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The Surficial Geology Of Southern Logan County, North Dakota, John W. Bonneville
The Surficial Geology Of Southern Logan County, North Dakota, John W. Bonneville
Theses and Dissertations
Southern Logan County, North Dakota, was glaciated at least three different times during the Pleistocene epoch. Scattered patches of highly weathered iron-cemented drift found in the area of eroded Cretaceous bedrock in southwest-era Logan County are very possibly pre-Wisconsinan in age. Two younger drift sheets of Wisconsinan age cover the remaining portion of the county. One of these drifts, the Napoleon drift, is probably early Wisconsinan, and the other, the Burnstad-Streeter drift, is likely late Wisconsinan in age.
A great diversity in types of glacial topography and individual features is found in southern Logan County. Excellent examples of end moraine, …