| Deposit ID | 10014031 |
|---|---|
| MRDS ID | D010644 |
| Record type | Site |
| Current site name | Chandler Tunnel |
| Alternate or previous names | Claim: Little Ida, Ms 67 |
| Related records | 10216275 |
| Geographic coordinates: | -106.60116, 37.42891 (WGS84) |
|---|---|
| Elevation | 3505 |
| Relative position | 0.4 MILES S 81 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 | NW OF NW | Colorado |
| Commodity | Importance |
|---|---|
| Gold | Primary |
| Silver | Primary |
| Copper | Secondary |
| Materials | Type of material |
|---|---|
| Chalcopyrite | Ore |
| Covellite | Ore |
| Tennantite | Ore |
| Result | 11-TON CRUDE ORE SHIPMENT IN 1929 CONTAINED 1.8 OZ/TON AU, 18 OZ/TON AG, 16.9% CU |
|---|
| 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) | -106.60116, 37.42891 |
|---|
| 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 |
| Discovery year | 1876 |
| Discoverer | San Juan Consolidated Mining Co. (Claimant) |
| Year of first production | 1875 |
| Year of last production | 1957 |
| District name | Summit (Summitville) District |
|---|
| Ownership category | Private |
|---|
| Type | Operator |
|---|---|
| Owner | General Minerals Corp. |
| Home office | Grand Junction |
| First year | 1957 |
| Type of workings | Underground |
|---|---|
| Length | 877.82M |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | D010644 | |
| U.S. Bureau of Mines | Minerals Availability System | MAS | 0081050009 |
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.
BLM MINERAL SURVEY MS 67
COLORADO DIV. MINES INF. REPT. AND ANNUAL OPERATOR REPTS.
| Subject category | Comment text |
|---|---|
| Deposit | MINE DEVELOPED PRINCIPALLY ON LITTLE ANNIE VEIN ZONE, MOST EXTENSIVELY DEVELOPED VEIN AND LARGEST AU PRODUCER IN DISTRICT. DEPOSIT IS NW-SE-TRENDING, NEARLY VERTICAL, IRREGULARLY TABULAR MASS OF LIMONITE-STAINED, HIGHLY SILICIFIED ROCK, ALMOST ENTIRELY VUGGY QUARTZ WITH LOCAL SELVAGES OR INCLUSIONS OF QUARTZ-ALUNITE ROCK. ZONE APPARENTLY ENDS ON SE NEAR WINCHESTER PORTAL. NE-TRENDING CROSS-FRACTURES REFLECTED BY PROJECTIONS OF SILICIFIED ROCK AND ELONGATED PIPES, SUCH AS ANNIE BELLE VEIN EXTENDING SW FROM ANNIE OPEN CUT. HIGHLY OXIDIZED ORE (AURIFEROUS LIMONITE) STOPED ABOVE IDA LEVEL, SOME MINED BETWEEN IDA AND CHANDLER LEVELS. UNOXIDIZED AU-CU SULFIDE ORE ON CHANDLER LEVEL AND AS DEEP AS REYNOLDS LEVEL BUT CONTINUITY UNKNOWN. CHANDLER LEVEL ALSO DEVELOPS DEXTER (ODIN) VEIN TO MINOR EXTENT. |
| 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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