Tmb Associates Claims

The Tmb Associates Claims is a gold mine located in Washoe county, Nevada at an elevation of 4,600 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: Tmb Associates Claims  

State:  Nevada

County:  Washoe

Elevation: 4,600 Feet (1,402 Meters)

Commodity: Gold

Lat, Long: 40.43361, -119.38778

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 Tmb Associates Claims

Tmb Associates Claims MRDS details

Site Name

Primary: Tmb Associates Claims
Secondary: NBMG Sample Sites 476,477
Secondary: Lake Range Mont Morillonite


Commodity

Primary: Gold
Secondary: Clay


Location

State: Nevada
County: Washoe
District: San Emidio Desert Area.


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: Tmb Associates
Years: 1979 -

Owner Name: Exploration Associates, Of Tucson
Years: 1979 -


Production

Not available


Deposit

Record Type: Site
Operation Category: Occurrence
Operation Type: Unknown
Years of Production:
Organization:
Significant: N
Deposit Size: S


Physiography

Not available


Mineral Deposit Model

Model Name: Hot-spring Au-Ag


Orebody

Not available


Structure

Not available


Alterations

Alteration Type: L
Alteration Text: Strong Silicification, Argillization


Rocks

Name: Tuff
Role: Host
Age Type: Host Rock
Age Young: Pliocene


Analytical Data

Analytical Data: SAMPLE 476 OF SELECTED FINELY LAMINATED SUBAQUEOUS SINTER CONTAINS 0.02% MG, 0.07% CA, 0.1% TI, 100 PPM MN, 5 PPM AG, 10 PPM B, 1000 PPM BA, 1.5 PPM BE, 20 PPM CU, 50 PPM LA, 100 PPM PB, 100 PPM SR, 20 PPM V, 30 PPM ZR. SAMPLE 477 OF REED-BEARING SINTER CONTAINS 0.02% MG, 0.07% CA, 20 PPM MN, 1.5 PPM AG, 50 PPM B, 500 PPM BA, 2 PPM BE, 10 PPM CU, 50 PPM LA, 100 PPM PB, 100 PPM SR, 20 PPM V, 10 PPM ZR.


Materials

Ore: Gold
Ore: Montmorillonite
Gangue: Chalcedony


Comments

Comment (Workings): DRILL ROADS, SHALLOW? DRILL HOLES

Comment (Location): ON A HILL ON THE NE SIDE OF THE SAN EMIDIO DESERT . INFO FROM LAND.ST :(1972)

Comment (Development): CLAIMS IN AREA STAKED BY EXPLORATION ASSOCIATES (OF TUCSON) FOR TMB ASSOCIATES IN 1979. EXPLORED FOR PRECIOUS METALS IN 1979-81; NO PREVIOUS EXPLORATION. SEVERAL KM OF NEW DRILL ROADS, SHALLOW? DRILL HOLES.

Comment (Deposit): THE AREA HAS BEEN KNOWN FOR 15 YRS OR MORE TO CONTAIN SILICIFIED REEDS IN PLIOCENE SEDIMENTARY ROCKS AN AREA OF 2-3 SQ. KM. IN THE PLIOCENE TUFFACEOUS AND VOLCANICLASTIC SEDIMENTARY ROCKS IS ARGILLIZED AND SILICIFIED. UNALTERED EQUIVALENT? STRATA ARE EXPOSED TO THE EAST OF THE LONE MINERALIZED HILL. THE HILL APPEARS TO BE CAPPED BY STRONGLY SILICIFIED SEDIMENTS, WHICH ARE UNDERLAIN AND SURROUNDED? BY ARGILIZED ROCKS. THE SILICIFIED ROCKS CONSIST, IN PART, OF SYN DEPOSITIONAL SUBAQUEOUS SPRING SINTER, PROBABLY PRODUCED BY SUBLACUSTRINE, SILICA-CHARGED HOT SPRINGS WHICH VENTED DURING THE DEPOSITION OF THE PLIOCENE SEDIMENTS. IN ADDITION TO THE REED-BEARING SUBAQUEOUS SINTER, A VERY FINELY AND EVENLY LAMINATED SINTER IS INTERPRETED AS BEING SUBAQUEOUS ALSO. THE PLIOCENE SEDIMENTARY ROCKS ARE GENTLY DIPPING, AND IN THE SILICIFIED AREA CONTAIN IRREGULAR PODS AND LENSES (UP TO 0.5 M THICK) OF LIGHT TO DARK GREY CHALCEDONY, BELIEVED TO BE SINTER. A FEW SILICIFIED HYDROTHERMAL?

Comment (Deposit): BRECCIAS WERE NOTED. AT A PROSPECT SYMBOL SHOWN ON THE TOPOMAP APPROX. ON THE SEC 27/SEC28 LINE, ARGILLIZED, TUFFACEOUS SEDIMENTS (SMECTITE CLAYS AND SELENITE GYPSUM ARE PRESENT) ARE EXPOSED. THIS PROSPECT IS PROBABLY THE LAKE RANGE MONTMORILLONITE DESCRIBED BY PAPKE (1969, P.113). ARGILLIC ALTERATION PROBABLY RESULTED FROM HYDROTHERMAL ALTERATION DURING THE PERIOD OF HOT SPRING DISCHARGE IN THE PLIOCENE LAKE PRODUCING A SINTER CAP OVER ARGILLIZED SEDIMENTS.


References

Reference (Deposit): GARSIDE, L.J., 15 JUN 83, NBMG FIELD EXAMINATION AND SAMPLE ANALYSES.

Reference (Deposit): BONHAM, H.F., JR., AND PAPKE, K.G., 1969, NBMG BULL 70, P.108-130.

Reference (Deposit): GARSIDE, L.J. AND SCHILLING, J.M., 1979, THERMAL WATERS OF NEVADA; NBMG BULL. 91.

Reference (Deposit): NBMG STAFF, 1985, NBMG OFR 85-3.


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.