Start Series
Previous (Earlier)
Next (Later)
View Text
Steven Dutch, Natural and Applied Sciences, University
of Wisconsin - Green Bay
First-time Visitors: Please visit Site Map and Disclaimer. Use
"Back" to return here.
|
|
Possible Early Pleistocene Drainage in Wisconsin Start Series Previous (Earlier) Next (Later) View Text |
Possible Early Pleistocene Drainage in Wisconsin
The early Pleistocene or pre-Pleistocene drainage system of Wisconsin may have looked like this. Bedrock in the western two-thirds of the state is shown with present outcrop patterns, but the Paleozoic of eastern Wisconsin is shown as it may have been before extensive glacial erosion.
Most of the western drainages are shown as they are at present, along with the present Mississippi, which is probably an early Pleistocene ice-marginal drainage. Whether the Mississippi was the major trunk drainage at this time is not known.
Following a hypothesis advanced by Lawrence Martin, the lower Wisconsin River is shown draining eastward. Unlike most valleys, the Wisconsin River narrows as it goes downstream, becoming narrowest at Boscobel. This suggests that the Wisconsin River may have originally flowed east, but was diverted sometime during the Pleistocene.
Return to Geology of Wisconsin Index
Return to Professor Dutch's Home Page
Created 4 October 2000, Last Update 17 July 2003
Not an official UW Green Bay site