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Numerical simulation of the paleohydrology of glacial Lake Oshkosh, eastern Wisconsin, USA

Published online by Cambridge University Press:  20 January 2017

James A. Clark ,
Kevin M. Befus ,
Thomas S. Hooyer ,
Peter W. Stewart ,
Taylor D. Shipman ,
Chris T. Gregory  and
Deborah J. Zylstra
James A. Clark*
Affiliation:
Department of Geology and Environmental Science, Wheaton College, Wheaton, IL 60187, USA
Kevin M. Befus
Affiliation:
Department of Geology and Environmental Science, Wheaton College, Wheaton, IL 60187, USA
Thomas S. Hooyer
Affiliation:
Wisconsin Geological and Natural History Survey, Madison, WI, USA
Peter W. Stewart
Affiliation:
Department of Geology and Environmental Science, Wheaton College, Wheaton, IL 60187, USA
Taylor D. Shipman
Affiliation:
Department of Geology and Environmental Science, Wheaton College, Wheaton, IL 60187, USA
Chris T. Gregory
Affiliation:
Department of Geology and Environmental Science, Wheaton College, Wheaton, IL 60187, USA
Deborah J. Zylstra
Affiliation:
Department of Geology and Environmental Science, Wheaton College, Wheaton, IL 60187, USA
*
*Corresponding author.E-mail address:[email protected] (J.A. Clark).
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Abstract

Proglacial lakes, formed during retreat of the Laurentide ice sheet, evolved quickly as outlets became ice-free and the earth deformed through glacial isostatic adjustment. With high-resolution digital elevation models (DEMs) and GIS methods, it is possible to reconstruct the evolution of surface hydrology. When a DEM deforms through time as predicted by our model of viscoelastic earth relaxation, the entire surface hydrologic system with its lakes, outlets, shorelines and rivers also evolves without requiring assumptions of outlet position. The method is applied to proglacial Lake Oshkosh in Wisconsin (13,600 to 12,900 cal yr BP). Comparison of predicted to observed shoreline tilt indicates the ice sheet was about 400 m thick over the Great Lakes region. During ice sheet recession, each of the five outlets are predicted to uplift more than 100 m and then subside approximately 30 m. At its maximum extent, Lake Oshkosh covered 6600 km2 with a volume of 111 km3. Using the Hydrologic Engineering Center-River Analysis System model, flow velocities during glacial outburst floods up to 9 m/s and peak discharge of 140,000 m3/s are predicted, which could drain 33.5 km3 of lake water in 10 days and transport boulders up to 3 m in diameter.

Keywords

Lake OshkoshOutburst floodGlacial isostasyPaleohydrologyGISGreat LakesProglacial lake
Type
Research Article
Information
Quaternary Research , Volume 69 , Issue 1 , January 2008 , pp. 117 - 129
Copyright
Elsevier Inc.

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