| Lat / long: | 40.76113, -86.39998 |
| Primary: | Zinc |
| Tertiary: | Sulfur |
| Ore: | Sphalerite |
| Gangue: | Calcite, Dolomite |
| Operation type: | Unknown |
| Production size: | None |
| Development status: | Occurrence |
| Host rock: | Wabash, Reefs, Make Up A Significant Part Of This Formation Large Barri Er-Like Banks Occur Around The Basins. Smaller Reefs Dot The State. Re Ef Rocks Are Porous Dolomite. Reefs Are Associated With Mississippi-Va Lley Type Deposits Elsewhere (Shaffer, 1981) |
| Host type: | Limestone |
| Structure: | Cincinnati Arch-Trends Nw-Se In North-Central Indiana |
| Tectonic: | Atop Cincinnati Arch, A Stable Paleozoic Platform Between Subsidin G Michigan And Illinois Basins. |
| Alteration processes: | Dolomitization |
| MRDS | W031990 |
| DEP | 10080655 |
| Reference | SHAFFER, NELSON R., 1981, POSSIBILITY OF MISSISSIPPI VALLEY-TYPE MI NERAL DEPOSITS IN INDIANA, INDIANA GEOLOGICAL SURVEY SPECIAL REPORT 21 , 49P |
| Reporter | Sutphin, David M. |