| Lat / long: | 38.2411, -109.26375 |
| Primary: | Copper |
| Ore: | Chalcocite, Chrysocolla, Covellite, Malachite |
| Gangue: | Pyrite |
| Orebody form: | TABULAR, LENS, PODS |
| Operation type: | Unknown |
| Production size: | Small |
| Development status: | Past Producer |
| Host rock: | Dakota Formation |
| Host type: | Shale,Sandstone,Conglomerate |
| Structure: | Clastic Units - 10 - 15 Ft Thick Separated By 30 Ft Barren Gray-Green Shale, Lisbon Valley Fault. |
| Tectonic: | Stable Platform |
| MRDS | DB00030 |
| DEP | 10015032 |
| Reference | {Deposit:: WEIR, G.W., AND PUFFETT, W.P., 1982, INCOMPLETE MANUSCRIPT ON STRATIGRAPHY AND STRUCTURAL GEOLOGY AND URANIUM-VANADIUM DEPOSITS OF THE LISBON VALLEY AREA, UTAH-COLORADO: U.S. GEOLOGICAL SURVEY OPEN-FILE REPORT 81-39, 292P.}{Deposit:: MONISON, S.J. AND PARRY, W.T., 1986, FORMATION OF CARBONATE-SULFATE VEINS ASSOCIATED WITH COPPER ORE DEPOSITS FROM SALINE BASIN BRINES, LISBON VALLEY, UTAH: ECONOMIC GEOLOGY, V. 81, P. 1853-1866.}{Reserve-Resource:: JONES, H., 1978} |
| Reporter | Jones, Harold H., Lindsey, David A. |