| Deposit ID | 10013472 |
|---|---|
| MRDS ID | D009781 |
| Record type | Site |
| Current site name | Pinos Altos Mine |
| Alternate or previous names | Cyprus Pinos Altos |
| Related records | 10135665 |
| Geographic coordinates: | -108.2384, 32.88567 (WGS84) |
|---|---|
| Elevation | 2103 |
| Location accuracy | 250(meters) |
| Relative position | ABOUT 8 MILES N 12 E OF SILVER CITY. |
Political divisions (FIPS codes)
Grant(county)
New Mexico(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Twin Sisters(quadrangle 1:24,000 scale)
Silver City(quadrangle 1:100,000 scale)
Silver City(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Upper Gila-Mangas(hydrologic unit)
Upper Gila(hydrologic accounting unit)
Upper Gila(hydrologic subregion)
Lower Colorado(hydrologic region)
Federal lands
Gila National Forest(National Forest)
National Forest FS(Type of land area)
FS(Federal land areas administered by FS)
| Country | State | County |
|---|---|---|
| United States | New Mexico | Grant |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| New Mexico | 016S | 014W | 25,36 | S2 (25); N2 (36) | New Mexico |
| Commodity | Importance |
|---|---|
| Copper | Primary |
| Zinc Critical | Primary |
| Silver | Primary |
| Gold | Secondary |
| Bismuth Critical | Secondary |
| Arsenic Critical | Secondary |
| Materials | Type of material |
|---|---|
| Argentite | Ore |
| Bismuthinite | Ore |
| Bornite | Ore |
| Chalcocite | Ore |
| Chalcopyrite | Ore |
| Copper | Ore |
| Covellite | Ore |
| Silver | Ore |
| Sphalerite | Ore |
| Tetrahedrite | Ore |
| Calcite | Gangue |
| Garnet | Gangue |
| Goethite | Gangue |
| Hematite | Gangue |
| Kaolinite | Gangue |
| Limonite | Gangue |
| Magnetite | Gangue |
| Marcasite | Gangue |
| Pyrite | Gangue |
| Pyrrhotite | Gangue |
| Quartz | Gangue |
| Rhodonite | Gangue |
| Sericite | Gangue |
| Model code | 59 |
|---|---|
| USGS model code | 18b |
| Deposit model name | Skarn Cu |
| Mark3 model number | 8 |
| Host or associated | Associated |
|---|---|
| Rock type | Plutonic Rock > Mafic Intrusive Rock > Diorite |
| Rock unit name | Pinos Altos Quartz Monzonite Stock; |
| Rock description | Pinos Altos Quartz Monzonite Stock; |
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Carbonate > Limestone |
| Rock unit name | Lake Valley;Oswaldo;Syrena;Beartooth |
| Rock description | Lake Valley;Oswaldo;Syrena;Beartooth |
| (1) | -108.2384, 32.88567 |
|---|
| General form | LENSES |
|---|---|
| Dip | } |
| Length | 762M |
| Width | 304.8M |
| Depth to top | 121.92M |
| Depth to bottom | 457.2M |
| Development status | Prospect |
|---|---|
| Commodity type | Metallic |
| Deposit size | Medium |
| Significant | No |
| Discovery year | 1948 |
| Discoverer | U.S. Smelting, Refining And Mining Co. |
| District name | Pinos Altos District |
|---|
| Ownership category | National Forest |
|---|
| Type | Operator |
|---|---|
| Owner | Boliden Minerals Corp., Silver City, N.M. ; Cyprus Minerals/St. Cloud Mining Co. Joint V |
| First year | 1982 |
| Last year | 1987 |
| Type | Owner |
|---|---|
| Owner | Exxon Minerals Co. |
| Home office | Tucson, Az. |
| First year | 1972 |
| Year | 1990 | ||||||||||||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Period | 1987-1990 | ||||||||||||||||||||||||||||
| Description | Cp_Grade: ^2.39% Cu, 3.61 Opt Ag, 0.010 Opt Au | ||||||||||||||||||||||||||||
| |||||||||||||||||||||||||||||
| Year | 1994 | |||||||||||||||||||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Period | 1987-1994 | |||||||||||||||||||||||||||||||||||
| Description | Cp_Grade: ^4.31% Cu, 2.63% Zn, 2.73 Opt Ag, 0.028 Opt Au | |||||||||||||||||||||||||||||||||||
| ||||||||||||||||||||||||||||||||||||
| Type | In-situ | |||||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Estimate year | 1978 | |||||||||||||||||||||
| Total resources | 3338000mt ore | |||||||||||||||||||||
| ||||||||||||||||||||||
| Type | In-situ | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Estimate year | 1987 | ||||||||||||||
| Total resources | 460000mt ore | ||||||||||||||
| |||||||||||||||
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | D009781 |
FINNEL, T. L., 1976 USGS MISC. FIELD STUDIES MAP, MF-779
MCKNIGHT, J. F., AND FELLOWS, M. L., 1978 ARIZONA GEOLOGICAL SOCIETY DIGEST, VOL 11, P. 1-8
ENGINEERING AND MINING JOURNAL, JUNE 1979, VOL 180, NO 6, P. 35, 39
NMBMMR GENERAL FILE DATA
OSTERBERG, M.W., ET. AL., 1992, ORE CONTROLS AT THE CYPRUS PINOS ALTOS CU ZN AG SKARN DEPOSIT, NEW MEXICO: SME/AIME PREPRINT 92-13, 11 P.
OSTERBERG, M. AND MULLER, P., 1994, GEOLOGY OF THE CYPRUS PINOS ALTOS DEPOSIT: CYPRUS-AMAX UNPUBLISHED REPORT, 29 P.
OSTERBERG AND MULLER (1994), P. 3
(1,2) OSTERBERG AND MULLER (1994) P. 3-4.
| Subject category | Comment text |
|---|---|
| Deposit | DEPOSIT CONSISTS OF TWO TYPES OF SKARN OCCURRING AS 25,000 TO 500,000 ST OREBODIES. EARLY (STAGE 1) SKARNS CONSIST OF RETROGRADE CALCITE-RHODONITE-PYRITE-SPHALERITE- MAGNETITE-HEMATITE MINERALIZATION OVERPRINTING PROGRADE GARNET SKARNS IN SYRENA FM. LIMESTONE ASSOCIATED WITH POTASSIC-ALTERED DIORITE INTRUSIVES. LATE (STAGE 2) SKARNS CONSIST OF CHLORITE-PYRITE-QUARTZ-CHALCOPYRITE-SPHALERITE-BARITE RETROGRADE MINERALIZATION OVERPRINTING PROGRADE GARNET SKARNS IN OSWALDO AND LAKE VALLEY FMS. LIMESTONE AND AS VEINS IN BEARTOOTH FM QUARTZITE ASSOCIATED WITH PROPYLITIC-ALTERED QUARTZ MONZONITE INTRUSIVES. STAGE 2 SKARN, RICH IN CU, BI, AND AS, OVERPRINTS EARLIER STAGE 1 ZN SKARN MINERALIZATION. WALL ROCK BETWEEN ORBODIES IS BARREN OF MINERALIZATION. EARLY ZN SKARNS ARE LOCATED AT TRANSITION FROM GARNET SKARN TO MARBLE IN THREE FAVORABLE BEDS IN THE SYRENA FM. LATE CU SKARN OVERPRINTS ON EARLY ZN SKARNS OCCUR ALONG NE-SW FRACTURE SETS. CU SKARNS ALSO OCCUR ALONG BASE OF OSWALDO |
| Deposit | FM/TOP OF LAKE VALLEY FM. AND ALONG NE-SW/NW-SE TRENDING CONJUGATE FAULT SETS IN BEARTOOTH FM. BEARTOOTH QUARTZITE ORES ARE CU-SILICA FLUX ORES. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-OCT-1982 | Menzie, David | New Mexico Bureau of Mines and Mineral Resources | |
| Updater | 15-OCT-1994 | Long, Keith R. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.