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Document Type

Research

Abstract

The gravels related to the Iowan glaciation of northeastern Iowa have been studied in the field and laboratory. Three factors were significant in the field correlation, (a) stratigraphic relations (b) topographic position and (c) amount of weathering. In the laboratory the size, range, shapes, and lithology of the gravels were studied but little of value for correlation purposes was obtained.

Publication Date

1931

Journal Title

Proceedings of the Iowa Academy of Science

Volume

38

Issue

1

First Page

206

Last Page

206

Copyright

©1931 Iowa Academy of Science, Inc.

Language

en

File Format

application/pdf

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