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.
Proceedings of the Iowa Academy of Science
©1936 Iowa Academy of Science, Inc.
Bissell, H. J.
"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