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- W2020616101 abstract "The region here designated as the Driftless Cuestaform Hill Land refers to that part of the inner basin of the Upper Mississippi unmantled by recent till sheets, where the local relief usually exceeds 250 feet. It is not identical with the well known Driftless Area although, in general, that region forms its innermost and roughest part. Relatively inconspicuous deposits of ancient glaciers cover extensive areas in its western and northern parts (Fig. 1). Except in a few sectors its circumference coincides with a belt enclosed between the local-relief isarithms of 200 and 300 feet (Fig. 2). Over considerable areas relief exceeds 500 feet and at a maximum reaches 800. Low hill country and rough plain are the most suitable descriptive terms for the region. Lying as it does in the midst of extensive youthful till plains, the Driftless Cuestaform Hill Land has distinctiveness not only in its degree of local relief but likewise in the patternful arrangement of its stream-eroded relief forms. In all schemes of physiographic subdivisions of the United States the region under consideration stands out as a clearly defined unit." @default.
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- W2020616101 date "1938-09-01" @default.
- W2020616101 modified "2023-09-23" @default.
- W2020616101 title "French Settlement in the Driftless Hill Land" @default.
- W2020616101 doi "https://doi.org/10.1080/00045603809357180" @default.
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