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Pavitte Copper prospect (Bailey Place; White Eagle Mine), Burnet Co., Texas, USA

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Latitude & Longitude (WGS84): 30° 46' 3'' North , 98° 17' 59'' West
Latitude & Longitude (decimal): 30.76743,-98.29976
Köppen climate type:Cfa : Humid subtropical climate


5 miles NW of Burnet.

Mineral List


12 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

Proterozoic
541 - 2500 Ma



ID: 2832895
Valley Spring Gneiss

Age: Proterozoic (541 - 2500 Ma)

Stratigraphic Name: Valley Spring Gneiss

Comments: Llano Series (from the Wilmarth Lexicon, USGS Bull. 896); Grenville Series Central Texas (Geol. Map of Texas, 1992, Bur. Econ. Geol.) Lower fm. of Llano series, also called Llano Group (Mutis-Duplat, 1982) in Llano Mason, Gillespie, and Burnet Counties.

Lithology: Major:{paragneiss}, Minor:{marble}

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.

References

Rocks & Minerals (1991): 66(3): 196-224.

 
Mineral and/or Locality  
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