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dc.creatorHerdendorf, Charles E.en_US
dc.creatorBailey, Martin L.en_US
dc.date.accessioned2006-07-07T02:29:12Z
dc.date.available2006-07-07T02:29:12Z
dc.date.issued1989-03en_US
dc.identifier.citationThe Ohio Journal of Science. v89, n1 (March, 1989), 16-22en_US
dc.identifier.issn0030-0950en_US
dc.identifier.urihttp://hdl.handle.net/1811/23300
dc.descriptionAuthor Institution: Center for Lake Erie Area Research, Department of Zoology, and Department of Geology and Mineralogy, The Ohio State Universityen_US
dc.description.abstractTest borings in the western basin of Lake Erie have revealed an extensive sub-bottom deposit of sand in a triangular region bounded by Stony Point on the mainland shore of Michigan, Middle Sister Island in Ontario, and West Sister Island in Ohio. The 550 km2 deposit is overlain by up to 7 m of more recent lacustrine silts and clays. The sand beds have an average thickness of 2.3 m, yielding a total volume of approximately 1.3 X 109 m3 of sand. A preliminary interpretation is that when the ancestral Detroit River first flowed into Early Lake Erie about 4-5,000 years B. P. deltaic sediments were deposited in the northern portion of the western basin. The material of these beds is primarily a clean, medium- to fine-grained, moderately well-sorted sand that appears to have commercial extraction quality.en_US
dc.format.extent2373698 bytes
dc.format.mimetypeapplication/pdf
dc.language.isoen_US
dc.titleEvidence for an Early Delta of the Detroit River in Western Lake Erieen_US


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