Pershing Mine

Producer in Pershing county in Nevada, United States with commodities Mercury, Antimony
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. Workings at the site
  20. Links to other databases
  21. Bibliographic references
  22. General comments
  23. Reporter information

Geologic information

Identification information

Deposit ID 10040309
MRDS ID M055022
Record type Site
Current site name Pershing Mine
Alternate or previous names Lovelock Quicksilver, Adamson Property
Related records 10198096

Geographic coordinates

Geographic coordinates: -118.16875, 40.13684 (WGS84)
Elevation 1359
Relative position 16 MI. E OF LOVELOCK

Site location context

Political divisions (FIPS codes)

Pershing(county)

Nevada(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

Buffalo Mountain(quadrangle 1:24,000 scale)

Lovelock(quadrangle 1:100,000 scale)

Lovelock(quadrangle 1:250,000 scale)

Hydrologic units (watersheds)

Carson Desert(hydrologic unit)

Carson(hydrologic accounting unit)

Central Lahontan(hydrologic subregion)

Great Basin(hydrologic region)

Geographic areas

Country State County
United States Nevada Pershing

Public Land Survey System information

Meridian Township Range Section Fraction State
Mount Diablo 26N 34E 08,09,16,17 Nevada

Comments on the location information

  • SEC. 8, SW 1/4 SEC. 9; N 1/2 SEC. 16; UTM TAKEN AT MAIN ADIT SEC. 8.

Commodities

Commodity Importance
Mercury Primary
Antimony Critical Tertiary

Materials information

Materials Type of material
Cinnabar Ore
Mercury Ore
Metacinnabar Ore
Ankerite Gangue
Barite Gangue
Calcite Gangue
Dolomite Gangue
Galena Gangue
Pyrite Gangue
Quartz Gangue
Sphalerite Gangue
Stibnite Gangue

Alteration

  • (Local) Silicification

Analytical data

Result 4 LB/TON HG
Result YIELD 57 LB HG/FT.

Mineral occurrence model information

Model code 177
USGS model code 27a
Deposit model name Hot-spring Hg

Host and associated rocks

  • Host or associated Associated
    Rock type Volcanic Rock (Aphanitic) > Mafic Volcanic Rock > Basalt
    Rock unit name Diabase Dikes
    Rock description Diabase Dikes
    Stratigraphic age (youngest) Late Triassic
    Stratigraphic age (youngest) Pleistocene
    Stratigraphic age (youngest) Late Jurassic
  • Host or associated Host
    Rock type Sedimentary Rock > Carbonate > Dolomite
    Rock unit name Lower Unit Of Post-Dun Glen Strata-Dolomite
    Rock description Lower Unit Of Post-Dun Glen Strata-Dolomite

Nearby scientific data

(1) -118.16875, 40.13684

Economic information

Geologic structures

Type of structure Regional
Structure description Relief Fault (Thrust) ; Reg.Trends: N 40 W
Type of structure Local
Structure description Nw Normal Fault; Overturned Anticlinorium

Ore body information

  • General form TABULAR
    Strike NW
    Dip MODERATE NE
    Thickness 4.57M
    Length 304.8M
    Width 15.24M

Controls for ore emplacement

  • Fractures In Dolomite, Faults Under Shale

Comments on the geologic information

  • CARBONATES CUT BY DIABASE DIKES. STRATIGRAPHIC UNIT CONSISTS OF SHALE OVERLAIN BY BLACK SANDSTONE, OVERLAIN BY THIN LAYER OF BUFF SANDSTONE, OVERLAIN BY CONGLOMERATIC DOLOMITE. THE BUFF SANDSTONE LAYER IS FOLLOWED AS A "KEY BED" IN THE UNDERGROUND MINING. MOST OF THE ORE BODIES OCCUR WHERE CINNABAR FILLS NUMEROUS IRREGULAR FRACTURES OR AS DISSEMINATED CRYSTALS IN THE UNBROKEN ROCK. DEPOSITS ARE FOLDED AND FAULTED INTO NW TRENDING RIDGES. SOUTH PART OF AREA-FANGLOMERATE; NORTH PART-BASALTS. ; GEOL.DESC: CARBONATES CUT BY DIABASE DIKES ; MAJOR.UNITS: UPPER TRIASSIC - LOWER JURASSIC SEDIMENTARY ROCKS

Economic information about the deposit and operations

Development status Producer
Commodity type Metallic
Deposit size Small
Significant No
Discovery year 1912
Discoverer Chris Mattevich
Year of first production 1916
Production years 1916-1917, 1928-1930, 1942-1944, 1946

Mining district

District name Antelope Springs

Land status

Ownership category BLM Administrative Area

Ownership information

  • Type Owner
    Owner United Mercury Corp.
    First year 1965

Comments on the reserve resource information

  • ESTIMATED RESERVES FOR 3000 FL (1942)

Workings at the site

  • Type of workings Underground
    Area 5.914HA
    Length 2133.6M
    Overall depth 76.2M
    Overall length 304.8M
    Overall width 4.57M

Comments on the workings information

  • WORKINGS AS OF 1949. LAST OPERATED 1958.

Comments on development

  • PRODUCTION YEARS 1916-17, 1928-30, 1942-44, 1946

Reference information

Bibliographic references

  • Deposit

    JOHNSON, M.G., 1977, GEOLOGY AND MINERAL DEPOSITS OF PERSHING COUNTY, NEVADA: NBMG BULL. 89

  • Deposit

    BAILEY AND PHOENIX, 1944, QUICKSILVER DEPOSITS IN NEVADA: NBMG BULL. 41, P. 164

  • Deposit

    LAWRENCE, F.C., 1963, ANTIMONY DEPOSITS OF NEVADA: NBMG BULL. 61, P. 167

  • Deposit

    HOLMES, 1965, MERCURY IN NEVADA; USBM 1C 8252, P. 249-250.

  • Production

    USBM UNPUB DATA

General comments

Subject category Comment text
Deposit TWO NARROW ECHELON RIDGES ARE FORMED BY CARBONATES CUT BY DIABASE DIKES. THE STRATIGRAPHIC UNITS CONSIST OF SHALE OVERLAIN BY BLACK SANDSTONE, OVERLAIN BY THIN LAYER OF BUFF SANDSTONE, OVERLAIN BY CONGLOMERATIC DOLOMITE. THE BUFF SANDSTONE LAYER IS FOLLOWED AS A "KEY BED" IN THE UNDERGROUND MINING. MOST OF THE ORE BODIES OCCUR WHERE CINNABAR FILLS NUMEROUS IRREGULAR FRACTURES OR AS DISSEMINATED CRYSTALS IN THE UNBROKEN ROCK. DEPOSITS ARE FOLDED AND FAULTED INTO NW TRENDING RIDGES. SOUTH PART OF AREA-FANGLOMERATE; NORTH PART-BASALTS.
Deposit DISCOVERED IN 1912. MINING BEGAN 1916. PRODUCTION YEARS 1916-17, 1928-30, 1942-44, 1946. THE MINE EXPLORES PARTS OF TWO NARROW NORTH WESTERLY TRENDING ESCHALON RIDGES ABOUT 2 MILES LONG. LARGEST PRODUCER IN DISTRICT. ; INFO.SRC : 1 PUB LIT

Reporter information

Type Date Name Affiliation Comment
Reporter 01-NOV-1973 Bergquist, Joel R. Nevada Bureau of Mines and Geology
Updater 01-OCT-1980 Royse, Sue E. Nevada Bureau of Mines and Geology
Updater 01-SEP-1994 Li, Zhiping (Peters, S.) U.S. Geological Survey

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.