Lessons From converting Alaska digital geologic maps to the USGS Geologic Map Schema (GeMS) (presentation): U.S. Geological Survey Digital Mapping Techniques Workshop Series DMT2020 (A Virtual Event), June 8-10, 2020

Geologic Map of the Park Reservoir Quadrangle, Sheridan County, Wyoming

The Mountain Geologist ◽

10.31582/rmag.mg.57.4.375 ◽

2020 ◽

Vol 57 (4) ◽

pp. 375-388

Author(s):

Ryan Bessen ◽

Jennifer Gifford ◽

Zack Ledbetter ◽

Sean McGuire ◽

Kyle True ◽

...

Keyword(s):

Structural Features ◽

Geologic Mapping ◽

Rock Types ◽

Basement Rocks ◽

Geologic Maps ◽

Geologic Map ◽

Tear Fault ◽

Mapping Techniques ◽

Wyoming Province ◽

Bighorn Mountains

This project involved the construction of a detailed geologic map of the Park Reservoir, Wyoming 7.5-Minute Quadrangle (Scale 1:24,000). The Quadrangle occurs entirely in the Bighorn National Forest, which is a popular recreation site for thousands of people each year. This research advances the scientific understanding of the geology of the Bighorn Mountains and the Archean geology of the Wyoming Province. Traditional geologic mapping techniques were used in concert with isotopic age determinations. Our goal was to further subdivide the various phases of the 2.8–3.0 Ga Archean rocks based on their rock types, age, and structural features. This research supports the broader efforts of the Wyoming State Geological Survey to complete 1:24,000 scale geologic maps of the state. The northern part of the Bighorn Mountains is composed of the Bighorn batholith, a composite complex of intrusive bodies that were emplaced between 2.96–2.87 Ga. Our mapping of the Park Reservoir Quadrangle has revealed the presence of five different Archean quartzofeldspathic units, two sets of amphibolite and diabase dikes, a small occurrence of the Cambrian Flathead Sandstone, two Quaternary tills, and Quaternary alluvium. The Archean rock units range in age from ca. 2.96–2.75 Ga, the oldest of which are the most ancient rocks yet reported in the Bighorn batholith. All the Archean rocks have subtle but apparent planar fabric elements, which are variable in orientation and are interpreted to represent magmatic flow during emplacement. The Granite Ridge tear fault, which is the northern boundary of the Piney Creek thrust block, is mapped into the Archean core as a mylonite zone. This relationship indicates that the bounding faults of the Piney Creek thrust block were controlled by weak zones within the Precambrian basement rocks.

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