| Lat / long: | 35.50454, -79.43087 |
| Primary: | Talc-Soapstone |
| Secondary: | Mica |
| Ore: | Pyrophyllite |
| Gangue: | Chloritoid, Quartz |
| Orebody form: | TABULAR AND LENSES |
| Discovery year: | 1902 |
| Operation type: | Unknown |
| Production size: | Medium |
| Development status: | Past Producer |
| First production started: | 1903 |
| Last production ended: | 1990 |
| Host type: | Tuff |
| Associated type: | Rhyolite |
| Structure: | Deposit Deformed By The Glendon Fault. Regional Folds Ne-Trending, Overturned To The East (West-Dipping Limbs)., Overturned And Attenuated Fold From Reverse Faulting Along The Glendon Fault. |
| Alteration processes: | Pyrophyllite Appears To Be Controlled By A Fracture System That Predates The Last Movement On The Glendon Fault. |
| MRDS | RE00539 |
| DEP | 10055252 |
| Reference | {Deposit:: STUCKEY, J.L., 1967, PYROPHYLLITE DEPOSITS IN NORTH CAROLINA: NORTH CAROLINA DEPARTMENT OF CONSERVATION AND DEVELOPMENT, DIVISION OF MINERAL RESOURCES BULLETIN 80}{Deposit:: KLEIN, T.L., SITE VISITS, 1980-1986} |
| Reporter | Klein, T.L. |