| Deposit ID | 10310444 |
|---|---|
| Record type | Site |
| Current site name | RBM Deposit |
| Alternate or previous names | Bald Mountain Mine project |
| Related records | 10310383, 10310443, 10310446 |
| Geographic coordinates: | -115.547, 39.92381 (WGS84) |
|---|---|
| Elevation | 2530 |
| Relative position | The RBM deposit on the western edge of Bald Mountain, about 60 miles northwest of Ely and 60 miles south-southeast of Elko, Nevada. |
Political divisions (FIPS codes)
White Pine(county)
Nevada(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Big Bald Mountain(quadrangle 1:24,000 scale)
Newark Lake(quadrangle 1:100,000 scale)
Ely(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Little Smoky-Newark 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 | White Pine |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Mount Diablo | 024N | 057E | 15 | Nevada | |
| Mount Diablo | (UNSURVEYED) | Nevada |
| Commodity | Importance |
|---|---|
| Gold | Primary |
| Silver | Secondary |
| Mercury | Tertiary |
| Arsenic Critical | Tertiary |
| Lead | Tertiary |
| Zinc Critical | Tertiary |
| Copper | Tertiary |
| Tellurium Critical | Tertiary |
| Bismuth Critical | Tertiary |
| Antimony Critical | Tertiary |
| Materials | Type of material |
|---|---|
| Gold | Ore |
| Clay | Ore |
| Limonite | Ore |
| Quartz | Ore |
| Marcasite | Ore |
| Arsenopyrite | Ore |
| Galena | Ore |
| Sphalerite | Ore |
| Chalcopyrite | Ore |
| Pyrite | Gangue |
| Model code | 75 |
|---|---|
| USGS model code | 19c |
| Deposit model name | Distal disseminated Ag-Au |
| Mark3 model number | 18 |
| Host or associated | Host | ||||
|---|---|---|---|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock | ||||
| Rock type qualifier | fine grained | ||||
| |||||
| Host or associated | Host | ||||
|---|---|---|---|---|---|
| Rock type | Sedimentary Rock | ||||
| Rock type qualifier | calcareous | ||||
| |||||
| Host or associated | Host | ||||
|---|---|---|---|---|---|
| Rock type | |||||
| Rock unit name | Antelope Valley Limestone | ||||
| |||||
| Host or associated | Host | ||
|---|---|---|---|
| Rock type | Plutonic Rock > Porphyry | ||
| Rock type qualifier | quartz-feldspar porphyry stock with satellitic dikes and sills | ||
| |||
| Host or associated | Associated | ||||
|---|---|---|---|---|---|
| Rock type | |||||
| Rock unit name | Bald Mountain Stock | ||||
| |||||
| (1) | Carbonate Shelf Sequence - Dolomite, limestone, and shale |
|---|
| Type of structure | Local |
|---|---|
| Structure description | NW-striking normal faults that dip steeply west and east, with lesser N-striking faults. |
| Type of structure | Regional |
| Structure description | To the west of the Bald Mountain district, geologic interpretations are dominated by recognition of Paleozoic deformation, whereas to the east, interpretations emphasize Mesozoic contraction and plutonism and Tertiary extension. |
| Operation type | Surface-Underground |
|---|---|
| Development status | Producer |
| Commodity type | Metallic |
| Deposit size | Small |
| Significant | Yes |
| Year of first production | 1988 |
| District name | Bald Mountain District |
|---|
| Ownership category | BLM Administrative Area |
|---|---|
| Area name | Ely BLM district |
| Type | Owner-Operator |
|---|---|
| Owner | Barrick Gold Corp. |
| Year | 2006 |
NBMG Mining District Files 323, Press Clippings
NBMG, 1988, NBMG MI-1987.
GSN 1985 Meeting and Fall Field Trip Roadlog
Adamson, T.J., 1987, in Bulk Mineable Precious Metal Deposits of the Western U.S., 1987 GSN, Field Trip Guidebook and Technical Volume.
NBMG, 1994, MI-1993
Nutt, C.J., Hofstra, A.H., Hart, K.S., and Mortensen, J.K., 2000, Structural setting and genesis of gold deposits in the Bald Mountain-Alligator Ridge area, east-central Nevada, in Cluer, J.K., Price, J.G., Struhsacker, E.M., Hardyman, R.F., and Morris, C.L., eds., Geology and Ore Deposits 2000: The Great Basin and Beyond: Geological Society of Nevada Symposium Proceedings, May 15-18, 2000, p. 513-537.
Hitchborn and others, 1996, Geology and Gold Deposits of the Bald Mountain Mining District, White Pine County, Nevada, in Geology and Ore Deposits of the American Cordillera Symposium Proceedings, eds. A. Coyner and P. Fahey.
The Geological Society of Nevada 1996 Spring Field trip, Geology and Gold Deposits of Eastern Nevada, GSN Special Publication No. 23.
BLM, 2004, Bald Mountain Mine Exploration Program Programmatic Environmental Assessment NV040-04-023, Case File # N78825.
| Subject category | Comment text |
|---|---|
| Deposit | The RBM deposit is located along a NW-trending structural zone and consists of two main minerlized zones: the RBM main vein , which strikes N45W, and the RBM west vein, which strikes N75W. Dips are vertical to 60E. The West vein is oxidized near surface with a massive sulfide ore zone at depth consisting of pyrite, marcasite, arsenopyrite, galena, sphalerite, chalcopyrite, and possible tellurium-bearing sulfides. Sedimentary rocks at the deposit are fine-grained limestone, impure sandstone, quartzite, and siltstone of the Antelope Valley Formation and Eureka Quartzite. The sediments were intruded by quartz feldspar porphyry which has been altered. The quartz feldspar porphyry is present in the western portion of the deposit and hosts most of the gold mineralization. Faulted contacts betwen the sedimentary rocks and the dikes acte as conduits for mineralizing fluids. The RBM deposit was originally in the upper part of the Bald Mountain system above the Top deposit, and was subsequently downdropped along the Ruby listric fault to its present position. More than 1 km of gold-bearing rock between the RBM deposit and present day exposures of the originally underlying Top deposit was removed by erosion. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-NOV-2004 | 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.