| Lat / long: | 33.12343, -109.36759 |
| Primary: | Copper |
| Secondary: | Silver |
| Ore: | Chalcocite, Chalcopyrite, Chrysocolla, Cuprite, Malachite |
| Gangue: | Limonite, Magnetite |
| Orebody form: | IRREGULAR AND IN NARROW STRINGERS |
| Discovery year: | 1872 |
| Operation type: | Unknown |
| Production size: | Small |
| Development status: | Producer |
| First production started: | 1937 |
| Last production ended: | 1951 |
| Host type: | Schist |
| Associated rock: | Pinal Schist;Precambrian Granite Basement;Morenci Granite Porphyry |
| Associated type: | Quartz Monzonite |
| Structure: | Normal Faulting Confined To Pre-Tertiary Rocks, Ore Occurs In Narrow Stringers Within Ore Zone In Monzonite Porphyry |
| Tectonic: | Metcalf Fault Block Region |
| Alteration processes: | Minor |
| MRDS | M800395 |
| DEP | 10048272 |
| Reference | {Deposit:: ABGMT-USBM FILE DATA}{Deposit:: ARIZONA DEPARTMENT OF MINERAL RESOURCES FILE DATA, UNDER STEVENS MINE}{Deposit:: BLM DISTRICT SHEET 837}{Deposit:: BENNETT, K.C., 1975, GEOLOGY AND ORIGIN OF THE BRECCIAS IN THE MORENCI-METCALF DISTRICT, GREENLEE COUNTY, ARIZONA: M.S. THESIS, UNIVERSITY OF ARIZONA, 153P.} |
| Reporter | Calder, Susan R. |