| Lat / long: | 30.63271, -98.71173 |
| Primary: | Vermiculite, Stone, Talc-Soapstone |
| Ore: | Serpentine, Talc, Vermiculite |
| Gangue: | Chlorite, Magnetite, Tremolite |
| Orebody form: | TABULAR, LENSE |
| Discovery year: | 1935 |
| Operation type: | Unknown |
| Production size: | Small |
| Development status: | Past Producer |
| Host rock: | Packsaddle Schist |
| Host type: | Schist,Serpentinite |
| Associated type: | Pegmatite,Granite |
| Alteration processes: | Serpentinite Altered To Soapstone Probably As Result Of Intrusion By Granite. Soapstone Alteration Forms An Enveloped Around A Serpentinite Core. Serpentinite May Be Metamorphosed Dunite. |
| MRDS | TC40197 |
| DEP | 10065160 |
| Reference | {Deposit:: CLABAUGH, S.E., AND BARNES, V.E., 1959, VERMICULITE IN CENTRAL TEXAS: TEXAS BUREAU OF ECONOMIC GEOLOGY REPT. INVEST. 40, P. 19-23.}{Deposit:: BARNES, V.E., 1945, SOAPSTONE AND SERPENTINE IN THE CENTRAL MINERAL REGION OF TEXAS, IN TEXAS MINERAL RESOURCES: UNIV. TEXAS PUB. 4301, P. 55-91.}{Other Database:: CIMRI} |
| Reporter | Long, Keith R. |