| Deposit ID | 10310395 |
|---|---|
| MRDS ID | W002908 |
| Record type | Site |
| Current site name | Aurora Mine Area |
| Alternate or previous names | Esmeralda, Cambridge, Old Humboldt Mine area, Humboldt West claim, Humboldt East claim, Humboldt vein, Prospectus vein, Martinez, Juniata Mine, Del Monte Mine, Wide West Mine, Johnson Mine, Pond Mine, Chihuahua Mine, Garibaldi Mine, Antelope Mine, Utah Mine, Silver Hill, Middle Hill, Last Chance Hill, Aurora Mine, Aurora Partnership Mine, Chesca Mine |
| Related records | 60001663 |
| Geographic coordinates: | -118.90179, 38.28631 (WGS84) |
|---|---|
| Elevation | 2290 |
| Relative position | The Aurora Mine area is located about 25 miles SW of Hawthorne; 3 miles east of the Nevada-California state line; and 15 miles north of Mono Lake. |
Political divisions (FIPS codes)
Mineral(county)
Nevada(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Aurora(quadrangle 1:24,000 scale)
Excelsior Mountains(quadrangle 1:100,000 scale)
Walker Lake(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
East Walker(hydrologic unit)
Walker(hydrologic accounting unit)
Central Lahontan(hydrologic subregion)
Great Basin(hydrologic region)
Federal lands
Humboldt-Toiyabe National Forest(National Forest)
National Forest FS(Type of land area)
FS(Federal land areas administered by FS)
| Country | State | County |
|---|---|---|
| United States | Nevada | Mineral |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Mount Diablo | 005N | 028E | 10, 17,18,19,20 | Nevada |
| Commodity | Importance |
|---|---|
| Gold | Primary |
| Silver | Primary |
| Materials | Type of material |
|---|---|
| Gold | Ore |
| Tetrahedrite | Ore |
| Electrum | Ore |
| Acanthite | Ore |
| Naumannite | Ore |
| Bromargyrite | Ore |
| Chalcopyrite | Ore |
| Pyrite | Ore |
| Quartz | Gangue |
| Adularia | Gangue |
| Calcite | Gangue |
| Model code | 150 |
|---|---|
| USGS model code | 25c |
| Deposit model name | Epithermal vein, Comstock |
| Mark3 model number | 16 |
| Host or associated | Host | ||||||||
|---|---|---|---|---|---|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Intermediate Volcanic Rock > Andesite | ||||||||
| Rock type qualifier | agglomerates and flows | ||||||||
| |||||||||
| Host or associated | Host | ||||||||
|---|---|---|---|---|---|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Latite | ||||||||
| Rock type qualifier | agglomerates and flows | ||||||||
| |||||||||
| Host or associated | Associated | ||
|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Rhyolite | ||
| |||
| Host or associated | Associated | ||
|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Mafic Volcanic Rock > Basalt | ||
| |||
| Host or associated | Associated | ||
|---|---|---|---|
| Rock type | Plutonic Rock > Granitoid > Granite | ||
| |||
| (1) | Alluvium, undifferentiated |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | A young, less than 3 Ma old, broad regional upwarp extends form the southwest of the Bodie Hills through the Bodie District to the area of the Aurora District. This upwarp may continue to the northeast, south of the Borealis mine. |
| Type of structure | Local |
| Structure description | Steep N-S striking faults offset the mineralized NE-striking faults. |
| General form | lenses and stringers |
|---|
| Operation type | Surface-Underground |
|---|---|
| Development status | Producer |
| Commodity type | Metallic |
| Deposit size | Large |
| Significant | Yes |
| Discovery year | 1860 |
| Discoverer | J.M. Brawley, J.M. Corey, E.R. Hicks |
| Year of first production | 1860 |
| Year of last production | 1998 |
| Production years | 1860-1869; 1914-1918; 1930s, 1983, and 1988-1998 with minor production in intervening years |
| District name | Aurora District |
|---|
| Ownership category | Private |
|---|---|
| Area name | Carson City BLM Administrative District |
| Type | Owner-Operator |
|---|---|
| Owner | Metallic Ventures |
| Year | 2004 |
Ross, D.C., 1961, Geology and Mineral Deposits of Mineral County, Nevada: NBMG Bull 58
Hill, J.M., 1915, Some Mining Districts in Northeastern California and Northwestern Nevada: USGS Bull 594
Ferguson, H.G., 1929, The Mining Districts of Nevada: Econ Geol, v. 24, no. 2, p 115-48.
Green, W.R., 1962, Structural Control of Mineralization at the Aurora Mining District, Mineral County, Nevada: M.S. Thesis, Univ. of Nevada.
Vanderburg, W.O., 1937, Recon. of Mining Districts in Mineral County, Nevada: U.S. Bur. Mines Inf. Circ. 6941, 79p.
Lincoln, F.C. 1923, Mining Districts of Nevada: Reno, Nevada Newsletter Pub. Co. p.137-8.
State Division of Mine Inspection, Dec. 1983, Directory of Nevada Mine Operations Active During Calendar Year 1983.
NBMG Mining District Files, File 189, Press Clippings.
Osborne, M.A., 1991, Epithermal Mineralization at Aurora, Nevada: Proceedings of the GSN 1990 Symposium, p. 1097-1110.
NBMG, 1990, The Nevada Mineral Industry: NBMG Special Publication MI-1989-2004.
Nevada Division of Minerals, Major Mines of Nevada 1989-2004.
Metallic Ventures Gold Inc. press releases, 1/20/2004, 11/12/04.
| Subject category | Comment text |
|---|---|
| Deposit | The Aurora silver-gold deposits are for the most part epithermal fissure vein deposits. Veins consist mostly of finely granular white quartz, which in some places has a milky-white porcelain-like appearance. The veins are commonly composed of layers of quartz of different grain sizes, and all the veins contain cavities lined with clear quartz crystals. The veins are a series of NE-striking to east-striking anastomosing quartz-adularia veins in pre- Esmeralda volcanic rocks that are exposed in a window in an area of predominantly barren younger rocks. A few ounces of placer gold (.408 fine) were recovered from Bodie Creek in 1940-41. Anastomosing quartz-adularia veins vary in width from less than an inch to as much as 60 feet (one reference states up to 130 feet). Average width is 4 feet. Most veins are wider at intersecting faults, with horsetailing of the veins at their extremes. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-DEC-2005 | LaPointe, D.D. | Nevada Bureau of Mines and Geology | |
| Editor | 01-SEP-2007 | Schruben, Paul G. | U.S. Geological Survey | Converted from S&A FileMaker format to Oracle. Edit checks on rocks, units, and ages with Geolex search, and other fields. |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.
These are landing pages for further research — the state agencies don't currently expose per-mine deep links.