| Deposit ID | 10060367 |
|---|---|
| MRDS ID | TC10745 |
| Record type | Site |
| Current site name | Cerro Colorado Mountains Perlite Deposit |
| Geographic coordinates: | -111.25069, 31.6918 (WGS84) |
|---|
Political divisions (FIPS codes)
Pima(county)
Arizona(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Cerro Colorado(quadrangle 1:24,000 scale)
Sells(quadrangle 1:100,000 scale)
Nogales(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Upper Santa Cruz(hydrologic unit)
Santa Cruz(hydrologic accounting unit)
Middle Gila(hydrologic subregion)
Lower Colorado(hydrologic region)
Federal lands
ST(Federal land areas administered by ST)
| Country | State | County |
|---|---|---|
| United States | Arizona | Pima |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Gila and Salt River | 20S | 11E | 6,7,17,18 | S2 OF SW4 (06); W2 (07); SE4 OF SE4 (07); NW4 (17) | Arizona |
| Commodity | Importance |
|---|---|
| Perlite | Primary |
| Host or associated | Host | ||
|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Glassy Rock > Vitrophyre | ||
| |||
| (1) | -111.25069, 31.6918 |
|---|
| General form | STRINGERS GRADING TO LAYERS |
|---|---|
| Thickness | 60.96M |
| Development status | Occurrence |
|---|---|
| Commodity type | Non-metallic |
| Significant | No |
| Ownership category | State |
|---|
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | TC10745 |
PHILLIPS, K.A., 1987, ARIZONA INDUSTRIAL MINERALS: ARIZONA DEPARTMENT OF MINES AND MINERAL RESOURCES REPORT 4, 185 P.
SMITH, RUSSELL, 1966, GEOLOGY OF THE CERRO COLORADO MOUNTAINS, PIMA COUNTY, ARIZONA: ARIZONA GEOLOGICAL SOCIETY DIGEST V. 8, P. 131-145.
PEIRCE, H.W., 1990, ARIZONA GEOLOGICAL SURVEY INDUSTRIAL MINERALS CARD FILE.
CIMRI
| Subject category | Comment text |
|---|---|
| Deposit | DARK GREY TO PINKISH-GREY STRINGERS OF PERLITIC GLASS OCCUR IN INCREASING ABUNDANCE UP-SECTION UNTIL THE PERLITE BECOMES A 100-200 FT THICK, CONTINUOUS LAYER. THIN SECTIONS OF THESE UNITS REVEAL A HYPOCRYSTALLINE TEXTURE WITH 60 TO 80 PERCENT GLASS. THE GLASS IN THE PERLITE IS FRESH EXCEPT FOR SLIGHT ALTERATION ALONG PERLITIC CRACKS AND CONTAINS ABUNDANT TRICHITES BUT NO TRACE OF SHARDS OR FLOW TEXTURE. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-APR-1990 | Bolm, Karen S. | U.S. Geological Survey | |
| Updater | 01-DEC-1992 | Orris, Greta J. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.
These are landing pages for further research — the state agencies don't currently expose per-mine deep links.