| Lat / long: | 34.81343, -98.91536 |
| Primary: | Copper |
| Gangue: | Anorthosite |
| Orebody form: | IRREGULAR SHEETS |
| Discovery year: | 1938 |
| Operation type: | Unknown |
| Deposit type: | Hydrothermal Vein |
| Production size: | None |
| Development status: | Occurrence |
| Host rock: | Hale Spring Pegmatites Of Quanah Granite |
| Host type: | Pegmatite |
| Associated rock: | Raggedy Mountain Gabbro Group-Glen Mountains Layered Complex-Zone M;Post Oak Conglomerate Of Hennessey Group |
| Associated type: | Anorthosite |
| Structure: | Wichita Mountains, Glen Mountains |
| Tectonic: | Aulacogen |
| Alteration processes: | Malachite And Azurite From Chalcopyrite In Granitic Pegmatite Veins In Anorthosite, Weathered With Granite Wash |
| MRDS | DE01772 |
| DEP | 10021976 |
| Reference | {Deposit:: MERRITT, C.A., 1938, OKLAHOMA ACADEMY OF SCIENCE, PROCEEDINGS, V. 18, P. 51-55.}{Deposit:: MERRITT, C.A., 1939, ECONOMIC GEOLOGY, V. 34, NO. 3, P. 268-286 (P. 275-278).}{Deposit:: RODEBUSH, CLARENCE, SEPTEMBER 1936, WPA PROJECT 65-65-538, SHEET 427, OGS FILE.}{Deposit:: SPENCER, A.B., 1961, UNIVERSITY OF OKLAHOMA, M.S. THESIS, 46 P.} |
| Reporter | Fay, Robert O. |