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Temple Hill Quarries, Sanpete Co., Utah, USA

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Latitude & Longitude (WGS84): 39° 16' 23'' North , 111° 37' 39'' West
Latitude & Longitude (decimal): 39.27306,-111.62750
GeoHash:G#: 9wbx7v7q4
Other regions containing this locality:Rocky Mountains, North America
Locality type:Group of Quarries
Köppen climate type:BSk : Cold semi-arid (steppe) climate


REF:Analytical Data:: SRC.REF: PRATT AND CALLAGHAN, LAND AND MINERAL RESOURCES SANPETE COUNTY, 1966
Deposit:: PRATT, A. P., AND CALLAGHAN, 1970 , LAND AND MINERAL RESOURCES OF SANPETE COUNTY, UTAH: UTAH GEOL. AND MINERALOG. SURVEY BULL. 85
Production:: DO
Commodities (Major) - Stone - Dimension
Development Status: Past Producer
Host Rock Unit: Alluvial Fan Gravels
Structure: Wasatch Monocline
Host Rock: Limestone, Shale
Tectonic Structure: Cordilleran Hingeline


Commodity List

This is a list of exploitable or exploited mineral commodities recorded at this locality.


Mineral List

 No mineral species recorded.

Rock Types Recorded

Note: this is a very new system on mindat.org and data is currently VERY limited. Please bear with us while we work towards adding this information!

Select Rock List Type

Alphabetical List Tree Diagram

Regional Geology

This geological map and associated information on rock units at or nearby to the coordinates given for this locality is based on relatively small scale geological maps provided by various national Geological Surveys. This does not necessarily represent the complete geology at this locality but it gives a background for the region in which it is found.

Click on geological units on the map for more information. Click here to view full-screen map on Macrostrat.org

Tertiary
2.588 - 66 Ma



ID: 2427841
Displaced block of the Oligocene(?) Crazy Hollow Formation

Age: Cenozoic (2.588 - 66 Ma)

Stratigraphic Name: Crazy Hollow Formation

Description: Unbroken block of the Crazy Hollow Formation (Tch) carried “piggyback” to its present position, during either Oligocene(?) or Miocene time, on a block of the Green River Formation that slid valleyward.

Reference: Witkind, I.J, M.P. Weiss, T.L. Brown. Geologic map of the Manti 30′ x 60′ quadrangle, Carbon, Emery, Juab, Sanpete, and Sevier Counties, Utah. Utah Geological Survey Map 212DM. [62]

Eocene
33.9 - 56 Ma



ID: 3190876
Cenozoic sedimentary rocks

Age: Eocene (33.9 - 56 Ma)

Lithology: Sedimentary rocks

Reference: Chorlton, L.B. Generalized geology of the world: bedrock domains and major faults in GIS format: a small-scale world geology map with an extended geological attribute database. doi: 10.4095/223767. Geological Survey of Canada, Open File 5529. [154]

Early Eocene - Late Paleocene
47.8 - 59.2 Ma



ID: 3014802
Flagstaff Formation

Age: Paleogene (47.8 - 59.2 Ma)

Stratigraphic Name: Flagstaff Formation

Comments: non-marine. Flagstaff Ls has sandy lenses derived from east; Hintze (1988) has a question mark next to it in the Capital Reef area; mostly not present in this province

Lithology: Major:{limestone,mixed clastic}, Minor:{dolostone}

Reference: Horton, J.D., C.A. San Juan, and D.B. Stoeser. The State Geologic Map Compilation (SGMC) geodatabase of the conterminous United States. doi: 10.3133/ds1052. U.S. Geological Survey Data Series 1052. [133]

Data and map coding provided by Macrostrat.org, used under Creative Commons Attribution 4.0 License



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