| Deposit ID | 10310424 |
|---|---|
| MRDS ID | M055027 |
| Record type | Site |
| Current site name | Buckskin National Project |
| Related records | 10040312, 10281271 |
| Geographic coordinates: | -117.54042, 41.79294 (WGS84) |
|---|---|
| Elevation | 2380 |
| Relative position | The deposit is located about 60 miles north of Winnemucca. |
Political divisions (FIPS codes)
Humboldt(county)
Nevada(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Buckskin Mountain(quadrangle 1:24,000 scale)
Quinn River Valley(quadrangle 1:100,000 scale)
McDermitt(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Little Humboldt(hydrologic unit)
Humboldt(hydrologic accounting unit)
Black Rock Desert-Humboldt(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 | Humboldt |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Mount Diablo | 045N | 039E | 11 | Nevada |
| Commodity | Importance |
|---|---|
| Gold | Primary |
| Silver | Primary |
| Antimony Critical | Secondary |
| Iron | Tertiary |
| Arsenic Critical | Tertiary |
| Lead | Tertiary |
| Zinc Critical | Tertiary |
| Copper | Tertiary |
| Materials | Type of material |
|---|---|
| Silver | Ore |
| Stibnite | Ore |
| Pyrite | Ore |
| Arsenopyrite | Ore |
| Electrum | Ore |
| Pyrargyrite | Ore |
| Miargyrite | Ore |
| Naumannite | Ore |
| Tetrahedrite | Ore |
| Galena | Ore |
| Chalcopyrite | Ore |
| Sphalerite | Ore |
| Bornite | Ore |
| Quartz | Gangue |
| Opal | Gangue |
| Chalcedony | Gangue |
| Model code | 150 |
|---|---|
| USGS model code | 25c |
| Deposit model name | Epithermal vein, Comstock |
| Mark3 model number | 16 |
| Model code | 104 |
| USGS model code | 25a |
| Deposit model name | Hot-spring Au-Ag |
| Mark3 model number | 45 |
| Host or associated | Host | ||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Rhyolite | ||||||||||||
| |||||||||||||
| Host or associated | Host | ||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Intermediate Volcanic Rock > Andesite | ||||||||||||
| Rock type qualifier | basaltic | ||||||||||||
| |||||||||||||
| Host or associated | Host | ||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Quartz Latite | ||||||||||||
| |||||||||||||
| Host or associated | Host | ||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Pyroclastic Rock | ||||||||||||
| |||||||||||||
| Host or associated | Host | ||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Rock type | Sedimentary Rock > Mixed Clastic/Volcanic Rock | ||||||||||||
| Rock type qualifier | volcaniclastic sediments with pool sinter | ||||||||||||
| |||||||||||||
| Host or associated | Associated | ||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Rhyolite | ||||||||||||
| |||||||||||||
| Host or associated | Associated | ||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Intermediate Volcanic Rock > Andesite | ||||||||||||
| Rock type qualifier | basaltic | ||||||||||||
| |||||||||||||
| (1) | -117.54042, 41.79294 |
|---|
| Type of structure | Local |
|---|---|
| Structure description | Two approximately orthogonal fault sets running approximately N-S and E-W have influenced hydrothermal mineralization. |
| General form | tabular |
|---|
| Operation type | Underground |
|---|---|
| Development status | Past Producer |
| Commodity type | Metallic |
| Deposit size | Small |
| Significant | Yes |
| Discovery year | 1907 |
| Discoverer | John Dermody |
| Year of first production | 1912 |
| Year of last production | 1941 |
| Production years | 1930, 1932-1933, 1938-1941 |
| District name | National District |
|---|
| Ownership category | Private |
|---|---|
| Ownership category | BLM Administrative Area |
| Area name | Winnemuca BLM District |
| Type | Owner-Operator |
|---|---|
| Owner | Romarco Minerals Inc. |
| Year | 2004 |
Willden, R., 1964, Geology and Mineral Deposits of Humboldt Co., Nev; NBMG Bull. 59.
Vanderburg, W.O., 1938, Reconnaissance of Mining Districts in Humboldt County, Nevada; U.S. B. M. Inf. Circ. 6995
Lindgren, W., 1915, Geology and Mineral Deposits of the National Mining District, Nevada: U.S.G.S. Bull 601.
Lawrence, E.F., 1963, Antimony Deposits of Nevada; NBMG Bull. 61.
Garside, L. J. And Bonham, M. F., Jr., 18 Aug 83, Field examination and tour led by Peter Vikre of ASARCO Minerals, and sample analyses.
NBMG Staff, 1985, NBMG OFR 85-3.
NBMG Map 88, 1986, Geology of Buckskin Mountain, by P. G. Vikre.
Nevada Dept. of Minerals, 1993
Miller and Rumpsey, USBM production figures
NBMG MI-86; MI-97
NBMG Map 91, 1st, 2nd, 3rd
Amer. Mines (1990), 1990
National Au Min. Industry News, 1 Aug 1986
Carper, 1920,MD133, I12
Amer. Mines (2000), 1999
Romarco Minerals Inc. press releases, April, May, 2004.
| Subject category | Comment text |
|---|---|
| Deposit | Buckskin-National is a volcanic-hosted gold-silver exploration project that exhibits exceptional discovery potential for high grade, bonanza gold and silver vein systems that are analogous to ore deposits at the nearby Ken Snyder Mine. Bonanza gold/silver ores mined during the early 1900's from underground workings along the Bell Vein in the eastern portion of the project area yielded a recorded production of approximately 24,000 ounces of gold and 300,000 ounces of silver from ore averaging approximately of 0.7 ounces gold and 8.8 ounces silver per ton. Mineralization consists of a complete hot springs gold system from surface sinter deposits to antimony-rich upper portions of veins to deeper ruby silver and gold-bearing quartz veins. The mines explore two N15W, 75SW-trending veins which are parallel to and on strike with the National and Birthday veins 7 km to the NW. The eastern vein is the Lawry and the western vein is the Bell vein, the latter of which is on the current Buckskin National property. The tops of the vein system can be seen at the surface in pits and stopes. The veins are on a 3m wide silicified zone with veins and stockworks of fine-grained chalcedonic quartz with fine laminated crustification. Stibnite occurs in the upper parts of these veins; it is absent or late-stage in deeper veins. There are 4 stages of vein mineralization: stage IV (latest, highest in system) stibnite and Ag sulfosalts and fine crustiform chalcedony; stage III strong pyrite and marcasite; stage II rhythmically crustified quartz-chalcedony veins with Ag sulfosalts and native gold (electrum); stage I (deepest) silver minerals associated with white K-mica and feldspar- stable alteration. The tops of these veins "apex" about 200 m below the paleosurface (pool sinters, etc.). Fluid inclusions from these veins indicate temperatures of approx 175 degrees C with some indications of overpressure. Hydrothermal breccias have been noted. The Bell Vein underground consists of a strong iron sulfide zone several meters wide with a 2060 cm crustified quartz vein in center. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-JUN-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.
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