| Deposit ID | 10040521 |
|---|---|
| MRDS ID | M055334 |
| Record type | Site |
| Current site name | Andies Mine |
| Alternate or previous names | Mdds 1-15 Claims, NBMG Sample Site 1467, Mayday and Shendell Claims and Wm and Uc Fractions |
| Related records | 10222362 |
| Geographic coordinates: | -115.74698, 37.56024 (WGS84) |
|---|---|
| Elevation | 1914 |
| Relative position | 18 MI SW OF TEM PIUTE |
Political divisions (FIPS codes)
Lincoln(county)
Nevada(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Tempiute Mountain South(quadrangle 1:24,000 scale)
Timpahute Range(quadrangle 1:100,000 scale)
Caliente(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Sand Spring-Tikaboo Valleys(hydrologic unit)
Central Nevada Desert Basins(hydrologic accounting unit)
Central Nevada Desert Basins(hydrologic subregion)
Great Basin(hydrologic region)
Federal lands
Bureau of Land Management(Bureau of Land Management NV)
Bureau of Land Management NV BLM(Type of land area)
BLM(Federal land areas administered by BLM)
| Country | State | County |
|---|---|---|
| United States | Nevada | Lincoln |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Mount Diablo | 004S | 055E | 36,25;25 | Nevada |
| Commodity | Importance |
|---|---|
| Mercury | Primary |
| Barium-Barite Critical | Tertiary |
| Silver | Tertiary |
| Zirconium Critical | Tertiary |
| Materials | Type of material |
|---|---|
| Calcite | Gangue |
| Gypsum | Gangue |
| Jarosite | Gangue |
| Limonite | Gangue |
| Pyrite | Gangue |
| Quartz | Gangue |
| Result | A FEW SAMPLES ASSAYED 15-40 LB/TON HG WITH GOOD VALUES JUST ABOVE THE LIMESTONE, BUT AVERAGE ORE GRADE WAS 2-3 LB HG/TON. SAMPLE 1467 CONTAINS 20 % FE, 7 PPM AG, 1500 PPM BA, 200 PPM ZR. |
|---|
| Model code | 177 |
|---|---|
| USGS model code | 27a |
| Deposit model name | Hot-spring Hg |
| Host or associated | Associated |
|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Rhyolite |
| Host or associated | Host |
|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Rhyolite |
| (1) | -115.74698, 37.56024 |
|---|
| General form | IRREGULAR , IRREGULAR , IRREGULAR |
|---|---|
| Strike | NORTHERLY . NE PREDOMINANTLY. NE PREDOMINANTLY |
| Dip | NEARLY FLAT-LYING |
| Thickness | 13.72M |
| Length | 91.44M |
| Width | 30.48M |
| Depth to top | 12.19M |
| Development status | Producer |
|---|---|
| Commodity type | Both |
| Deposit size | Small |
| Significant | No |
| Discovery year | 1919 |
| Discoverer | C.A. Anderson |
| Year of first production | 1955 |
| Production years | TO 1955 |
| District name | Don Dale District (Sometimes Included In Tempiute District. |
|---|
| Ownership category | BLM Administrative Area |
|---|
| Type | Owner |
|---|---|
| Owner | Don And Carol Williams, St. George, Ut. (Sept. Claim Owners); H.E. Brods Ky. . |
| First year | 1977 |
| Year | 1957 | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Period | To 1957 | ||||||||||||||
| Material | HG | ||||||||||||||
| Accuracy | Accurate | ||||||||||||||
| Description | Cp_Grade: ^2-3 Lb/Ton | ||||||||||||||
| |||||||||||||||
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | M055334 |
BAILEY, E. H., U S GEOLOGICAL SURVEY, PERSONAL FILES
HOLMES, 1965, MERCURY IN NEVADA: IN USBM IC 8252
TSCHANZ AND PAMPEYAN, 1970, GEOLOGY AND MINERAL DEPOSITS OF LINCOLN COUNTY, NEVADA: NBMG. BULL. 73
SMITH, P. AND BENTZ, J., 1983, FIELD EXAMINATION ON OCT 5, 1983.
MELBYE, C.E., 1956, GEOLOGIC EVALUATION OF THE ANDIES MERCURY PROPERTY; NBMG DISTRICT FILE 176.
MERCURY DEPOSITS IN NEVADA; UNPUBLISHED NBMG MANUSCRIPT.
USBM UNPUB DATA
| Subject category | Comment text |
|---|---|
| Deposit | AVERAGES 15 FT THICK; UP TO 40 FT OF OVERBURDEN . CINNABAR OCCURS AS SCATTERED CRYSTALS, THIN VEINCETS, AND COATINGS ON FRACTURE SURFACES IN ALTERED RHYOLITE, AND AS METACINNABAR IN SILICIFIED/OPALIZED RHYOLITE BRECCIA. MINERALIZED STRATA ARE SEPARATED BY LAYERS OF VERY LOW-GRADE OR BARREN MATERIAL.. CINNABAR OCCURS AS SCATTERED CRYSTALS, THIN VEINCETS, AND COATINGS ON FRACTURE SURFACES IN ALTERED RHYOLITE, AND AS METACINNABAR IN SILICIFIED/OPALIZED RHYOLITE BRECCIA. MINERALIZED STRATA ARE SEPARATED BY LAYERS OF VERY LOW-GRADE OR BARREN MATERIAL. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-DEC-1975 | Gassaway, Judith S. | 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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