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dc.creatorLanglois, Thomas H.en_US
dc.date.accessioned2005-10-01T01:11:18Z
dc.date.available2005-10-01T01:11:18Z
dc.date.issued1965-11en_US
dc.identifier.citationThe Ohio Journal of Science. v65 n6 (November, 1965), 343-352en_US
dc.identifier.issn0030-0950en_US
dc.identifier.urihttp://hdl.handle.net/1811/5118
dc.descriptionAuthor Institution: Department of Zoology and Entomology, The Ohio State University, Columbus, Ohio 43210en_US
dc.description.abstractThe tombolo at the northeastern end of South Bass Island, and a contiguous till bank on the southeastern shore were studied between 1936 and 1963. The bar of the tombolo represents the line of convergence of waves from the east which had passed on both sides of the dolomitic outcrop at the outer end of the bar. Waves from the west, approaching the bar at right angles, brought to it materials from both sides. Changing levels of Lake Erie alternately submerged and exposed the bar for prolonged periods. During periods of exposure, many plants appeared, which were subjected to overriding sheet-ice and then were eliminated by subsequent prolonged submergence. The adjacent till bank receded by a combination of the effects of shoving ice, frost, rain, waves, and winds (dehydration and sand-blasting). Boulders which washed out of the till bank were moved by waves and ice and accumulated near the landward end of the bar. These changes are illustrated by a set of dated photographs.en_US
dc.format.extent7671696 bytes
dc.format.mimetypeapplication/pdf
dc.language.isoen_US
dc.rightsReproduction 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.titleEcological Processes at a Section of Shoreline of South Bass Island, Lake Erieen_US


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