Standard Gypsum Corporation, Hillsborough Co., Florida, USA
Latitude & Longitude (WGS84): | 27° 56' 60'' North , 82° 28' 0'' West |
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Latitude & Longitude (decimal): | 27.95000,-82.46667 |
GeoHash: | G#: dhvr52jse |
Köppen climate type: | Cfa : Humid subtropical climate |
REF:Deposit:: NOT ON 1980/1981 MSHA LISTS
Deposit:: RCF LIST 10-81; REPT. #0850007
Deposit:: CMS LIST 10-81; REPT. #0850007
Deposit:: MAY BE A PROCESSING PLANT
Commodities (Major) - Gypsum-Anhydrite
Development Status: Unknown
Commodity List
This is a list of exploitable or exploited mineral commodities recorded at this locality.Mineral List
2 valid minerals.
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
Cenozoic 0 - 66 Ma ID: 3186031 | Cenozoic sedimentary rocks Age: Cenozoic (0 - 66 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] |
Middle Miocene - Chattian 11.62 - 28.1 Ma ID: 2905140 | Hawthorn Group, Arcadia Formation, Tampa Member Age: Cenozoic (11.62 - 28.1 Ma) Stratigraphic Name: Tampa Member Description: The Tampa Member consists predominantly of limestone with subordinate dolostone, sand and clay (Scott, 1988). The lithology of the Tampa Member is very similar to that of the subsurface limestone part of the Arcadia Formation except that the Tampa Member contains noticeably less phosphate (Scott, 1988). The limestone in the Tampa is white to yellowish gray, fossiliferous and variably sandy and clayey mudstone, wackestone and packstone with minor to no phosphate grains. Sand and clay beds are like those in the undifferentiated Arcadia Formation. Mollusks and corals are common in the Tampa Member as molds and casts, silicified pseudomorphs and original shell material. The Tampa Member and the lower part of the Arcadia Formation form the upper part of the Floridan aquifer system (FAS) in parts of southern Florida (Miller, 1986; Scott, 1991). Lithology: Major:{limestone}, Minor:{dolostone,sand,clay}, Incidental:{coral} 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] |
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