Mine detail: Kiowa Copper Company Prospect

Previously called ''

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Location

Lat / long:

34.82843, -98.91869

Resource(M)

Primary:	Copper
Orebody form:	VEINS
Discovery year:	1904

Production

Operation type:	Unknown
Deposit type:	Hydrothermal Vein
Production size:	Small
Development status:	Past Producer
Production years:	BEFORE 1904

Geology

Host rock:	Hale Spring Pegmatites Of Quanah Granite
Host type:	Pegmatite
Associated rock:	Raggedy Mountain Gabbro Group-Glen Mountains Layered Complex Zone G;Post Oak Conglomerate In Hennessey Group
Associated type:	Troctolite
Structure:	Wichita Mountains, Glen Mountains
Tectonic:	Aulacogen
Alteration processes:	Weathered Olivine Gabbro In Hennessey Group

References

MRDS	DE01769
DEP	10098090
Reference	{Deposit:: BAIN, H.F., 1904, U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 31, P. 82-93 (P. 89, 92).}{Deposit:: SHEAD, A.C., 1929, OGS BULLETIN 14, 138 P. (P. 4, 18, 29, 87).}{Deposit:: RODEBUSH, CLARENCE, SEPTEMBER 1936, WPA PROJECT 65-65-538, SHEET 425, KIOWA CO., OKLAHOMA, OGS FILE.}{Deposit:: SPENCER, A.B., 1961, UNIVERSITY OF OKLAHOMA, M.S. THESIS, 46 P.}
Reporter	Fay, Robert O.