Adriene Mine

The Adriene Mine is a antimony mine located in Pershing county, Nevada at an elevation of 5,049 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: Adriene Mine  

State:  Nevada

County:  Pershing

Elevation: 5,049 Feet (1,539 Meters)

Commodity: Antimony

Lat, Long: 40.25972, -118.30111

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 Adriene Mine

Adriene Mine MRDS details

Site Name

Primary: Adriene Mine
Secondary: Louis Lay Claim
Secondary: NBMG Sample Site 2581


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: Rosal Mining And Land Co.
Years: 1957 -


Production

Not available


Deposit

Record Type: Site
Operation Category: Past Producer
Deposit Type: Vein
Operation Type: Unknown
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

Alteration Type: L
Alteration Text: Sericitization


Rocks

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


Analytical Data

Analytical Data: ADRIENE NO. 2:6.81-10.46% SB, 0.48-0.50 OZ AG, TRACE A. SAMPLE 2581 OF QUARTZ STOCKWORK MATERIAL AND HOST ROCK CONTAINS 0.7 % FE, 0.07 % MG, 3 % CA, 0.05 % TI, 150 PPM MN, 0.5 PPM AG, 1500 PPM AS, 30 PPM B, 150 PPM BA, 10 PPM CR, 200 PPM CU, 100 PPM LA, 15 PPM NI, 2000 PPM PB, +10000 PPM SB, 300 PPM SR, 700 PPM ZN, 50 PPM ZR, AND 0.1 PPM AU, BY AA ANALYSIS.


Materials

Ore: Stibnite
Gangue: Tourmaline
Gangue: Quartz
Gangue: Clay
Gangue: Sericite


Comments

Comment (Location): SW/4 SEC. 29, HAS 5079 BM AT TOP OF HILL

Comment (Deposit): THE PROPERTY INCLUDES CLAIMS NOS. 1,2, AND 3. ON ADRIENE NO. 1 CLAIM TWO QUARTZ-ANTIMONY VEINS OCCUR IN INTERBEDDED SHALE AND QUARTZITE WITH MAIN VEIN, 8 TO 12 INCHES WIDE, STRIKES N5W AND DIPS 45-65 DEGREES W TERMINING AGAINST A 6 TO 12 INCH VEIN STRIKING N65W AND DIPS 70 DEGREES S. QUARTZ-SB SINGERS OCCUR AT THE INTERSECTION OF THE TWO VEINS. ON ADRIENE NO. 2 CLAIM 4 TO 24 INCH QUARTZ-SB VEINS STRIKING N20W AND DIPPING 70-75 DEGREES W OCCUR IN QUARTZE WITH SOME INTERBEDDED SANDSTONE. THE VEIN MAY BE A CONTINUATION OF THAT ON THE ADRIENE NO.1 CLAIM. ANTIMONY OCCURS AS PODS AND INDIVIDUAL CRYSTALS OF STIBNITE IN THE QUARTZ STRINGERS. MUCH OF THE STIBNITE HAS BEEN OXIDIZED. PODS OF SB OXIDE AND STIBNITE IN 2-5 CM QUARTZ VEINLETS; PHYLLITES ARE LARGELY BARREN, PROBABLY A FACTOR OF THE GREATER COMPETENCY OF SANDSTONE VERSUS PHYLLITES.; MODEL NAME COULD ALSO BE: SIMPLE SB.

Comment (Workings): TWO SHALLOW SHAFTS, SEVERAL TRENCHES AND AN OPEN CUT AND ADIT, DRILL ROADS, DRILL HOLES, 3-5 YEARS OLD.

Comment (Geology): ON ADRIENE NO. 1 CLAIM TWO QUARTZ-ANTIMONY VEINS OCCUR IN INTER BEDDED SHALE AND QUARTZITE WH MAIN VEIN, 8 TO 12 INCHES WIDE, STRIKES N5W AND DIPS 45-65 DEGREES W TERMINATI AGAINST A 6 TO 12 INCH VEIN STRIKING N65W AND DIPS 70 DEGREES S. QUARTZ-SB STRIERS OCCUR AT THE INTERSECTION OF THE TWO VEINS. ON ADRIENE NO. 2 CLAIM 4 TO 24 INCH QUARTZ-SB VEINS STRIKING N20W AND DIPPING 70-75 DEGREES W OCCUR IN QUARTZITEITH SOME INTERBEDDED SANDSTONE. THE VEIN MAY BE A CONTINUATION OF THAT ON THE ADRIENE NO. 1 CLAIM. ANTIMONY OCCURS AS PODS AND INDIVIDUAL CRYSTALS OF STIBNITE IN THE QUARTZ STRINGERS. MUCH OF THE STIBNITE HAS BEEN OXIDIZED.

Comment (Development): NO ACTIVITY IN 1985; IDLE 4-5 YEARS.

Comment (Deposit): THE PROPERTY INCLUDES THE ADRIENE CLAIMS NOS. 1.2. AND 3, LOCATED END TO END ALONG A NORTHWEST-TRENDING RIDGE. IT IS DEVELOPED BY 2 SHALLOW SHAFTS, SEVERAL TRENCHES, AND AN OPEN CUT AND ADIT. ; INFO.SRC : 1 PUB LIT; 2 UNPUB REPT; 3 FIELD OBSERV


References

Reference (Deposit): VANDERBURG, W.O., 1936, RECONNAISSANCE OF MINING DISTRICTS IN PERSHING COUNTY, USBM INF CIRC 6902.

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

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 BULLETON 61.


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.