| Deposit ID | 10310446 |
|---|---|
| Record type | Site |
| Current site name | Rat Deposit |
| Alternate or previous names | Rat Pit |
| Related records | 10310383, 10310443, 10310444 |
| Geographic coordinates: | -115.547, 39.92381 (WGS84) |
|---|---|
| Elevation | 2530 |
| Relative position | The mine area is located approximately 60 miles northwest of Ely, Nevada and 60 miles 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 | 20 29 | Nevada |
| Commodity | Importance |
|---|---|
| Gold | Primary |
| Mercury | Tertiary |
| Materials | Type of material |
|---|---|
| Gold | Ore |
| Pyrite | Gangue |
| Clay | Gangue |
| Limonite | Gangue |
| Quartz | 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 > Siltstone | ||
| Rock type qualifier | sandy | ||
| Rock unit name | Dunderburg Shale | ||
| |||
| Host or associated | Host | ||
|---|---|---|---|
| Rock type | Sedimentary Rock > Carbonate > Limestone | ||
| Rock unit name | Dunderburg Shale | ||
| |||
| Host or associated | Host | ||
|---|---|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock | ||
| Rock type qualifier | fine grained | ||
| Rock unit name | Dunderburg Shale | ||
| |||
| Host or associated | Host | ||
|---|---|---|---|
| Rock type | Sedimentary Rock | ||
| Rock type qualifier | calcareous | ||
| Rock unit name | Hamburg Dolomite | ||
| |||
| Host or associated | Associated | ||||
|---|---|---|---|---|---|
| Rock type | Plutonic Rock > Porphyry | ||||
| Rock type qualifier | quartz-feldspar porphyry stock with satellitic dikes and sills | ||||
| Rock unit name | Bald Mountain Stock | ||||
| |||||
| (1) | Carbonate Shelf Sequence - Dolomite, limestone, and shale |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | The Bald Mountain district is located in an area of thinned crust along the eastern side of the Late Proterozoic rift that split the North American craton. It is also in the west-central portion of the Late Devonian-Early Mississippian Antler foreland basin, and near the eastern edge of deformation related to the late Paleozoic Humboldt orogeny 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. |
| Type of structure | Local |
| Structure description | NW-striking normal faults that dip steeply west and east, with lesser N-striking faults. |
| General form | tabular to irregular |
|---|
| Operation type | Surface |
|---|---|
| Development status | Producer |
| Commodity type | Metallic |
| Deposit size | Small |
| Significant | Yes |
| Year of first production | 1993 |
| Production years | 1993-1996 |
| 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 road log
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 deposit is hosted in the lowermost part of the Dunderberg Shale. Ore was structurally controlled and adjacent to and locally within NW-striking dikes of quartz-feldspar porphyry. Interbedded limestone and siltstone are altered to marble and hornfels adjacent to the dikes. Silicification and decalcification are concentrated in the lower Dunderberg above its contact with the underlying Hamburg, and in faults and fractures in the Dunderberg. The Hamburg is silicified along bedding and fracture networks in the Rat deposit. Pervasive sericitization and weak argillization (mainly supergene) affected the dike, and spotty silicification is along the margins of the dike and in the adjacent Dunderberg. Fine-grained disseminated gold is associated with silica, clay, carbonaceous material, iron oxides, and secondary iron-arsenic minerals. Ore zones are characterized by quartz veining, stockwork formation, and silicified breccia. The ore zone is overlain b a blanket of barren remobilized carbon. |
| 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.