| Lat / long: | 39.2216, -115.48394 |
| Primary: | Silver |
| Tertiary: | Copper, Manganese, Iron |
| Ore: | Silver, Chlorargyrite, Bromargyrite, Acanthite, Aurorite, Quartz, Pyrite, Iron |
| Gangue: | Calcite |
| Discovery year: | 1867 |
| Operation type: | Surface-Underground |
| Deposit type: | pluton-related polymetallic replacement |
| Production size: | Large |
| Development status: | Past Producer |
| Production years: | 1868-1888, 1911? |
| First production started: | 1868 |
| Last production ended: | 1888 |
| Host rock: | upper Hamburg Formation and lower Dunderberg Shale |
| Host type: | Shale,Limestone |
| Associated rock: | Seligman Stock and Monte Cristo Stock |
| Associated type: | Porphyry,Granodiorite |
| Structure: | The White Pine Range is a typical N-S-trending Basin and Range fault block composed of a sequence of Paleozoic carbonate and clastic sedimentary rocks intruded by two Cretaceous- age granitic stocks. |
| Alteration processes: | Deposit was oxidized |
| MRDS | M233758 |
| DEP | 10310457 |
| Reference | Long, K.R., DeYoung, J.H., Jr., and Ludington, S.D., 1998, Database of significant deposits of gold, silver, copper, lead, and zinc in the United States; Part A, Database description and analysis; part B, Digital database: U.S. Geological Survey Open-File Report 98-206, 33 p., one 3.5 inch diskette. |
| Reporter | Martin, Paul (Tingley, J.V.), LaPointe, D.D., Schruben, Paul G. |