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Florence Valley : An Abandoned Stream Valley, Florence Township, Erie County, Ohio

Please use this identifier to cite or link to this item: http://hdl.handle.net/1811/5575

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dc.creator Hole, Thornton J. F. en_US
dc.creator Redmond, Charles E. en_US
dc.date.accessioned 2005-10-01T02:58:32Z
dc.date.available 2005-10-01T02:58:32Z
dc.date.issued 1970-11 en_US
dc.identifier.citation The Ohio Journal of Science. v70 n6 (November, 1970), 341-346 en_US
dc.identifier.issn 0030-0950 en_US
dc.identifier.uri http://hdl.handle.net/1811/5575
dc.description Author Institution: U.S.D.A. Soil Conservation Service, Sandusky, Ohio en_US
dc.description.abstract An abandoned stream valley, here called Florence Valley, was found in eastern Erie County, Ohio. Florence Valley is about one mile long and connects the valleys of Chappel Creek and the Vermilion River. There is evidence that Florence Valley was formed as a result of the capture of a tributary of the Vermilion River by Chappel Creek. Chappel Creek, at the junction of Florence Valley and the valley of Chappel Creek, has a rightangled bend, which displays morphology characteristic of an "elbow-of-capture." The gradient of the eastern two-thirds of Florence Valley slopes toward the Vermilion River. Because the Vermilion River is more deeply entrenched than is Chappel Creek, this stream capture must have taken place at a time when the base level was at a higher elevation, when Chappel Creek had a shorter course and steeper gradient than did the Vermilion River. These conditions are believed to have existed during the time of Lake Maumee III. en_US
dc.format.extent 418415 bytes
dc.format.mimetype application/pdf
dc.language.iso en_US
dc.rights Reproduction of articles for non-commercial educational or research use granted without request if credit to The Ohio State University and The Ohio Academy of Science is given. en_US
dc.title Florence Valley : An Abandoned Stream Valley, Florence Township, Erie County, Ohio en_US