Johnson-Heizer Mine

The Johnson-Heizer Mine is a antimony mine located in Pershing county, Nevada at an elevation of 4,551 feet.

About the MRDS Data:

All mine locations were obtained from the USGS Mineral Resources Data System. The locations and other information in this database have not been verified for accuracy. It should be assumed that all mines are on private property.

Mine Info

Name: Johnson-Heizer Mine

State:  Nevada

County:  Pershing

Elevation: 4,551 Feet (1,387 Meters)

Commodity: Antimony

Lat, Long: 40.28056, -118.32444

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Satelite image of the Johnson-Heizer Mine

Johnson-Heizer Mine MRDS details

Site Name

Primary: Johnson-Heizer Mine
Secondary: S.P., Ott Heizer Mine
Secondary: NBMG Sample Site 2579


Commodity

Primary: Antimony
Tertiary: Silver
Tertiary: Gold


Location

State: Nevada
County: Pershing
District: Willard District


Land Status

Land ownership: Private
Note: the land ownership field only identifies whether the area the mine is in is generally on public lands like Forest Service or BLM land, or if it is in an area that is generally private property. It does not definitively identify property status, nor does it indicate claim status or whether an area is open to prospecting. Always respect private property.


Holdings

Not available


Workings

Not available


Ownership

Owner Name: Santa Fe Minerals, (S. P.)
Years: 1985 -


Production

Year: 1916
Time Period: -1916
Material type: ORE SB
Description: Cp_Grade: ^45% Sb
Year: 1916
Material type: ORE SB
Description: Ap_Grade: ^45% Sb Ore


Deposit

Record Type: Site
Operation Category: Past Producer
Deposit Type: Vein
Operation Type: Unknown
Year First Production: 1916
Discovery Year: 1916
Years of Production:
Organization:
Significant: N
Deposit Size: S


Physiography

Not available


Mineral Deposit Model

Model Name: Low-sulfide Au-quartz vein


Orebody

Not available


Structure

Not available


Alterations

Not available


Rocks

Name: Shale
Role: Host
Age Type: Host Rock
Age Young: Late Jurassic


Analytical Data

Analytical Data: SAMPLE 2579, DUMP SELECT OF VEIN MATERIAL IN PHYLLITE CONTAINS 1 % FE, 0.5 % MG, 1.5 % CA, 0.07 % TI, 300 PPM MN, 0.7 PPM AG, 1000 PPM AS, 70 PPM B, 30 PPM BA, 1 PPM BE, 30 PPM CR, 50 PPM CU, 50 PPM LA, 10 PPM NI, 150 PPM PB, +1000 PPM SB, 300 PPM SR, 15 PPM V, 500 PPM ZN, 50 PPM ZR, AND 2.0 PPM AU (BY AA ANALYSIS).


Materials

Ore: Stibiconite
Ore: Stibnite
Gangue: Quartz
Gangue: Calcite
Gangue: Pyrite


Comments

Comment (Development): CONSISTS OF TWO ORE BODIES MINED AT DIFFERENT TIMES. THE SOUTHERN BODY WAS FIRST MINED IN 1916; THE NORTHERN IN 1946. THE DEPOSIT WAS EXPLORED BY TRENCHING FOR 2500 FT ALONG SHEAR ZONE. NO ACTIVITY IN 1985.

Comment (Deposit): FOUND IN 1916. CONSISTS OF TWO ORE BODIES MINED AT DIFFERENT TIMES. THE SOUTHERN ORE BODY WAS FIRST MINED IN 1916. THE NORTHERN ORE BODY WAS NOT MINED TILL 1946. DEPOSIT IS DEVELOPED BY A 264-FT. INCLINED SHAFT FROM WHICH SOME 440 FEET OF DRIFTING AND CONSIDERABLE STOPING WERE DONE. EXPLORED BY TRENCHING FOR 2500 FT. ALONG SHEAR ZONE; SHAFT WAS SUNK ON VEIN TO THE SOUTHEAST. ; INFO.SRC : 1 PUB LIT; 2 UNPUB REPT; 3 FIELD OBSERV

Comment (Deposit): CONSISTS OF TWO ORE BODIES. VEIN VARIES IN THICKNESS FROM 6 TO 25 INCHES, AVERAGING 12 INCHES. STIBNITE OCCURS AS PODS, VEINLETS, AND FINE HAIRLIKE CRYSTALS, COMMONLY IN QUARTZ AND CALCITE STRINGERS. PYRITE PRESENT ALONG EDGE OFUARTZ STRINGERS. STIBNITE ALSO OCCURS ALONG BEDDING PLANES IN THE CONTORTED AND ECCIATED SHALE WALL ROCK. THE STIBNITE HAS BEEN PARTIALLY OXIDIZED TO YELLOW ANDHITE SB-OXIDES NEAR THE SURFACE. VEIN ZONE APPROXIMATELY PARALLELS BEDDING IN SEDIMENTARY ROCKS WITH VEINS BEST DEVELOPED IN QUARTZITE BED.; MODEL NAME COULD ALSO BE: SIMPLE SB.

Comment (Workings): DEPOSIT IS DEVELOPED BY A 264-FT INCLINED SHAFT FROM WHICH SOME 440 FEET OF DRIFTING AND CONSIDERABLE STOPING WERE DONE.

Comment (Geology): VEIN VARIES IN THICKNESS FROM 6 TO 25 INCHES, AVERAGING 12 INCHES. STIBNITE OCCURS AS PODS, VEINLETS, AND FINE HAIRLIKE CRYSTALS, COMMONLY IN QUARTZ AND CALCITE STRINGERS. PYRITE PRESENT ALONG EDGE OF QUARTZ STRGERS. STIBNITE ALSO OCCURS ALONG BEDDING PLANES IN THE CONTORTED AND BRECCIATED ALE WALL ROCK. THE STIBNITE HAS BEEN PARTIALLY OXIDIZED TO YELLOW AND WHITE SB-ODES NEAR THE SURFACE.


References

Reference (Deposit): JOHNSON, M.G., 1977, GEOLOGY AND MINERAL DEPOSITS OF PERSHING COUNTY, NEVADA; NBMG BULLETIN 89.

Reference (Deposit): LAWRENCE, E.F., 1963, ANTIMONY DEPOSITS OF NEVADA; NBMG BULLETIN 61.

Reference (Deposit): SOUTHERN PACIFIC CO., 1964, MINERALS FOR INDUSTRY-NORTHERN NEVADA AND NORTHSTERN UTAH-SUMMARY OF GEOLOGICAL SURVEY 1955-1961, V.1, SO. PACIFIC CO, SAN FRANCISCO, P 13.

Reference (Deposit): BONHAM, H.F., 17 JUL 85, NBMG FIELD EXAMINATION AND SAMPLE ANALYSIS. #5. NBMG STAFF, 1985, NBMG OFR 85-3.

Reference (Production): JOHNSON, 1977


Nevada Gold

Gold Districts of Nevada

Nevada has a total of 368 distinct gold districts. Of the of those, just 36 are major producers with production and/or reserves of over 1,000,000 ounces, 49 have production and/or reserves of over 100,000 ounces, with the rest having less than 100,000 ounces. Read more: Gold Districts of Nevada.