Steven Dutch, Natural and Applied Sciences, University
of Wisconsin - Green Bay
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The oldest known rocks in the continental United States, over 3 billion years old, outcrop in the Minnesota River Valley. Numerous outcrops occur between Montevideo and Granite Falls along U.S. 212.
The map above, admittedly a large graphic, shows the area between Montevideo and Granite Falls. The Minnesota River Valley was a major glacial spillway. Note the anastamosing channels southwest of the valley and the broad flat-bottomed and highly underfit river valley itself
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Although there are no outcrops in Montevideo itself, they begin appearing a couple of kilometers southeast of town on US 212. There are a number exposed in road cuts, and any hill protruding from the valley floor is likely to be an outcrop as well. |
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The picture at left and those below are of outcrops along US 212 a few kilometers SE of Montevideo. |
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Left: the flat-bottomed floor of the Minnesota River valley.
Below: amphibolite exposed on US 212 about halfway between Montevideo and Granite Falls. |
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Large outcrop northwest of Granite Falls protruding from valley floor. |
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Flat-bottomed floor of the Minnesota River valley. |
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Large outcrop northwest of Granite Falls protruding from valley floor. |
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Flat-bottomed floor of the Minnesota River valley, looking toward Granite Falls. The light patch on the ridge at right center is a large quarry. |
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Flat-bottomed floor of the Minnesota River valley. |
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Left and below: outcrops just northwest of Granite Falls on US 212. |
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State Highway 23 affords a good view of the Minnesota River Valley as it climbs the valley wall south of Granite Falls. |
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Created 7 April 2003, Last Update 03 July 2003
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