| Lat / long: | 46.40306, -90.3079 |
| Primary: | Iron |
| Ore: | Goethite, Hematite |
| Orebody form: | STRATABOUND |
| Discovery year: | 1848 |
| Operation type: | Unknown |
| Production size: | Small |
| Development status: | Past Producer |
| Production years: | 1887 TO 1913 EXCEPT FOR 1888-1894, AND 1911. |
| First production started: | 1887 |
| Last production ended: | 1913 |
| Host rock: | Ironwood Formation |
| Host type: | Iron Formation |
| Structure: | N-Dipping Sediments; Regional Trends Are East To West., An E-W Linear Iron Formation Going From Gogebic, Mi, To Ironwood, Mi, And To Mellen, Wi, And A Bit Farther W. |
| Tectonic: | Canadian Shield |
| Alteration processes: | Gogebic Iron Range Is In The Chlorite Metamorphic Zone In The Least Metamorphosed Area Of The Upper Peninsula. |
| MRDS | W062002 |
| DEP | 10082654 |
| Reference | {Deposit:: HEYL, A.V., JR., AGNEW, A.F., LYONS, E.J., AND BEHRE, C.H., JR., WITH SPECIAL SECTIONS BY FLINT, A.E., 1959, THE GEOLOGY OF THE UPPER MISSISSIPPI VALLEY ZINC-LEAD DISTRICT: U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 309, 310 P}{Deposit:: SCHMIDT, 1980: USGS BULLETIN 1460}{Production:: LAKE SUPERIOR IRON ORE ASSOCIATION, 1952, P. 53.} |
| Reporter | Sutphin, David M. (Cannon, W. F.), Mason Jr., G.T. |