Niagara Escarpment

Niagara Escarpment

also called  Lake Ridge  

      ridge in North America that extends (with breaks) for more than 650 miles (1,050 km) from southeastern Wisconsin north to the Door Peninsula in the eastern part of the state, through the Manitoulin Islands of Ontario in northern Lake Huron, southward across the Bruce Peninsula, and then eastward around the southwestern end of Lake Ontario. The escarpment is the eroded headland of a hard, Silurian-aged dolomite; as such the rock has stood up to the forces of weathering and glaciation better than nearby shales. The ridge crosses the U.S.-Canadian boundary at Niagara Falls and terminates just east of Rochester, N.Y. Its forested crest stands from 250 to 1,000 feet (75 to 300 m) above the surrounding lowlands. Several rivers, notably the Niagara, have cut gorges through the scarp, leaving recessed cataracts, including the famous Niagara Falls. Such cities as Rochester have grown up adjacent to cataracts (Genesee Falls), taking advantage of the cheap power supply. The escarpment also shelters the intensive Niagara fruit belt along the southern shore of Lake Ontario and forms the Garden Peninsula in Michigan.

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Universalium. 2010.

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