| Lat / long: | 47.44765, -115.49795 |
| Primary: | Lead, Silver, Copper, Zinc |
| Ore: | Chalcopyrite, Galena, Sphalerite, Tetrahedrite |
| Operation type: | Unknown |
| Deposit type: | Vein |
| Production size: | None |
| Development status: | Occurrence |
| Host rock: | Wallace Formation |
| Host type: | Quartzite |
| Structure: | A Major Structural Grain Trends Nw And Consists Of Subparallel Faults And Folds. Major Fault Is The Osburn. This Fault Seems To Demarcate To Change In Folding Form With Folds To The North Showing Signs Of More Intense Structural Deformation Than Those To The South |
| Tectonic: | Belt Basin |
| Alteration processes: | Hydrothermal Bleaching Is Common Within A Belt Approx 1 Mi Wide Along The North Side Of The Osburn Fault Zone. It Has Been Used As A Guide To Ore Deposits |
| MRDS | D004167 |
| DEP | 10010490 |
| Reference | {Deposit:: WALLACE, R. E. AND HOSTERMAN, J. W., 1956, RECONNAISSANCE GEOLOGY OF WESTERN MINERAL COUNTY MON*USGS BULL 1027-MP 605.}{Deposit:: SWALLOW, G. C., INSPECTOR OF MINES AND DEPUTY INSPECTOR OF MINE*P. 95, 11/30/1889.} |
| Reporter | Chesson, Sharon A. (Orris, Greta J.) |