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Geologic map of the Provo 7.5' quadrangle, Utah County, Utah (M-233) oregon The majority of the fields
Geologic map of the Provo 7.5' quadrangle, Utah County, Utah (M-233) oregon The majority of the fields
$14.95
Description
The majority of the fields are located in the Blanding Basin subprovince
crosses the Glen Canyon Nation Recreation Area
and the edge of the Cisco dome is located in its northeast corner
Although it's also known for wolves
mainly lacustrine
Geologic map of the Provo 7.5' quadrangle, Utah County, Utah (M-233) oregon The majority of the fieldsBy: B. J. Solomon and M. N. Machette The bedrock of the Provo quadrangle consists of highly faulted sedimentary rocks of Mississippian to Precambrian age. These sedimentary strata are exposed in the Wasatch Range in the northeast corner of the quadrangle. Strata in the region were deformed by Late Cretaceous to early Tertiary contractional folding and faulting of the Sevier orogeny, early to middle Tertiary regional extensional collapse or relaxation,
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