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dc.contributor.advisorWhite, Sidney E.en_US
dc.creatorTaylor, Harold R.en_US
dc.date.accessioned2014-02-17T18:31:16Z
dc.date.available2014-02-17T18:31:16Z
dc.date.issued1969-12en_US
dc.identifier.urihttp://hdl.handle.net/1811/59211
dc.description.abstractThe purpose of this study is to see if the cobble lithology in a Wisconsin Carroll esker would infer direction of ice movement. Roundness was also studied to determine, in a gross fashion, distance of travel of the cobbles. The data shows a high carbonate to clastic ratio with foreign rock (igneous and metamorphic) about equal to clastic. This indicates an ice movement from a west of north direction from the esker. The data also indicates little or no variation in the direction of the ice movement.en_US
dc.language.isoen_USen_US
dc.publisherThe Ohio State Universityen_US
dc.relation.ispartofseriesThe Ohio State University. Department of Geology Senior Theses; 1969en_US
dc.titleDetermination of direction of late Wisconsin ice movement from stone counts in Carroll eskeren_US
dc.typeThesisen_US
dc.description.embargoNo embargoen_US


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