, such as the greater persistence of stronger rock types during transport. Sixteen sites were sampled along the Fagge River, with ~50 grains collected at each site. Fifty grains were also taken from each major tributary or moraine. In addition, a sample was collected from each of 20 outcrops, distributed among the 3 lithologies in the study area. The composition of each grain was determined by visual examination with a hand lens and standard rock identification charts. The abundance of each rock type has been examined as a function of sampling location. The most abundant gravel compositions are “Orthogneiss,” “Paragneiss” and “Ortho- or Paragneiss.” There was a wide variation of abundances in all rock types throughout the length of the drainage basin. Although no significant trends were found, “Orthogneiss,” “Amphibolite,” and “Other” became somewhat more abundant downstream, while “Paragneiss,” “Ortho- or Paragneiss” and “Jointed Gneiss” are still present.en_US
dc.description.sponsorshipDAAD Rise fellowship (German Academic Exchange Program – Research Internships in Science and Engineering)en_US
dc.description.sponsorshipOhio State University Office of Diversity and Inclusion Undergraduate Research Grant approved by James Mooreen_US
dc.description.sponsorshipPROSA joint project (High-resolution measurements of morphodynamics in rapidly changing PROglacial Systems of the Alps)en_US
dc.description.sponsorshipThe German Research Foundation (DFG)en_US
dc.description.sponsorshipThe Austrian Science Fund (FWF)en_US
dc.description.sponsorshipThe Tyrolean Hydropower Company (TIWAG, Innsbruck)en_US
dc.description.sponsorshipThe School of Earth Sciences Goldthwait Geology Funden_US
dc.description.sponsorshipMartin-Luther-Universität Halle-Wittenbergen_US
dc.language.isoen_USen_US
dc.publisherThe Ohio State Universityen_US
dc.relation.ispartofseriesThe Ohio State University. School of Earth Sciences Undergraduate Research Theses; 2014en_US
dc.subjectgravel compositionen_US
dc.subjectproglacial environmenten_US
dc.subjectgravel distributionen_US
dc.titleControls on gravel composition in a proglacial environment Kaunertal, Austriaen_US
dc.typeThesisen_US
dc.description.embargoNo embargoen_US
dc.rights.ccAttribution 3.0 United Statesen_US
dc.rights.ccurihttp://creativecommons.org/licenses/by/3.0/us/en_US
dc.description.academicmajorAcademic Major: Earth Sciencesen_US


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