| Lat / long: | 34.82843, -98.91869 |
| Primary: | Copper |
| Orebody form: | VEINS |
| Discovery year: | 1904 |
| Operation type: | Unknown |
| Deposit type: | Hydrothermal Vein |
| Production size: | Small |
| Development status: | Past Producer |
| Production years: | BEFORE 1904 |
| 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 |
| 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. |