Home > Iowa Academy of Science > Journals & Newsletters > Proceedings of the Iowa Academy of Science > Volume 43 (1936) > Annual Issue
Document Type
Research
Abstract
The area under consideration has a dimension of 8 miles east-west and 4 miles north-south, and includes the canyons of Spring Creek and Hobble Creek, Utah County, Utah. These streams flow off the west flank of a southern portion of the Wasatch Range, and have cut canyons to a depth of over 3,000 feet, exposing sections of upper Paleozoic sediments. Pennsylvanian rocks in the vicinity of the southern Wasatch Mountains have received little attention from stratigraphers. In this paper an attempt is made to describe the sequence of Pennsylvanian rocks in the region.
Publication Date
1936
Journal Title
Proceedings of the Iowa Academy of Science
Volume
43
Issue
1
First Page
239
Last Page
243
Copyright
©1936 Iowa Academy of Science, Inc.
Language
en
File Format
application/pdf
Recommended Citation
Bissell, H. J.
(1936)
"Pennsylvanian Stratigraphy in the Southern Wasatch Mountains, Utah,"
Proceedings of the Iowa Academy of Science, 43(1), 239-243.
Available at:
https://scholarworks.uni.edu/pias/vol43/iss1/57