Buckskin National Project

Past Producer in Humboldt county in Nevada, United States with commodities Gold, Silver, Antimony, Iron, Arsenic, Lead, Zinc, Copper
Sections on this page
  1. Identification information
  2. Geographic coordinates
  3. Site location context
  4. Geographic areas
  5. Public Land Survey System information
  6. Commodities
  7. Materials information
  8. Alteration
  9. Mineral occurrence model information
  10. Host and associated rocks
  11. Nearby scientific data
  12. Geologic structures
  13. Ore body information
  14. Controls for ore emplacement
  15. Economic information about the deposit and operations
  16. Mining district
  17. Land status
  18. Ownership information
  19. Bibliographic references
  20. General comments
  21. Reporter information

Geologic information

Identification information

Deposit ID 10310424
MRDS ID M055027
Record type Site
Current site name Buckskin National Project
Related records 10040312, 10281271

Comments on the site identification

  • This record describes the current Buckskin National prospect on the east side of the district, but includes descriptive material from MRDS record # M055027 which describes the historic Buckskin National Mine.

Geographic coordinates

Geographic coordinates: -117.54042, 41.79294 (WGS84)
Elevation 2380
Relative position The deposit is located about 60 miles north of Winnemucca.

Site location context

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)

Geographic areas

Country State County
United States Nevada Humboldt

Public Land Survey System information

Meridian Township Range Section Fraction State
Mount Diablo 045N 039E 11 Nevada

Comments on the location information

  • The deposit is located in the National Mining District on the north-east flank of Buckskin Mountain and is covered by 103 unpatented lode mining claims.

Commodities

Commodity Importance
Gold Primary
Silver Primary
Antimony Critical Secondary
Iron Tertiary
Arsenic Critical Tertiary
Lead Tertiary
Zinc Critical Tertiary
Copper Tertiary

Comments on the commodity information

  • Ore Materials: silver, stibnite, pyrite, arsenopyrite, electrum, pyrargyrite, miargyrite, naumannite, tetrahedrite plus an approximatey equal amount of base metal sulf-ides including galena, chalcopyrite, sphalerite, bornite
  • Gangue Materials: quartz, opal, chalcedony

Materials information

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

Alteration

  • (Local) Alteration consists predominantly of silicification and intense clay alteration. Alteration outward from the pyritic zone enveloping the Bell vein is kaolinite, followed by illite/montmorillonite, then by quartz-chlorite-quartz-calcite, then fresh rock. The kaolinite zone is more extensive in the hanging wall of the veins. There is little unaltered rock under Buckskin Mountain. Magnetite in the calcite-quartz-chlorite zone goes to pyrite in the illite-montmorillonite zone. Vertical alteration zoning is: top of Buckskin mtn.= silica cap, Hg and silicification; 20- m down (vertically) rhyolite is altered to alunite + quartz; -then to depths of several hundred meters selvages of kaolinitic alteration border the veins to depths of several hundred meters; then at depths below the level of the workings (core-drilled by ASARCO), K-mica alteration reportedly occurs in and around the veins.

Mineral occurrence model information

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 and associated rocks

  • Host or associated Host
    Rock type Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Rhyolite
    Stratigraphic age (youngest) Early Miocene
    Chronological age 16
    Dating method K-Ar
    Stratigraphic age (youngest) Middle Miocene
    Chronological age 14
    Dating method K-Ar
  • Host or associated Host
    Rock type Volcanic Rock (Aphanitic) > Intermediate Volcanic Rock > Andesite
    Rock type qualifier basaltic
    Stratigraphic age (youngest) Middle Miocene
    Chronological age 14
    Dating method K-Ar
    Stratigraphic age (youngest) Early Miocene
    Chronological age 16
    Dating method K-Ar
  • Host or associated Host
    Rock type Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Quartz Latite
    Stratigraphic age (youngest) Early Miocene
    Chronological age 16
    Dating method K-Ar
    Stratigraphic age (youngest) Middle Miocene
    Chronological age 14
    Dating method K-Ar
  • Host or associated Host
    Rock type Volcanic Rock (Aphanitic) > Pyroclastic Rock
    Stratigraphic age (youngest) Early Miocene
    Chronological age 16
    Dating method K-Ar
    Stratigraphic age (youngest) Middle Miocene
    Chronological age 14
    Dating method K-Ar
  • Host or associated Host
    Rock type Sedimentary Rock > Mixed Clastic/Volcanic Rock
    Rock type qualifier volcaniclastic sediments with pool sinter
    Stratigraphic age (youngest) Middle Miocene
    Chronological age 14
    Dating method K-Ar
    Stratigraphic age (youngest) Early Miocene
    Chronological age 16
    Dating method K-Ar
  • Host or associated Associated
    Rock type Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Rhyolite
    Stratigraphic age (youngest) Middle Miocene
    Chronological age 14
    Dating method K-Ar
    Stratigraphic age (youngest) Early Miocene
    Chronological age 16
    Dating method K-Ar
  • Host or associated Associated
    Rock type Volcanic Rock (Aphanitic) > Intermediate Volcanic Rock > Andesite
    Rock type qualifier basaltic
    Stratigraphic age (youngest) Early Miocene
    Chronological age 16
    Dating method K-Ar
    Stratigraphic age (youngest) Middle Miocene
    Chronological age 14
    Dating method K-Ar

Nearby scientific data

(1) -117.54042, 41.79294

Economic information

Geologic structures

Type of structure Local
Structure description Two approximately orthogonal fault sets running approximately N-S and E-W have influenced hydrothermal mineralization.

Ore body information

  • General form tabular

Controls for ore emplacement

  • "fissure vein", N-trending faults and E-W- trending faults

Comments on the geologic information

  • The fissure vein averages 4 ft wide, and was opened up for 3000 ft. along strike on the 10-ft level. The rhyolitic rocks are peraluminous.

Economic information about the deposit and operations

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

Mining district

District name National District

Land status

Ownership category Private
Ownership category BLM Administrative Area
Area name Winnemuca BLM District

Ownership information

  • Type Owner-Operator
    Owner Romarco Minerals Inc.
    Year 2004

Comments on the workings information

  • The historic deposit was developed by a shaft, 3 adits, and other underground workings totalling over 6500 feet. A mill burned in 1937. Recent surface exploration work includes core drill holes

Comments on other economic factors

  • 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. Bulk mineable reserve reported in1990 was 138,251 tons of ore grading 0.363 oounces per ton Au and 3.37 ounces per ton Ag. In 1997 reserves of 50,221 Au and 466,243 ounces of Ag were reported.

Comments on development

  • Silver and gold claims were staked on Buckskin Peak prior to 1907. The Buckskin National Mine was worked intermittently from 1912 through 1940 and was initially covered by 2 patented and 9 unpatented claims. The Buckskin National Gold Mining Co. was incorporated in 1912. It was equipped with a 100-ton flotation mill, but the ore was found to be unsuitable for the flotation process. From about 1928 to 1938 the property was run by the Nevada Lucky Tiger Mining Co. under a lease. In June, 1937, 50 men were employed mining 50 tons of ore per day. The historic Buckskin National Mine last operated in the 1930s . MC CORMICK ET. AL. 1942.
    ASARCO was leasing property in 1983 from owners, the time Buckskin National Gold Mining Co. but there was no activity at that time. ASARCO drilled 1000 m or more of core holes in the property.

    In April 2004 Romarco Minerals Inc. announced the beginning of an exploration program on its newly acquired Buckskin-National Project. Romarco acquired a 100% operating interest in the 103 unpatented lode mining claims that comprise the project area, subject to terms and obligations of lease agreements between Romarco and three private parties. The planned 2004 exploration program will involve a comprehensive approach including mapping the surface and underground geology, logging all available existing drill cores, conducting a widespread systematic soil sampling program, and initiating diamond drilling of bonanza vein targets. Additionally, existing drill core that was never split, sampled, and assayed will be split and assayed for gold, silver, and associated elements. The logging and sampling of existing drill core is currently underway, and field activities will begin in late May or June.

Comments on the environmental information

  • Magmatism associated with continental extension under reducing conditions

Reference information

Bibliographic references

General comments

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.

Reporter information

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.

Beyond USGS

Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.

External references

Authoritative Nevada resources

These are landing pages for further research — the state agencies don't currently expose per-mine deep links.