| Deposit ID | 10023693 |
|---|---|
| MRDS ID | I001102 |
| Record type | Site |
| Current site name | D Hill Area |
| Alternate or previous names | Gypsite Quarries |
| Geographic coordinates: | -110.38372, 31.35903 (WGS84) |
|---|---|
| Location accuracy | 1000(meters) |
| Relative position | Estimated, Used Center Of Section 11. |
Political divisions (FIPS codes)
Cochise(county)
Arizona(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Campini Mesa(quadrangle 1:24,000 scale)
Nogales(quadrangle 1:100,000 scale)
Nogales(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Upper San Pedro(hydrologic unit)
San Pedro-Willcox(hydrologic accounting unit)
Middle Gila(hydrologic subregion)
Lower Colorado(hydrologic region)
Federal lands
Coronado National Forest(National Forest)
National Forest FS(Type of land area)
FS(Federal land areas administered by FS)
| Country | State | County |
|---|---|---|
| United States | Arizona | Cochise |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Gila and Salt River | 24S | 019E | 2,11,12,13,14,15 | Arizona |
| Commodity | Importance |
|---|---|
| Gypsum-Anhydrite | Primary |
| Materials | Type of material |
|---|---|
| Gypsum | Ore |
| Host or associated | Host |
|---|---|
| Rock type | Unconsolidated Deposit > Clay, Mud |
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock > Shale |
| (1) | -110.38372, 31.35903 |
|---|
| Development status | Past Producer |
|---|---|
| Commodity type | Non-metallic |
| Significant | No |
| Ownership category | |
|---|---|
| Area name | Coronado National Forest |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | I001102 |
PHILLIPS, K.A., 1987, ARIZONA INDUSTRIAL MINERALS: ARIZONA DEPARTMENT OF MINES AND MIENRAL RESOURCES REPORT 4, 185 P
CIMRI
| Subject category | Comment text |
|---|---|
| Deposit | THE DEPOSITS OF TALC ARE UP TO 60 M LONG, 30 M WIDE, AND 30 M DEEP AND ARE FOUND WITHIN THE DIABASE AND CARBONATE ROCKS. THE DEPOSITS ARE DERIVED FROM HYDROTHERMAL METAMORPHISM OF THE DOLOMITIC LIMESTONE AND EXTEND OVER SEVERAL KM IN THE PONTA GROSSA AND CASTRO REGION. ONLY SUPERFICIALLY EXPOSED BODIES ARE MINED. OVERBURDEN IS 3-4 M DEEP. |
| Deposit | GYPSUM-GYPSITE OVERLIES CLAY AND SHALE. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-OCT-91 | 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.