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Precambrian/Paleozoic unconformity at Chippewa Falls, Wisconsin

By
M. E. Ostrom
M. E. Ostrom
Wisconsin Geological and Natural History Survey, 3817 Mineral Point Road, Madison, Wisconsin 53705
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Published:
January 01, 1987

Abstract

Stream cut in east bank of Duncan Creek just northof first bridge south of Glen Lock Dam in Irvine Parknear north city limits of Chippewa Falls (Fig. 1) in the NW½, SW½, NE½, Sec.31, T.29N., R.8W., Chippewa County (Chippewa Falls 7¼-minute Quadrangle, 1972). Exposure can be reached by foot path from northeast side of bridge northward for about 300 ft (90 m).

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Contents

DNAG, Centennial Field Guides

North-Central Section of the Geological Society of America

Donald L. Biggs
Donald L. Biggs
531 Hayward Avenue Ames, Iowa 50010
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Geological Society of America
Volume
3
ISBN electronic:
9780813754093
Publication date:
January 01, 1987

GeoRef

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