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The Champlain Sea was a temporary inlet of the Atlantic Ocean, created by the retreating glaciers during the close of the last ice age.〔L.J. Chapman and D.F. Putnam. 1951. The Physiography of Southern Ontario. University of Toronto Press, Toronto. 284 p. plus map in four sections.〕〔Anderson, T.W. 1989. Vegetation changes over 12,000 years. Geos 18:39–47.〕 The Sea once included lands in what are now the Canadian provinces of Quebec and Ontario, as well as parts of the American states of New York and Vermont.〔(Lake Champlain Basin Atlas: Geology Page )〕 The mass of ice from the continental ice sheets had depressed the rock beneath it over millennia. At the end of the last ice age, while the rock was still depressed, the Saint Lawrence and Ottawa River valleys, as well as modern Lake Champlain, were below sea level and flooded once the ice no longer prevented the ocean from flowing into the region.〔(Paleoceanography of the Champlain Sea, Hanover Park, Canada )〕 As the land gradually rose again (a process known as isostatic rebound), the sea coast gradually retreated to its current location. The sea lasted from about 13,000 years ago to about 10,000 years ago and was continuously shrinking during that time, since the rebounding continent was slowly rising above sea level. At its peak, the sea extended inland as far south as Lake Champlain and somewhat farther west than the city of Ottawa, Ontario, and farther up the Ottawa River past Pembroke.〔 The remaining glaciers fed the sea during that time, making it more brackish than typical seawater. It is estimated that the sea was as much as above the level of today's Saint Lawrence and Ottawa Rivers.〔Barnett, P.J. 1988. History of the northwestern arm of the Champlain Sea. Pp 25–36 in Gadd, N.R. (ed.) ''The Late Quaternary Development of the Champlain Sea Basin''. Geological Association of Canada, Special Paper 36. Map 5.〕 The best evidence of this former sea is the vast clay plain deposited along the Ottawa and St. Lawrence Rivers.〔Chapman, L.J. and D.F. Putnam. 1984. ''The Physiography of Southern Ontario''. Third edition. Ontario Geological Survey, Special Volume No.2. Government of Ontario, Toronto.〕 This resulted in distinctive forest types,〔Keddy, C.J. 1993. ''Forest History of Eastern Ontario''. A report prepared for the Eastern Ontario Forest Group.〕 and large wetlands. Other modern evidence of the sea can be seen in the form of whale fossils, (belugas, fin whales,〔(Paleobiology database: Daveluyville collection )〕 and bowhead whales) and marine shells〔(University of Calgary: Champlain Sea fossils )〕 that have been found near the cities of Ottawa, Ontario, and Montreal, Quebec. There are also fossils of oceanic fish such as capelin.〔McAllister, D.E., C.R. Harrington, S.L. Cumbaa, and C.B. Renaud. 1988. "Paleoenvironmental and biogeographic analyses of fossil fishes in peri-Champlain Sea deposits in Eastern Canada". Pp 241–258 in Gadd, N.R. (ed.) ''The Late Quaternary Development of the Champlain Sea Basin''. Geological Association of Canada, Special Paper 36.〕 The Sea also left ancient shorelines in the former coastal regions, and the Leda clay deposits in areas of deeper water.〔("Residents seek reassurance in wake of deadly slide" ) ''The Globe and Mail'', May 12, 2010.〕 The northern shore of lake was in southern Quebec where outcrops of the Canadian shield form the Eardley Escarpment. This escarpment still has distinctive plants that may date back to the sea.〔Brunton, D. and J.D. Lafontaine. 1974. An unusual escarpment flora in Western Quebec. The Canadian Field-Naturalist 88(3):337–344.〕 The Eardley Escarpment is known locally as the Gatineau Hills; part of the Mattawa fault at the southeastern edge of the Ottawa-Bonnechere Graben, in Eastern Ontario and the Outaouais region of Quebec, more commonly known as the Ottawa Valley. ==References== 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Champlain Sea」の詳細全文を読む スポンサード リンク
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