| Lat / long: | 38.15302, -113.85138 |
| Tertiary: | Copper |
| Ore: | Chrysocolla, Malachite |
| Gangue: | Limonite, Pyrite, Quartz |
| Orebody form: | TABULAR |
| Operation type: | Unknown |
| Deposit type: | Vein |
| Production size: | None |
| Development status: | Occurrence |
| Host type: | Ash-Flow Tuff |
| Associated rock: | Intracauldron Unit Of The Wah Wah Springs Tuff Member Of The Needles Range Formation |
| Associated type: | Ash-Flow Tuff |
| Structure: | Pioche Mineral Belt, Sevier Orogenic Belt., Fracture Zone At N 60 W 71 Ne To Vertical |
| Tectonic: | Basin And Range Extension |
| Alteration processes: | Propylitic And Weak Argillic |
| MRDS | M058927 |
| DEP | 10088830 |
| Reference | {Deposit:: GRANT, S.K., AND BEST, M.G., 1979, GEOLOGIC MAP OF THE PINTO SPRINGS AND PART OF THE ATCHISON CREEK QUADRANGLES, BEAVER AND IRON COUNTIES, UTAH: U.S. GEOLOGICAL SURVEY OPEN FILE REPORT 79-1656.}{Deposit:: SHUBAT, M.A., 1985, ON-SITE INVESTIGATION, UGMS} |
| Reporter | Shubat, Michael A. |