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Event: A new look at Wisconsin glaciation – We Are Sauk Prairie Series

A new look at Wisconsin glaciation – We Are Sauk Prairie Series
Jan
17

Join us on Thursday, January 17th for our monthly, “We Are Sauk Prairie” series.  Our programs are free and open to the public.  Refreshments and snacks are offered.

What: Refining the Chronology of the Last Glaciation in South-Central Wisconsin

Who: Dr. Eric Carson, Quaternary Geologist / Associate Professor, Wisconsin Geological & Natural History Survey, University of Wisconsin Extension

When: Thursday, January 17, 6:30pm to 8:00pm

Where:  Ruth Culver Community Library, 540 Water Street, Prairie du Sac

Ice of the Green Bay Lobe of the Laurentide Ice Sheet last covered south-central Wisconsin, including the eastern Baraboo Hills, roughly 20,000 years ago. While the processes and general chronology of this glaciation are well understood, a precise record of ice advance and retreat near its maximum position has long been elusive.

Over the past several years, researchers at the Wisconsin Geological and Natural History Survey have been collecting core data from a variety of geologic settings in the Devils Lake gorge, western Baraboo Hills, Badger Army Ammunition plant land, and Black Earth Creek areas. Many of the locations cored were lakes during the last glaciation. While these lakes no longer exist, the sediments deposited on those lake beds provide abundant plant material that has been radiocarbon dated, and the dates correlated to the specific glacial events that caused the lakes to exist.

This work is providing absolutely new insight into the timing of the ice as it advanced and retreated: ice last reached its maximum position in the Devils Lake gorge area ~24,600 years ago and remained there until it started to retreat ~18,500 years ago. Prior to ice retreating from the area, it experienced a small advance, most likely shortly after 21,200 years ago. Ice had retreated to the very eastern end of the Baraboo Hills by ~17,400 years ago and allowed the catastrophic drainage of glacial Lake Wisconsin, the enormous lake that covered what today is known as the Central Sand Plain in central Wisconsin.