Devil's Lake: Trapped by the End Moraine
Travis Suggitt
While working on a portion of the Ice Age Trail in southern Wisconsin, our crew spent the evenings swimming in nearby Devil's Lake. I was fortunate to make friends with Dave, an employee of the Ice Age Trail Alliance who is extremely knowledgeable on the area's formation. While sitting on the beach of the lake, Dave pointed at various features and described their geological history. He explained that until around 10,000 years ago, this lake was part of a river with the lake's east and west quartzite bluffs forming its banks.
Looking south-east across Devil's Lake, the ancient river's original path can be visualized as it would have followed the bluffs (Skillet Creek Media, 2020b). |
The end moraine, which dammed Devil's Lake, is seen here as the shorter hill between the two bluffs (Skillet Creek Media, 2020a). |
Pointing north, Dave explained that a less noticeable hill exists from the same process. The glacier wasn't able to cut through or go over the eastern quartzite bluff in its final advances, so the end moraine wraps around it leaving sedimentary dams on the north and south ends of Devil's Lake.
Photo References:
Skillet Creek Media. (2020a). Did glaciers make Devil's Lake? https://www.devilslakewisconsin.com/learning-center/did-glaciers-make-devils-lake/
Skillet Creek Media. (2020b). Tumbled Rocks Trail. https://www.devilslakewisconsin.com/activities/hiking/devils-lake-trail-details-descriptions/tumbled-rocks-trail/
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