Everything about The Valparaiso Moraine totally explained
The
Valparaiso Moraine is a
terminal moraine around the
Lake Michigan basin in North America. It is a series of hills and ridges made up of
glacial till and
sand. It was formed during the Crown Point Phase of the
Wisconsin Glaciation. At this time the glacier covering the area had grown thin, so it was restrained by the
dolomite rock layers of the Lake Michigan basin. Where the glacier stopped, glacial till piled up, creating the hills of the moraine. After the Valparaiso Moraine was formed, the glacier retreated and formed the
Tinley Moraine.
Many towns in northwest
Indiana and northeast
Illinois are named after the Valparaiso Moraine or the Tinley Moraine. Also, many small creeks or rivers start in the Valparaiso Moraine. The moraine itself was named after the city of
Valparaiso, Indiana where the moraine is narrower and higher than in other places.
The Valparaiso Moraine forms part of the
St. Lawrence Seaway Divide and the
Great Lakes Drainage Basin. Water on one side of the moraine flows into Lake Michigan, of the
Great Lakes and eventually into the
Atlantic Ocean, and water on the other side flows into the
Kankakee River which flows into the
Mississippi River, which eventually flows into the
Gulf of Mexico.
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