Glacial Lake Wisconsin
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Glacial Lake Wisconsin was a prehistoric proglacial lake that existed from approximately 18,000 to 14,000 years ago, at the end of the last ice age, in the central part of present-day Wisconsin in the United States.
[edit] Formation and Demise
Before the last glacier, a somewhat different Wisconsin River drained the north-central part of the state, running around the east end of the Baraboo Hills. Around 18,000 years ago, the Green Bay lobe of the Wisconsin glaciation crept in from the east, butting up against the Baraboo Hills. With that outlet closed, the water backed up, filling the basin to the north and west, forming Glacial Lake Wisconsin.[1]
The water rose to as deep as 160 feet, with a surface area eight times the size of modern Lake Winnebago,[2] a big cold lake stretching north to the site of Wisconsin Rapids. Eventually it found a new outlet, flowing west to the Mississippi via the east fork of the Black River near City Point.[1] With water flowing out again, the lake stopped rising.
Islands poked up out of this icy lake, some of which remain today as the sandstone bluffs of central Wisconsin - Mill Bluff[3] and Roche-a-Cri, for example. The lake existed for thousands of years, with storms and ice scouring sand off those bluffs. Streams from the glacier to the north and east also carried in sand and silt which settled at the bottom of the lake, roughing in the flat sandy Central Plain that we see today when we follow I-90/94.
About 14,000 years ago, as the climate warmed, the glacier began to retreat. The lake water reopened the path around the Baraboo Hills. Once the trickle began, it quickly melted a larger channel through the ice and became a torrent. In a catastrophic flood, most of the huge lake probably drained out the south end in no more than a few weeks - possibly a few days. Upstream, the current cut new channels through the lake-bottom sand. After removing the lake-bottom sand, it cut canyons through the weak Cambrian sandstone beneath, which had existed long before the lake, forming the Dells of the Wisconsin River that the boat tours show today.[1]
This lake during the last glacier was probably not the only Glacial Lake Wisconsin. Earlier glaciers probably blocked the Wisconsin River, producing earlier glacial lakes in central Wisconsin. Less is known about them because their evidence has been eroded away or buried.[3]
[edit] See also
[edit] References
- ^ a b c Dott, Robert H., Jr; John W. Attig (2004). Roadside Geology of Wisconsin. Missoula, Montana: Mountain Press Publishing Company. pp. 199-205. ISBN 0-87842-492-X.
- ^ "Geologic History". Lower Wisconsin State Riverway Board. http://lwr.state.wi.us/subcategory.asp?linksubcatid=440&linkcatid=481&linkid=. Retrieved 2012-05-20.
- ^ a b Black, Robert F. (1974). "Chapter 8: Mill Bluff Pinnacles". National Park Service Scientific Monograph (National Park Service). http://www.cr.nps.gov/history/online_books/science/2/chap8.htm. Retrieved 2012-05-20.
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