| Lat / long: | 46.49166, -81.06645 |
| Primary: | Copper, Nickel, PGE, Gold, Cobalt, Selenium, Tellurium, Silver |
| Discovery year: | 1960 |
| Operation type: | Unknown |
| Production size: | Yes |
| Development status: | Producer |
| First production started: | 1967 |
| Last production ended: | 1978 |
| Host rock: | Copper Cliff Offset (Sudbury Sublayer) |
| Host type: | Diorite |
| Structure: | Apophysis Of The Sublayer At The Base Of This Nickel Irruptive. |
| Tectonic: | Intracratonic Intrusion Triggered By Meteoritic Impact. |
| MRDS | ISM0187 |
| DEP | 10106771 |
| Reference | {Deposit:: ONTARIO GEOLOGICAL SURVEY, SMDR000910.}{Deposit:: SOUCH, B.E., PODOLSKY, T., AND GEOLOGICAL STAFF, INTERNATIONAL NICKEL COMPANY OF CANADA, LIMITED, 1969, THE SULPHI-DE ORES OF SUDBURY--THEIR PARTICULAR RELATIONSHIP TO A DISTINC-TIVE INCLUSION-BEARING FACIES OF THE NICKEL IRRUPTIVE, IN WILS-ON, H.D.B., ED., MAGMATIC ORE DEPOSITS: ECONOMIC GEOLOGY MONO-GRAPH NO. 4, P. 252-261.}{Deposit:: PATTISON, E.F., 1979, THE SUDBURY SUBLAYER: CANADIAN MINERALOGIST, V. 17, PT. 2, P. 257-274.} |
| Reporter | Zwartendyk, Jan |