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Authors

Charles Keyes

Document Type

Research

Abstract

Bozeman Beds is a term which is applied to certain gravel deposits that saddle the continental divide in Montana and Idaho. These beds are true epirotic accumulations. They appear to be mainly fluviatile in origin; although they manifestly are partly eolic in nature. Consisting of gravels, sands and silts they chiefly lie in old intermontane valleys. Their age is pre-Glacial.

Publication Date

1919

Journal Title

Proceedings of the Iowa Academy of Science

Volume

26

Issue

1

First Page

467

Last Page

469

Copyright

©1919 Iowa Academy of Science, Inc.

Language

en

File Format

application/pdf

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