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The loess cover of northeastern Wisconsin

Published online by Cambridge University Press:  20 January 2017

Randall J. Schaetzl  and
John W. Attig
Randall J. Schaetzl*
Affiliation:
Department of Geography, 128 Geography Bldg, Michigan State University, East Lansing, MI 48824-1117, USA
John W. Attig
Affiliation:
Wisconsin Geological and Natural History Survey, 3817 Mineral Point Road, Madison, WI 53705-5100, USA
*
*Corresponding author. Fax: + 1 517 432 1671. E-mail address:soils@msu.edu (R.J. Schaetzl).
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Abstract

We present the first study of the distribution, genesis and paleoenvironmental significance of late Pleistocene loess in northeastern Wisconsin and adjacent parts of Michigan's Upper Peninsula. Loess here is commonly 25–70 cm thick. Upland areas that were deglaciated early and remained geomorphically stable preferentially accumulated loess by providing sites that were efficient at trapping and retaining eolian sediment. Data from 419 such sites indicate that the loess was mainly derived from proglacial outwash plains and to a lesser extent, hummocky end moraines within and near the region, particularly those toward the east of the loess deposits. Most of the loess was transported on katabatic winds coming off the ice sheet, which entrained and transported both silt and fine sands. The loess fines markedly, and is better sorted, distal to these source regions. Only minimal amounts of loess were deposited in this area via westerly winds. This research (1) reinforces the observation that outwash plains and end moraines can be significant loess sources, (2) provides evidence for katabatic winds as significant eolian transport vectors, and (3) demonstrates that the loess record may be variously preserved across landscapes, depending on where and when geomorphically stable sites became available for loess accumulation.

Keywords

WisconsinMichiganOutwash plainsDrumlinsKatabatic windsGlacial anticyclone

Information

Type
Research Article
Information
Quaternary Research , Volume 79 , Issue 2 , March 2013 , pp. 199 - 214
Copyright
University of Washington

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