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Document Type

Research

Abstract

A traverse across a small first-order watershed in loess has been studied. The loess is Wisconsin in age and has a vertical tripartition that can be explained on a regional basis. Clear stratification is present in the middle loess increment. Moisture distribution patterns correlate highly with differences in particle-size distribution. The explanatory physical phenomena must be moisture-tension relationships.

Publication Date

1968

Journal Title

Proceedings of the Iowa Academy of Science

Volume

75

Issue

1

First Page

225

Last Page

233

Copyright

© Copyright 1968 by the Iowa Academy of Science, Inc.

Language

EN

File Format

application/pdf

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