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dc.creatorVolpi, Richard W.en_US
dc.creatorSzabo, John P.en_US
dc.date.accessioned2006-07-07T02:27:29Z
dc.date.available2006-07-07T02:27:29Z
dc.date.issued1988-12en_US
dc.identifier.citationThe Ohio Journal of Science. v88, n5 (December, 1988), 174-180en_US
dc.identifier.issn0030-0950en_US
dc.identifier.urihttp://hdl.handle.net/1811/23280
dc.descriptionAuthor Institution: Department of Geology, University of Akronen_US
dc.description.abstractThe clay mineralogy of three pre-Woodfordian tills of the Grand River lobe in Columbiana County, Ohio, shows the influence of the underlying Pennsylvanian strata of the Allegheny Plateau. The mean diffraction intensity ratios (DI) of these sandy tills range from 0.5 to 0.7. These ratios are comparable to those of the underlying bedrock; 60% of the variance of the clay mineralogy may be attributed to the bedrock. Weathered bedrock and weathered older drift are possible sources of kaolinite. Locally entrained Pennsylvanian sandstone clasts at the base of the glacier may have acted as tools for extensive abrasion of softer argillaceous shales. This abrasion may have produced tills having a higher kaolinite content than those near the edge of the Allegheny Escarpment in north-central Ohio.en_US
dc.format.extent1252131 bytes
dc.format.mimetypeapplication/pdf
dc.language.isoen_US
dc.titleInfluence of Local Bedrock on the Clay Mineralogy of Pre-Woodfordian Tills of the Grand River Lobe in Columbiana County, Ohioen_US


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