| Deposit ID | 10310541 |
|---|---|
| Record type | Site |
| Current site name | Afgan Deposit |
| Alternate or previous names | Afghan deposit |
| Geographic coordinates: | -116.32413, 39.72605 (WGS84) |
|---|---|
| Relative position | The deposit is located approximately 40 km northwest of Eureka, NV. |
Political divisions (FIPS codes)
Eureka(county)
Nevada(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Bartine Ranch NE(quadrangle 1:24,000 scale)
Simpson Park Mountains(quadrangle 1:100,000 scale)
Millett(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Diamond-Monitor 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 | Eureka |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Mount Diablo | 021N | 050E | 01, 02, 03, 04 | Nevada | |
| Mount Diablo | 022N | 050E | 25, 26, 33, 34, 35, 36 | Nevada |
| Commodity | Importance |
|---|---|
| Gold | Primary |
| Materials | Type of material |
|---|---|
| Gold | Ore |
| Model code | 173 |
|---|---|
| USGS model code | 26a.1 |
| Deposit model name | Sediment-hosted Au |
| Mark3 model number | 17 |
| Host or associated | Host | ||
|---|---|---|---|
| Rock type | |||
| Rock unit name | Webb Formation | ||
| |||
| (1) | -116.32413, 39.72605 |
|---|
| Type of structure | Local |
|---|---|
| Structure description | Paleozoic thrusting and folding and Tertiary age high angle faulting have affected rocks in the mine area. Limestone beds are gently folded along ENE-trending fold axes, forming anticlines and synclines that plunge 10-40 degrees to the east. The dominant Tertiary fault sets strike northwest and north-south; other sets strike east-northeast and northeast. |
| Type of structure | Regional |
| Structure description | The deposit is located in a window of lower plate rocks below the Roberts Mountain Thrust and lying along the NW-trending Battle Mountain-Eureka Trend of mineral deposits. |
| General form | disseminated |
|---|
| Operation type | Surface |
|---|---|
| Development status | Prospect |
| Commodity type | Metallic |
| Deposit size | Small |
| Significant | Yes |
| Discoverer | . |
| District name | Antelope District |
|---|
| Ownership category | BLM Administrative Area |
|---|---|
| Area name | Battle Mountain BLM District |
| Type | Owner-Operator |
|---|---|
| Owner | White Knight Resources, Ltd. |
| Year | 2001 |
Geology and Mineralization of the Gold Bar District, Southern Roberts Mountains, Eureka County, Nevada, 1998, French, G.M., Fenne, F.K., Maus, D.A., Rennebaum, T.D., and Jennings, T.A., in Sediment-hosted Gold Deposits of the Eureka (Ruby Hill Mine) and Gold Bar Districts, East-Central Nevada, Geological Society of Nevada Special Publication No., 27, 1998 Spring Field Trip Guidebook.
Long, K.R., DeYoung, J.H., Jr., and Ludington, S.D., 1998, Significant deposits of gold, silver, copper, lead, and zinc in the United States: U.S. Geological Survey Open-File Report 90-206A, 33 p.; 98-206B. one 3.5 inch diskette.
NBMG MI-96 thru MI-99
Simpson Park Mtns. Land Status, 1979
Amer. Mines (2000), 1999
Amer. Mines (2001) 2000
Maher, 1997
Castleworth (Pan Nevada) website, Feb. 2006.
BLM Claim Microfiche, 1997
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-MAY-2003 | 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.