| Lat / long: | 40.60836, -86.66387 |
| Primary: | Zinc, Lead |
| Tertiary: | Sulfur |
| Ore: | Sphalerite |
| Gangue: | Dolomite |
| Operation type: | Unknown |
| Production size: | None |
| Development status: | Occurrence |
| Host rock: | Wabash, Reefs Make Up A Significant Part Of This Formation Large Barrie R-Like Banks Occur Around The Basins. Smaller Reefs Dot The State. Ree F Facies Are Porous Dolomite. Reefs Are Associated With Mississippi-Va Lley Type Deposits Elsewhere (Shaffer, 1981) |
| Host type: | Dolomite |
| Structure: | Cincinnati Arch, A Stable Paleozoic Platform Between Subsiding Mich Igan And Illinois Basins. Trends Nw/Se. |
| Tectonic: | Locale Is Atop Cincinnati Arch |
| Alteration processes: | Dolomitization, Dissolution |
| MRDS | W031992 |
| DEP | 10080657 |
| 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. |