Please use this identifier to cite or link to this item: https://hdl.handle.net/11681/5192
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dc.contributor.authorWilliams, S. Jeffress-
dc.contributor.authorCarter, Charles H. (Charles Henry)-
dc.contributor.authorMeisburger, Edward P.-
dc.contributor.authorFuller, Jonathan A.-
dc.date.accessioned2016-03-21T14:17:08Z-
dc.date.available2016-03-21T14:17:08Z-
dc.date.issued1980-11-
dc.identifier.urihttp://hdl.handle.net/11681/5192-
dc.descriptionMiscellaneous Report-
dc.descriptionAbstract: About 2,250 square kilometers of the Lake Erie bottom between Conneaut and Toledo, about 25 percent of Ohio's open lake part of Lake Erie, was surveyed to assess potential sand and gravel resources. Primary survey data consist of 690 kilometers of high-resolution seismic reflection profiles between Conneaut and Toledo; 58 vibracores with a maximum length of 6.1 meters were also taken between Conneaut and Marblehead, Ohio. Survey limits were generally from the -7.5-meter depth contour to about the -14-meter depth contour, a maximum of about 16 kilometers offshore.-
dc.publisherCoastal Engineering Research Center (U.S.)-
dc.publisherEngineer Research and Development Center (U.S.)-
dc.relationhttp://acwc.sdp.sirsi.net/client/en_US/search/asset/1007446-
dc.relation.ispartofseriesMiscellaneous report (Coastal Engineering Research Center (U.S.)) ; no. 80-10.-
dc.rightsApproved for Public Release, Distribution is Unlimited-
dc.sourceThis Digital Resource was created from scans of the Print Resource-
dc.subjectGeomorphology-
dc.subjectLake Erie-
dc.subjectOhio-
dc.subjectSand Resources-
dc.subjectSediments-
dc.subjectSeismic Reflection-
dc.subjectVibracores-
dc.titleSand resources of southern Lake Erie, Conneaut to Toledo, Ohio: a seismic reflection and vibracore study-
dc.typeReporten_US
Appears in Collections:Miscellaneous Report

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