| Deposit ID | 10039941 |
|---|---|
| MRDS ID | M051145 |
| Record type | Site |
| Current site name | Unnamed Copper Deposit |
| Geographic coordinates: | -111.02069, 32.50094 (WGS84) |
|---|
Political divisions (FIPS codes)
Pima(county)
Arizona(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Tortolita Mountains(quadrangle 1:24,000 scale)
Casa Grande(quadrangle 1:100,000 scale)
Tucson(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
LG(Federal land areas administered by LG)
| Country | State | County |
|---|---|---|
| United States | Arizona | Pinal |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Gila and Salt River | 011S | 013E | 04 | Arizona |
| Commodity | Importance |
|---|---|
| Copper | Primary |
| Materials | Type of material |
|---|---|
| Chrysocolla | Ore |
| Malachite | Ore |
| Epidote | Gangue |
| Hematite | Gangue |
| Limonite | Gangue |
| Quartz | Gangue |
| Specularite | Gangue |
| Host or associated | Host |
|---|---|
| Rock type | Plutonic Rock > Granitoid > Quartz Monzonite |
| Rock unit name | San Maniego;Tortolita Quartz Monzonite |
| Rock description | San Maniego;Tortolita Quartz Monzonite |
| Host or associated | Host |
|---|---|
| Rock type | Plutonic Rock > Mafic Intrusive Rock > Diorite |
| (1) | -111.02069, 32.50094 |
|---|
| General form | IRREGULAR |
|---|
| Development status | Prospect |
|---|---|
| Commodity type | Metallic |
| Deposit size | Small |
| Significant | No |
| District name | Owl Head District |
|---|
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | M051145 |
BANKS, N., DOCKTOR, R., AND BRISKEY, J., 1976, MAPS OF MINES ETC, IN THE TORTOLITA MTNS QUAD, MAP A, OPEN FILE
| Subject category | Comment text |
|---|---|
| Deposit | MINERALIZED DISCONTINUOUS QUARTZ VEINS. QUARTZ VEINS "MINED OUT" AND NO LONGER EXPOSED IN WORKINGS. ALTERED WALL ROCK, WHERE PRESENT, APPEARS TO BE THE RESULT OF SURFICIAL WEATHERING RATHER THAN HYDROTHERMAL ALTERATION. QUARTZ VEINS OFTEN BRECCIATED AND RECEMENTED WITH QUARTZ AND (OR) SPECULARITE. SULFIDE MINERALS APPARENTLY ACCOMPANIED SPECULARITE. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-SEP-1976 | Briskey, Joseph A. | U.S. Geological Survey | |
| Updater | 01-APR-1981 | Harner, Joy L. (Peterson, Jo) | 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.