| Deposit ID | 10014032 |
|---|---|
| MRDS ID | D010645 |
| Record type | Site |
| Current site name | Copper Hill Mine |
| Geographic coordinates: | -106.59754, 37.42308 (WGS84) |
|---|---|
| Elevation | 3599 |
| Relative position | 0.52 MILES S 26 W FROM SUMMITVILLE |
Political divisions (FIPS codes)
Rio Grande(county)
Colorado(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Summitville(quadrangle 1:24,000 scale)
Antonito(quadrangle 1:100,000 scale)
Durango(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Alamosa-Trinchera(hydrologic unit)
Rio Grande Headwaters(hydrologic accounting unit)
Rio Grande Headwaters(hydrologic subregion)
Rio Grande(hydrologic region)
Federal lands
Rio Grande National Forest(National Forest)
National Forest FS(Type of land area)
FS(Federal land areas administered by FS)
| Country | State | County |
|---|---|---|
| United States | Colorado | Rio Grande |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| New Mexico | 037N | 004E | 30 | NE OF SW | Colorado |
| Commodity | Importance |
|---|---|
| Gold | Primary |
| Silver | Primary |
| Copper | Secondary |
| Model code | 85 |
|---|---|
| USGS model code | 22c |
| Deposit model name | Polymetallic veins |
| Mark3 model number | 46 |
| Host or associated | Associated | ||||
|---|---|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Quartz Latite | ||||
| Rock unit name | Quartz Latite Of South Mountain;Summitville Andesite | ||||
| Rock description | Quartz Latite Of South Mountain;Summitville Andesite | ||||
| |||||
| Host or associated | Associated |
|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Intermediate Volcanic Rock > Andesite |
| Host or associated | Host |
|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Quartz Latite |
| Rock unit name | Quartz Latite Of South Mountain;Summitville Andesite |
| Rock description | Quartz Latite Of South Mountain;Summitville Andesite |
| (1) | -106.59754, 37.42308 |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | San Juan Volcanic Field |
| Type of structure | Local |
| Structure description | Platoro Caldera, Summitville Caldera, Summitville Fault, South Mountain Dome |
| Development status | Past Producer |
|---|---|
| Commodity type | Metallic |
| Deposit size | Small |
| Significant | No |
| District name | Summit (Summitville) District |
|---|
| Ownership category | Private |
|---|
| Type of workings | Surface/Underground |
|---|---|
| Length | 1524M |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | D010645 |
PATTON, H.B., 1917, GEOLOGY AND ORE DEPOSITS OF THE PLATORO-SUMMITVILLE MINING DISTRICT, COLORADO: CGS BULL. 13.
LIPMAN, P.W., 1974, GEOLOGIC MAP OF THE PLATORO CALDERA AREA, SOUTHEASTERN SAN JUAN MOUNTAINS, SOUTHWESTERN COLORADO: USGS MAP I-828.
| Subject category | Comment text |
|---|---|
| Deposit | MINE DEVELOPED ON HIDDEN VEIN AND COPPER HILL-ESMOND VEIN ZONES AND TO LESSER EXTENT ON NORTH TEWKSBURY AND BLACK WONDER VEIN ZONES. HIDDEN VEIN ZONE IS NARROW, OBSCURED, HIGHLY SILICIFIED AND MINERALIZED ZONE TRENDING N 40 TO 60 W AND CONTAINING CONTINUOUS TABULAR MASS OF VUGGY QUARTZ ROCK IN QUARTZ-ALUNITE ZONE FLANKED BY HIGHLY ARGILLIZED ROCK. ON VEIN TREND TO SE ARE SEVERAL PIPELIKE MASSES OF HIGHLY SILICIFIED ROCK LIKEWISE SURROUNDED BY ARGILLIZED ENVELOPES AND PROBABLY MARKING LOCAL UPWARD PROJECTIONS OF MORE CONTINUOUS VEIN ZONE AT DEPTH. ON NARROW GAUGE AND 104 SUBLEVEL (BOTH BELOW COPPER HILL LEVEL), VEIN ZONE CONSISTS OF MANY IRREGULAR. DISCONTINUOUS, AND OVERLAPPING MASSES. ENTIRE ZONE DIPS ABOUT 85 SW. LYING NE OF AND SUBPARALLEL TO HIDDEN VEIN ZONE IS COPPER HILL-ESMOND VEIN ZONE, A LARGE MASS OF HIGHLY SILICIFIED ROCK INQUARTZ-ALUNITE ZONE EXTENDING ACROSS MAIN MINERALIZED AREA FROM COPPER HILL KNOB TO ESMOND VEIN. MASS CONTAINS IRREGULARLY DISTRIBUTED COMPACT QUARTZ |
| Deposit | ZONES WITH VUGGY QUARTZ PIPELIKE ORE BODIES. LARGE SILICIFIED MASS CAPPING COPPER HILL KNOB APPARENTLY GIVES WAY AT DEPTH TO SERIES OF MORE DISTINCT SILICIFIED ZONES SEPARATED BY SEPTA OF LESS ALTERED ROCK. ON SURFACE, VUGGY QUARTZ MASSES RANGE FROM ELONGATE BRANCHING BODIES REFLECTING FORMER JOINT PATTERN TO MORE PIPELIKE MASSES WITH IRREGULAR BUT GENERALLY EQUIDIMENSIONAL HORIZONTAL CROSS-SECTIONS. LARGEST MASSES OF VUGGY QUARTZ ROCK OCCUR NEAR NW END OF VEIN ZONE NEAR ESMOND AND DEL NORTE MINES AND PICKENS CUT. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-JUN-1983 | Schwochow, Stephen D. | Colorado Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.
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