The New Tempiute Mine is a tungsten, silver, fluorine-fluorite, and zinc mine located in Lincoln county, Nevada at an elevation of 7,300 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
Elevation: 7,300 Feet (2,225 Meters)
Commodity: Tungsten, Silver, Fluorine-Fluorite, Zinc
Lat, Long: 37.63083, -115.62806
Map: View on Google Maps
Satelite View
MRDS mine locations are often very general, and in some cases are incorrect. Some mine remains have been covered or removed by modern industrial activity or by development of things like housing. The satellite view offers a quick glimpse as to whether the MRDS location corresponds to visible mine remains.
New Tempiute Mine MRDS details
Site Name
Primary: New Tempiute Mine
Secondary: NBMG Sample Sites 1452
Secondary: 1453
Secondary: 1454.
Commodity
Primary: Tungsten
Primary: Silver
Primary: Fluorine-Fluorite
Primary: Zinc
Tertiary: Bismuth
Location
State: Nevada
County: Lincoln
District: Tempiute District
Land Status
Land ownership: BLM Administrative Area
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: Union Carbide, Minerals Division
Owner Name: Union Carbide
Production
Not available
Deposit
Record Type: Site
Operation Category: Producer
Operation Type: Unknown
Discovery Year: 1916
Years of Production:
Organization:
Significant: N
Deposit Size: S
Physiography
Not available
Mineral Deposit Model
Model Name: W skarn
Orebody
Not available
Structure
Type: L
Description: Intersecting High-And Low-Angle Faults Striking Nw And Sw, Exposed On Face Of The Open Pit; Shearing Parallel To Bedding
Alterations
Alteration Type: L
Alteration Text: Argillic, Bleaching, Silicification
Rocks
Name: Granite
Role: Associated
Age Type: Host Rock
Age Young: Mississippian
Name: Granite
Role: Associated
Age Type: Associated Rock
Age Young: Pliocene
Analytical Data
Analytical Data: SAMPLES 1452, 1453, 1454 CONTAIN 15-20% FE, 3000-GREATER THAN 5000 PPM MN, 0-1 PPM AG, 0-200 PPM AS 0-1000 PPM BA, 0-150 PPM CO, 100-200 PPM CU, 0-300 PPM MO, 0-70 PPM NI, 10-100 PPM PB, 0-300 PPM SR, 20-150 PPM V, 50-10,000 PPM W, 700-GREATER THAN 10,000 PPM ZN.
Materials
Ore: Scheelite
Ore: Sphalerite
Ore: Bismuthinite
Ore: Fluorite
Ore: Chalcopyrite
Gangue: Siderite
Gangue: Tremolite
Gangue: Nontronite
Gangue: Quartz
Gangue: Calcite
Gangue: Pyrite
Gangue: Garnet
Gangue: Iron
Gangue: Wollastonite
Comments
Comment (Deposit): ADJACENT TO THE QUARTZ VEINS. WORKINGS EAST OF THE OPEN PIT NEAR THE SADDLE INCLUDE ANOTHER SMALL RATHER DEEP AND NARROW OPEN PIT WHICH EXCAVATED ORE ALONG THE CONTACT OF THE INTRUSIVE AND THE SKARN ZON
Comment (Workings): OPEN PIT; ADIT OR CAVE; NARROW DEEP PIT
Comment (Development): SOUTHERN-MOST WORKINGS OF UNION CARBIDE'S PROPERTY AT TEMPIUTE. NO PRODUCTION AT TIME OF EXAMINATION IN 1983. BUT DEVELOPMENT WORK, BLASTING, ETC. WAS BEIN CONTINUED.
Comment (Location): UNSURVEYED ; INFO FROM LAND.ST :1972
Comment (Deposit): SKARN ZONE OF WHICH ONLY MINOR REMNANTS REMAIN EXPOSED ALONG 3-5 BENCHES. ON THE E AND W SIDES. TONGUES OF THE GRANITE BODY EXTEND INTO THE LIMESTONE UNIT AND ARE ARGILLICALLY ALTERED, BLEACHED, HEAVILY IRON-STAINED WITH LIMESTONE-HORNFELS ALONG THE CONTACT. SKARN MINERALS INCLUDE GARNET, PYRITE, BISMUTHINITE (?), PYRRHOTITE, CHALCOPYRITE, SPHALERITE, FLUORITE, CALCITE, AND WOLLASTONITE. THE IRON-RICH SULFIDES ARE ALTERED TO A GREENISH CLAYEY MATERIAL RESEMBLING NONTRONITE. WESTERN EDGE OF SKARN ZONE IS MORE GOSSANY; LIMONITE-STAINED, AND EXHIBITS A GREATER DEGREE OF HYDROTHERMAL ALTERATION WITH MUCH SLAG-LIKE MATERIAL. A MASSIVE WHITE QUARTZ VEIN WITH ABUNDANT OPEN SPACES CARRYING OXIDIZED PYRITE GRAINS AND GHOSTS, CUTS BOTH THE LIMESTONE AND THE SKARN ZONE. VERY FINE TREMOLITE CRYSTALS ARE INTERGROWN IN THE LIMESTONE. MASSIVE (UP TO SEVERAL FEET WIDE) VEINS/CLOTS OF CRYSTALLINE CALCITE/SIDERITE/MANGANOSIDERITE OCCUR IN THE LIMESTONE. LOCALLY THE LIMESTONE IS SILICIFIED NEAR AND
References
Reference (Deposit): SMITH, P. AND BENTZ, J., 1983, FIELD EXAMINATION REPORT, OCT. 3, 1983.
Reference (Deposit): TSCHANZ, E.H. AND PAMPEYAN, C.M., 1970, NBMG BULL. 73.
Nevada Gold
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.
