Home > Iowa Academy of Science > Journals & Newsletters > Proceedings of the Iowa Academy of Science > Volume 26 (1919) > Annual Issue
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
Recommended Citation
Keyes, Charles
(1919)
"Southward Extension of the Bozeman Tertiaries into Utah,"
Proceedings of the Iowa Academy of Science, 26(1), 467-469.
Available at:
https://scholarworks.uni.edu/pias/vol26/iss1/43