Date of Award:
5-1958
Document Type:
Thesis
Degree Name:
Master of Science (MS)
Department:
Geology
Committee Chair(s)
J. Stewart Williams
Committee
J. Stewart Williams
Committee
Clyde T. Hardy
Committee
Donald R. Olsen
Abstract
Wellsville Mountain forms the extreme northern end of the Wasatch Range in northern Utah. It lies at the western margin of the Middle Rocky Mountain province and is bordered by valleys of the Basin and Range province. Many geologic investigations have been made in this region. Much of the Wasatch Range has been studied and mapped as well as parts of the Bear River Range, east of Cache Valley, and the Malad Range which extends north from Wellsville Mountain; however, the geology of Wellsville Mountain has not been studied or mapped in detail. Some reconnaissance mapping has been done and sections of Cambrian and Pennsylvanian formations have been measured on the western mountain front (Maxey, 1941; Williams, 1943), but little is known about the middle Paleozoic formations and the structural geology of the northern part of the mountain.
Checksum
1c7a182d22857b5e5e21004c65a71fa2
Recommended Citation
Beus, Stanley S., "Geology of the Northern Part of Wellsville Mountain, Northern Wasatch Range, Utah" (1958). All Graduate Theses and Dissertations. 4430.
https://digitalcommons.usu.edu/etd/4430
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