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Schulter, Okmulgee Co., Oklahoma, USA

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Latitude & Longitude (WGS84): 35° 31' 0'' North , 95° 57' 30'' West
Latitude & Longitude (decimal): 35.51667,-95.95833
GeoHash:G#: 9y7f03t78
Köppen climate type:Cfa : Humid subtropical climate


Ref.: Rocks & Minerals: 72(4): 252-264.

Mineralization is on area coal mine dumps.


Mineral List


4 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

Paleozoic
252.17 - 541 Ma



ID: 3187973
Paleozoic sedimentary rocks

Age: Paleozoic (252.17 - 541 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]

Pennsylvanian
298.9 - 323.2 Ma



ID: 2834588
Calvin Sandstone

Age: Pennsylvanian (298.9 - 323.2 Ma)

Stratigraphic Name: Calvin Sandstone

Description: OKLAHOMA CITY- Medium-grained, thin-bedded to massive sandstone nd silty shale. Thickness ranges from 230 to about 440 feet. FORT SMITH- Shale and sandstone. ARDMORE-SHERMAN- Sandstone, brown, medium-grained, with some gray shale; thickness, 40 to 320 feet, thinner southward.

Comments: Area of Coalgate quad, Coal and Hughes Cos, OK in Arkoma basin and Chautauqua platform where unit is exposed in north-central and western parts of quad. Composed of massive and thin-bedded sandstone with some shaly beds in upper part, 140-240 ft thick. For nearly 140 ft upward from base, is massive but not very hard sandstone. In southern part of outcrop, lower sandy member becomes shaly, and even the massive beds which occur are more friable than same deposits in northern part of quad. Near middle of lower sandstone member, west of Sand Creek, there is a shaly and slightly calcareous bed which contains hematite; bright-red color of this bed upon weathering is a characterisitic feature of unit. Upper part of unit is least shaly in northern part of area, and many beds are hard and weather into slabs and hard plates. Upper 90-100 ft here contains two, and in places more, shaly beds 10-20 ft thick. Sandstone beds of this upper portion decrease southwestward from 40 ft to thin layers interstratified with shales. (Taff, 1901).

Lithology: Major:{sandstone}, Minor:{shale}

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



This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.
 
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