| Deposit ID | 10013570 |
|---|---|
| MRDS ID | D009936 |
| Record type | Site |
| Current site name | Sunshine Lode Mine |
| Alternate or previous names | Grandview Mine |
| Geographic coordinates: | -107.7126, 39.69637 (WGS84) |
|---|---|
| Elevation | 2256 |
| Location accuracy | 500(meters) |
| Relative position | 12 MILES N 18 E FROM RIFLE |
Political divisions (FIPS codes)
Garfield(county)
Colorado(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Rifle Falls(quadrangle 1:24,000 scale)
Glenwood Springs(quadrangle 1:100,000 scale)
Leadville(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Colorado Headwaters-Plateau(hydrologic unit)
Colorado Headwaters(hydrologic accounting unit)
Colorado Headwaters(hydrologic subregion)
Upper Colorado(hydrologic region)
Federal lands
Bureau of Land Management(Bureau of Land Management CO)
Bureau of Land Management CO BLM(Type of land area)
BLM(Federal land areas administered by BLM)
| Country | State | County |
|---|---|---|
| United States | Colorado | Garfield |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| 6th Principal | 004S | 092W | 15,16 | SW OF SW OF SE OF SE | Colorado |
| Commodity | Importance |
|---|---|
| Zinc Critical | Primary |
| Lead | Primary |
| Silver | Primary |
| Gold | Secondary |
| Copper | Secondary |
| Manganese Critical | Tertiary |
| Materials | Type of material |
|---|---|
| Hydrozincite | Ore |
| Plumbojarosite | Ore |
| Calcite | Gangue |
| Dolomite | Gangue |
| Jarosite | Gangue |
| Limonite | Gangue |
| Marcasite | Gangue |
| Selenite | Gangue |
| Host or associated | Host | ||
|---|---|---|---|
| Rock type | Sedimentary Rock > Carbonate > Limestone | ||
| Rock unit name | Leadville Limestone;Belden Formation | ||
| Rock description | Leadville Limestone;Belden Formation | ||
| |||
| (1) | -107.7126, 39.69637 |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | White River Uplift, Grand Hogback Monocline. |
| General form | PINCH AND SWELL |
|---|---|
| Thickness | 1.07M |
| Length | 91.44M |
| General form | PINCH AND SWELL |
|---|
| Development status | Past Producer |
|---|---|
| Commodity type | Metallic |
| Deposit size | Small |
| Significant | No |
| Discovery year | 1925 |
| Year of first production | 1927 |
| Year of last production | 1951 |
| District name | Rifle Creek District |
|---|
| Ownership category | Federal |
|---|
| Year | 1951 | ||||||||||||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Period | 1927-1951 | ||||||||||||||||||||||||||||
| Accuracy | Accurate | ||||||||||||||||||||||||||||
| Description | Cp_Grade: ^9.27% Zn, 2.75% Pb, 3.4 Oz/Ton Ag | ||||||||||||||||||||||||||||
| |||||||||||||||||||||||||||||
| Type of workings | Underground |
|---|---|
| Area | 0.202HA |
| Length | 219.46M |
| Overall depth | 60.96M |
| Overall length | 79.25M |
| Overall width | 27.43M |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | D009936 |
HEYL, A.V., 1964, OXIDIZED ZINC DEPOSITS OF THE UNITED STATES, PART 3--COLORADO: USGS BULL. 1135-C, P. 32-33, 53-54, PL. 5.
TWETO, OGDEN, AND OTHERS, 1978, GEOLOGIC MAP OF THE LEADVILLE 1X2 QUADRANGLE, NORTHWESTERN COLORADO: USGS MAP I-999
MICROFILM MINERAL COMMODITY DOC. 3425-3426 (FROM ORIGINAL CRIB RECORD)
HEYL (1964) AS COMPILED FROM U.S. BUREAU OF MINES MINERAL YEARBOOKS
| Subject category | Comment text |
|---|---|
| Deposit | DEPOSIT LIES IN NARROW GRABEN TRENDING N 10 TO 15 W BOUNDED BY NEARLY PARALLEL STEEPLY NE-DIPPING FAULTS AND CONTAINING SHEARED LEADVILLE LIMESTONE BRECCIA UP TO 60 FT WIDE, SOME IN FAULT CONTACT WITH BELDEN FM SHALES. SULFIDES OCCUR AS DISSEMINATED CRYSTALS AND COLLOFORM CRUSTS CEMENT, REPLACE, AND PARTLY FILL VUGGY LIMESTONE BRECCIA. SULFIDES FAIRLY COMPLETELY OXIDIZED. SMITHSONITE BOXWORKS REPLACE CRUSTS AND DISSEMINATED SPHALERITE CRYSTALS. MUCH OF SMITHSONITE THAT REPLACES ADJACENT CALCITE HAS FURTHER ALTERED TO HYDROZINCITE. CERUSSITE LOCALLY REPLACES GALENA; LIMONITE STAINS AND PSEUDOMORPHS AFTER MARCASITE CAVITIES FROM REPLACE SPHALERITE COATED WITH MN OXIDES, POSSIBLE RESIDUE OF MANGANOAN SPHALERITE. SELENITE CRYSTALS IN VUGS SUGGEST SUPERGENE DEPOSITION BY SULFATE-RICH SOLUTIONS FROM OXIDIZING ORES. ABUNDANCE OF HYDROZINCITE AND LATERAL EXTENT OF SULFIDE OXIDATION SUGGEST DEPOSIT IS NEAR LATE PROGRESSIVE STAGE OF OXIDATION. SIMPLE MINERALOGY, LEANNESS OF AG, COLLOFORM |
| Deposit | CRUSTS, OPEN VUGS, COARSE DISSEMINATED CRYSTALS, AND ABUNDANT CARBONATE GANGUE INDIGATE LOW-TEMPERATURE EPITHERMAL DEPOSITION SIMILAR TO MISSISSIPPI VALLEY-TYPE ZN DEPOSITS. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-JAN-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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