| Lat / long: | 45.48833, -90.05677 |
| Primary: | Copper |
| Secondary: | Gold |
| Tertiary: | Zinc |
| Ore: | Bornite, Chalcocite, Chalcopyrite, Electrum, Gold, Magnetite, Pyrite, Pyrrhotite, Tennantite, Tetrahedrite |
| Discovery year: | 1979 |
| Operation type: | Unknown |
| Production size: | Unknown |
| Development status: | Prospect |
| Host rock: | Quartz-Sericite Schists |
| Host type: | Rhyolite |
| Structure: | Steeply Dipping Isoclinally Folded To Locally Gently Dipping Volcanic Sections., Main Zone Is At The Western Edge Of A Felsic Center Developed On The Flanks Of A Mafic Volcanic-Intrusive Complex |
| Tectonic: | Back-Arc Basin. Laberge Suggests That These Metasediments May Have Been Deposited In A Number Of Basins Formed By Fault Grabens During The Late Penokean Orogeny. |
| Alteration processes: | Upper Greenschist To Lower Amphibolite Facies. In The Main Zone There Is Partial Replacement Of Previously Deposited Exhalite. |
| MRDS | W060003 |
| DEP | 10082577 |
| Reference | {Deposit:: DEMATTIES, 1990, ECON. GEOL., V.85, P. 1908-1916}{Deposit:: LABERGE, G.L., ED., VOLCANOGENIC MASSIVE SULFIDE DEPOSITS OF NORTHERN WISCONSIN--A COMMEMORATIVE VOLUME: INSTITUTE ON LAKE SUPERIOR GEOLOGY, PROCEEDINGS, V. 42, PT. 2.}{Reserve-Resource:: LABERGE, 1996.} |
| Reporter | Nicholson, S.W., Sutphin, David M., Mason Jr., G.T. |