| Deposit ID | 10037376 |
|---|---|
| MRDS ID | M032076 |
| Record type | Site |
| Current site name | Homestake Mine |
| Related records | 10270923 |
| Geographic coordinates: | -114.07194, 37.92468 (WGS84) |
|---|---|
| Elevation | 2158 |
| Relative position | 1/2 MILE S OF DEER LODGE |
Political divisions (FIPS codes)
Lincoln(county)
Nevada(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Deer Lodge Canyon(quadrangle 1:24,000 scale)
Caliente(quadrangle 1:100,000 scale)
Caliente(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Meadow Valley Wash(hydrologic unit)
Lower Colorado-Lake Mead(hydrologic accounting unit)
Lower Colorado-Lake Mead(hydrologic subregion)
Lower Colorado(hydrologic region)
| Country | State | County |
|---|---|---|
| United States | Nevada | Lincoln |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| 01N | 71E | 19 | Nevada |
| Commodity | Importance |
|---|---|
| Gold | Primary |
| Silver | Primary |
| Materials | Type of material |
|---|---|
| Copper | Ore |
| Alunite | Gangue |
| Fluorite | Gangue |
| Pyrite | Gangue |
| Quartz | Gangue |
| Result | SAMPLES 1727 AND 1728 CONTAIN, RESPECTIVELY: 200 PPM MN, 50 AND 5 PPM AG, 20 AND 0 PPM AU, 200 AND 500 PPM BA, 0 AND 100 PPM MO, 20 AND 50 PPM PB, 0 AND 200 PPM SR, 10 AND 100 PPM V, 0 AND 100 PPM ZR. |
|---|
| Model code | 150 |
|---|---|
| USGS model code | 25c |
| Deposit model name | Epithermal vein, Comstock |
| Mark3 model number | 16 |
| Host or associated | Associated |
|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Latite |
| Host or associated | Host |
|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Rhyolite |
| Host or associated | Host |
|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Latite |
| Host or associated | Host |
|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Intermediate Volcanic Rock > Andesite |
| (1) | -114.07194, 37.92468 |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | N-S And E-W Vein Systems |
| Type of structure | Local |
| Structure description | Fault Is Probably Pre-Mineral, For Although Slicks Are Present On Footwall, Vein Is Relatively Unbrecciated. |
| General form | IRREGULAR |
|---|---|
| Strike | N-S TO N15E |
| Dip | 40-50W |
| Development status | Past Producer |
|---|---|
| Commodity type | Metallic |
| Deposit size | Small |
| Significant | No |
| District name | Eagle Valley (Fay, Gold Springs) District (Fay, Gold Springs) District |
|---|
| Ownership category | Private |
|---|
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | M032076 |
TSCHANTZ CM & PAMPEYAN EH, 1970, GEOLOGY AND MINERAL DEPOSITS OF LINCOLN CO, NEV BUR MINES BULL 73
USGS, 1920, PP 111, P. 563-568.
BENTZ, J. AND SMITH, P., 1983, FIELD EXAMINATION REPORT, SEPT 19, 1983.
| Subject category | Comment text |
|---|---|
| Deposit | OPEN-CENTERED FISSURE VEINS AND VEINLETS WHICH CARRY PYRITE. THE HANGING WALL AND FOOTWALL ANDESITES ARE IRON-STAINED, BLEACHED, SILICIFIED, AND HEAVILY QUARTZ-VEINED. THE ROCKS ARE NOTABLY BRECCIATED (SLICCKS ARE ABUNDANT) AND SHOW A NETWORK OF CRUSTIFORM QUARTZ VEINS AND VEINLETS WHICH EXTEND OUTWARD INTO THE WALLROCK ADJACENT TO THE MAIN VEIN. QUARTZ VEINING OF WALLROCKS INCREASES WIDTH OF VEIN EXPOSURE TO 10 FT OR MORE. MAIN VEIN IS SHEARED BY SEVERAL SMALL E-W STRUCTURES AND MAY BE TRUNCATED BY ONE SUCH STRUCTURE AT THE SOUTHERN END OF THE EXPOSURE. |
| Deposit | CRUSTIFIED EPITHERMAL QUARTZ VEIN WITH ADULARIA (ALUNITE ?) APPEARS TO HAVE BEEN EMPLACED ALONG A SHEAR ZONE. UPPER PORTION OF EXPLORED VEIN CONSISTS OF MASSIVE TO COCKADE QUARTZ WHICH ENCASES SILICIFIED ANDESITE AND POSSIBLY SOME RHYOLITE FRAGMENTS WHICH WERE PROBABLY RIPPED UP AND INCORPORATED IN VEIN DURING EMPLACEMENT. MAIN VEIN IS A MASSIVE TO BANDED, SUGARY TO CHALCEDONIC GREENISH WHITE QUARTZ-ADULARIA (?) VEIN OVER 5 FT WIDE. MOST QUARTZ IS VERY FINE-GRAINED AND TYPICALLY FORMS UNDULATORY CHALCEDONIC BANDS PARALLEL TO THE VEIN. SOME OF THE BANDS ARE DARK WITH FINELY DISPERSED SULFIDES WHICH ARE PROBABLY AG-BEARING MINERALS, AND IN SEVERAL SAMPLES, VERY FINE-GRAINED FREE GOLD WAS NOTED IN THE SULFIDE-RICH LENSES. GOLD ALSO OCCURS WITH PYRITE, MINOR CHALCOPYRITE AND BLUE METALLIC SULFIDES IN FINE-GRAINED CLOTS DISPERSED RANDOMLY THROUGHOUT SUGARY QUARTZ VEIN IN DUMP SAMPLES AND IN OUTCROP. THE GOLD-BEARING FINE-GRAINED QUARTZ VEIN IS CROSSCUT BY LATE-STAGE CLEAR VITREOUS |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-FEB-1980 | Harner, Joy L. (Roberts, Ralph J.) | U.S. Geological Survey | |
| Updater | 01-AUG-1984 | La Pointe, D.D. (Tingley, J.V.) | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.
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