Lat / long: | 33.79591, -110.49458 |
Primary: | Asbestos |
Ore: | Chrysotile |
Orebody form: | LINEAR |
Operation type: | Unknown |
Deposit type: | Vein |
Production size: | Small |
Development status: | Past Producer |
Host rock: | Mescal Limestone |
Host type: | Limestone |
Associated type: | Diabase,Plutonic Rock |
Structure: | Northwest-Trending Fractures Are Numerous Where The Southern Deposit Is Exposed By Mine Workings. As A Result Of Water Solution Along The Fractures, And Of Slumping Of The Blocks Bounded By The Fractures, Vertical Openings As Much As 2 Feet Wide Exist Throughout Much Of The Deposit. As A Result, The Ground Is Very Heavy - The Limestone Above And Below The Ore Zone Caves Readily. |
Tectonic: | Basin And Range |
Alteration processes: | Serpentinization |
MRDS | M003041 |
DEP | 10102486 |
Reference | {Deposit:: BROMFIELD, C.S., AND SHRIDE, A.F., 1956, MINERAL RESOURCES OF THE SAN CARLOS INDIAN RESERVATION, ARIZONA: U.S. GEOLOGICAL SURVEY BULLETIN 1027-N, P. 661.}{Deposit:: STEWART, L.A., 1955, CHRYSOTILE-ASBESTOS DEPOSITS OF ARIZONA: USGS INFORMATION CIRCULAR 7706, P. 53.}{Deposit:: STEWART, HAURY, 1947, ARIZONA ASBESTOS DEPOSITS, GILA COUNTY, ARIZONA: U.S. BUREAU OF MINES REPORT OF INVESTIGATION 4100.}{Deposit:: PHILLIPS, K.A., 1987, ARIZONA INDUSTRIAL MINERALS: ARIZONA DEPARTMENT OF MINES AND MINERAL RESOURCES MINERAL REPORT 4, 185 P.}{Other Database:: CIMRI} |
Reporter | Gere, W., Hall, R. K. (Creasey, S. C.), Orris, Greta J. |