Written in 2002; 2,397 words; 10 sources; MLA; $ 73.95
Paper Summary:
This paper discusses the various geological processes that form the features and natural resources of the Great Lakes and provides a summary of the geologic history of the area. The Great Lakes are a chain of inland lakes, including Lake Ontario, Lake Erie, Lake Huron, Lake Michigan and Lake Superior which stretch from New York to Minnesota.
Spanning a surface area of 95,000 square miles, the five lakes represent the greatest stretch of fresh water on the planet.
Outline
Introduction
Geological Processes and Characteristics
Brief Geological History
Geology of the Great Lakes
Conclusion
From the Paper:
"Observation of existing ice sheets and glaciers indicate that they invariably flow downhill from elevated regions (Cox, 1999). Still, the postulated, hypothetical flow of the ice of the glacial theory was uphill out of basins and depressions like the basin of Lake Ontario. The ice is assumed to have flowed uphill out of Lake Ontario, over the steep cliffs of the Niagara Escarpment, and flowed uphill towards the area of northwestern New York. There are many geologic characteristics of the Great Lakes, including bedrock. The geologic setting of the Great Lakes basins began billions of years ago, with the formation of bedrock. The foundation for the present Great Lakes basin began about three billion years ago, during the Precambrian Era. Most bedrock is made up of sedimentary rock of Paleozoic age (which can be up to 600 million years old). However, the rock around Lake Superior, the deepest of the Great Lakes, is much older igneous and metamorphic rock, Pre-Cambrian in age (up to two billion years old)."
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