Steven Dutch, Professor Emeritus, Natural and Applied Sciences, University of Wisconsin - Green Bay

Start Series
Previous (Earlier)
Next (Later)
View Text


Thick dolostone units form a cuesta that dips gently toward Lake Michigan, forming the Door Peninsula. South of Lake Winnebago the edge of the Silurian rocks is mantled by thick glacial deposits. Silurian rocks also occur on the summit of Blue Mound west of Madison.

The Niagara Escarpment, the edge of the Silurian rocks, wraps around the Michigan Basin, It defines the east shore of Lake Winnebago and the Door Peninsula in Wisconsin and the Garden Peninsula in upper Michigan. It is mantled by thick glacial deposits north of there but emerges on Manitoulin Island in Lake Huron. It forms the Bruce Peninsula that separates Lake Huron from Georgian Bay. The Bruce Peninsula is a near twin of the Door Peninsula, although much less developed. The Escarpment then runs across Ontario and east into New York. Niagara Falls flows across it, giving it its name.

South of Lake Winnebago, the Silurian escarpment is largely concealed by glacial deposits. It is also much less streamlined by ice scour and has a much more ragged outline on the map. It forms a distinct landform in places in Illinois and Iowa.

The Niagara escarpment is purely erosional, marking the edge of a thick, resistant series of rock layers. It is not connected to any fault or other tectonic disturbance.

Return to Geology of Wisconsin Index
Return to Professor Dutch's Home Page

Created 27 Dec 1997, Last Update 11 January 2020