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Authors

Philip B. King

Document Type

Research

Abstract

Outlines the physiographic history of southwestern North Dakota; describes terraces and terrace gravels along Cannonball River, particularly in regard to pebbles of material not now found in the drainage basin of the stream; and suggests the existence in the area of an easterward dipping upland surface with possible continuations eastward and westward upon which the present streams, notably Missouri and Little Missouri, have anomalous courses.

Publication Date

1924

Journal Title

Proceedings of the Iowa Academy of Science

Volume

31

Issue

1

First Page

333

Last Page

333

Copyright

©1924 Iowa Academy of Science, Inc.

Language

en

File Format

application/pdf

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