The St. Croix river was formed relatively recently in geological terms. During the last ice age, a glacier blocked the south end of Lake Superior, forming glacial Lake Duluth. As the ice retreated, Lake Duluth broke though its banks to the south and started to drain. The water rushed to the south cutting first the St. Croix valley, and later the Mississippi River valley south of Hastings. Once the glaciers melted and Lake Duluth was empty, a small rise of land dividied the St. Croix river near the present day town of Solon Springs, Wisconsin. At this point, water on the northeast side of the divide flowed though the Bois Brule River to the north into Lake Superior. Water on the south and west side of the divide flowed south on the St. Croix River, and then flowing into the Mississippi River at Prescott, Wisconsin. This divide was not a hill or a mountain, rather it is no more than a matter of a few inches in a swampy area at the north end of Upper St. Croix Lake. This swampy area sits in the river valley carved by the glacial river flow. In contrast to the divide being only a few inches, the river valley is about 125 feet deep.
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Authored by John A. Weeks III, Copyright © 2007, all rights reserved.
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