Hulse Mine

The Hulse Mine is a uranium mine located in Lincoln county, Nevada at an elevation of 6,801 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: Hulse Mine  

State:  Nevada

County:  Lincoln

Elevation: 6,801 Feet (2,073 Meters)

Commodity: Uranium

Lat, Long: 38.45528, -114.33278

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.


Satelite image of the Hulse Mine

Hulse Mine MRDS details

Site Name

Primary: Hulse Mine
Secondary: Bluebird
Secondary: Ella, Minnie, and Lucky Dog Claims


Commodity

Primary: Uranium
Secondary: Silver
Secondary: Gold
Tertiary: Arsenic
Tertiary: Lead
Tertiary: Copper


Location

State: Nevada
County: Lincoln
District: Atlanta District; Silver Park District; Silver Springs 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

Type: Surface/Underground


Ownership

Owner Name: James G. Hulse
Home Office: Pioche
Years: 1945 -


Production

Not available


Deposit

Record Type: Site
Operation Category: Past Producer
Operation Type: Unknown
Discovery Year: 1954
Years of Production:
Organization:
Significant: N
Deposit Size: S


Physiography

Not available


Mineral Deposit Model

Model Name: Volcanogenic U


Orebody

Form: TABULAR TO POD-SHAPED


Structure

Type: L
Description: Fault Zone


Alterations

Alteration Type: L
Alteration Text: Pyrite Alters To Carphosiderite , Silicification, Oxidation , Silicification, Oxidation


Rocks

Not available


Analytical Data

Analytical Data: 0.41 OZ/T AG.
Analytical Data: NO AU
Analytical Data: 0.12 % PB
Analytical Data: 0.2 % CU
Analytical Data: 0.41 OZ/T AG. . ONE SAMPLE FROM THE PYRITE-BEARING AREA OF THE MINE CONTAINED 0.133 % U308
Analytical Data: NO AU
Analytical Data: 0.12 % PB
Analytical Data: 0.2 % CU
Analytical Data: CHEMICAL ANALYSIS OF 2 SAMPLES: .11%, .67% U .1%, .3% AS . ONE SAMPLE FROM THE PYRITE-BEARING AREA OF THE MINE CONTAINED 0.133 % U308


Materials

Ore: Uraninite
Ore: Uranophane
Ore: Argentite
Gangue: Pyrite
Gangue: Quartz
Gangue: Marcasite


Comments

Comment (Workings): UNDERGROUND WORKINGS INCLUDE WINZES, CROSSCUTS AND DRIFTS. THREE DIAMOND DRILL HOLES TOTALLING 660 FT WERE DRILLED IN 1955. SHALLOW TEST PITS WERE DUG BY THE USBM. A WOODEN HEADFRAME REMAINED IN 1981.

Comment (Location): AREA UNSURVEYED . LOCATED ON A SMALL HILL 3500 FT S OF ATLANTA MILL.. LOCATED ON A SMALL HILL 3500 FT S OF ATLANTA MILL. ; INFO FROM LAND.ST :(1972)

Comment (Commodity): OTHER ORE MINERALS NOT GIVEN IN THE LITERATURE

Comment (Production): TWO CARLOADS

Comment (Geology): PODS OF PYRITE-URANINITE ORE OCCUR IN TABULAR JASPEROID ZONES ALONG FLATLY DIPPING FAULTS WHICH CONTAIN SILICIFIED GOUGE 1-4 FEET THICK. MINERALIZATION CONTROLLED BY AN INTRUSIVE BRECCIA ZONE OR PIPE WHICH WAS LATER CUT BY MANY MINOR N 35-55 W FAULTS.

Comment (Deposit): PODS OF PYRITE-URANINITE ORE OCCUR IN TABULAR JASPEROID ZONES ALONG GENTLY DIPPING FAULTS WHICH CONTAIN 1-4 FT THICK SILICIFIED GOUGE ZONES. MINERALIZATION APPEARS TO HAVE BEEN CONTROLLED BY AN INTRUSIVE BRECCIA ZONE OR PIPE WHICH WAS LATER CUT BY MANY MINOR FAULTS STRIKING N 35-55W. THE JASPEROID BODY CONSISTS OF FRAGMENTS OF DOLOMITE AND VOLCANICS WHICH ARE COMPLETELY SILICIFIED. OPEN SPACES IN THE BRECCIA ARE COMMON. ROCKS FROM THE UPPER LEVELS OF THE MINE ARE COMPLETELY OXIDIZED. ON THE LOWEST MINE LEVEL, MUCH PYRITE IS DISSEMINATED IN DARK GREY TO BLACK HIGHLY SILICIFIED BRECCIA. THE SILICIFIED BRECCIA ZONE HAS BEEN INTRUDED BY MANY N70E-STRIKING 15-20W-DIPPING ALTERED RHYOLITE DIKES. URANIUM MINERALIZATION APPEARS TO BE CONFINED TO THE SILICIFIED BRECCIA BETWEEN THE DIKES. YELLOW SECONDARY URANIUM OXIDES OCCUR NEAR THE SURFACE. PYRITE REPORTEDLY ALTERS TO CARPHOSIDERITE.


References

Reference (Deposit): TSCHANTZ CM & PAMPEYAN EH, 1970, GEOLOGY AND MINERAL DEPOSITS OF LINCOLN CO., NEV BUR MINES BULL 73

Reference (Deposit): GARSIDE, L. J., 1973, NBMG BULL 81, P. 68-69.

Reference (Deposit): SHARP, B. J. AND MYERSON B. L., 1956, US AEC REPORT RME-2048

Reference (Deposit): USGS PP 455 A-F

Reference (Deposit): COX, JOHN W., 1981, GEOLOGY AND MINERALIZATION OF THE ATLANTA DISTRICT, LINCOLN COUNTY, NEVADA: M. S. THESIS, UNIV OF NEVADA, RENO.


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.