| Lat / long: | 38.45302, -113.07386 |
| Primary: | Copper |
| Tertiary: | Tungsten |
| Ore: | Bornite, Brochantite, Chalcopyrite, Chrysocolla, Grossularite, Muscovite, Powellite, Scheelite, Tenorite |
| Gangue: | Diopside, Gypsum, Idocrase, Magnetite |
| Orebody form: | IRREGULAR-VEINS |
| Discovery year: | 1960 |
| Operation type: | Unknown |
| Production size: | Small |
| Development status: | Past Producer |
| First production started: | 1962 |
| Host rock: | Toroweap Formation |
| Host type: | Dolomite |
| Associated type: | Quartz Monzonite |
| Structure: | Basin And Range, Assymetric North Plunging Anticline (Rocky Range) |
| Tectonic: | Paleozoic Miogeosyncline |
| Alteration processes: | Bleached, Marbleized, Skarn |
| MRDS | D005834 |
| DEP | 10101625 |
| Reference | {Deposit:: UTAH GEOLOGICAL ASSOCIATION, 1973 GEOLOGY OF THE MILFORD AREA PUBLICATION NO 3}{Deposit:: WHELAN, J.A., THE ROCKY MINING DISTRICT, IN PRESS, UTAH GEOLOGICAL AND MINERAL SURVEY.}{Production:: EVERTS, M L, 1979, ON-SITE INVESTIGATION: UTAH GEOLOGICAL AND MINERAL SURVEY} |
| Reporter | Everts, Michael L. |