Delamar Zinc

The Delamar Zinc is a zinc and lead mine located in Lincoln county, Nevada at an elevation of 6,401 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: Delamar Zinc  

State:  Nevada

County:  Lincoln

Elevation: 6,401 Feet (1,951 Meters)

Commodity: Zinc, Lead

Lat, Long: 37.51722, -114.79167

Map: View on Google Maps

Satelite View

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Satelite image of the Delamar Zinc

Delamar Zinc MRDS details

Site Name

Primary: Delamar Zinc
Secondary: North Star Claims
Secondary: NBMG Sample Site 1745


Commodity

Primary: Zinc
Primary: Lead
Secondary: Silver
Secondary: Manganese
Tertiary: Molybdenum
Tertiary: Iron
Tertiary: Barium-Barite
Tertiary: Copper
Tertiary: Strontium
Tertiary: Vanadium
Tertiary: Cadmium


Location

State: Nevada
County: Lincoln
District: Delamar (Ferguson) District 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

Not available


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

Not available


Orebody

Form: TABULAR


Structure

Type: R
Description: Abundant Normal Faults


Alterations

Alteration Type: L
Alteration Text: Silicification


Rocks

Name: Silt
Role: Host
Age Type: Host Rock
Age Young: Late Cambrian


Analytical Data

Analytical Data: ORE RAN 15-30 % ZN AND 6 % PB. SAMPLE 1745 CONTAINS 20 000 PPM PB, 500 PPM SR, 200 PPM V, 5000 PPM ZN, 10 % FE, 15 % CA, GREATER THAN 5000 PPM MN, 100 PPM AG, 500 PPM BA, 200 PPM CD, 500 PPM CU, 50 PPM MO.


Materials

Ore: Smithsonite
Gangue: Calcite


Comments

Comment (Workings): INCLINED SHAFT, 3 SHAFTS: MAIN SHAFT FAIRLY DEEP AND MAY BE INCLINED AT DEPTH. SOME DRILLING WAS DONE ON THE OTHER SIDE OF THE RIDGE SOUTH OF THESE WORKINGS PROBABLY SEVERAL YEARS AGO., 3 SHAFTS: MAIN SHAFT FAIRLY DEEP AND MAY BE INCLINED AT DEPTH. SOME DRILLING WAS DONE ON THE OTHER SIDE OF THE RIDGE SOUTH OF THESE WORKINGS PROBABLY SEVERAL YEARS AGO.

Comment (Geology): ORE IN LIMESTONE NEAR VOLCANIC CONTACT, CONTAINING 15-30% ZN, 6% PB.

Comment (Deposit): SHAFTS SUNK ON A NE-STRIKING FAULT IN THE CHISHOLM SHALE AND ON A NW-STRIKING FAULT BETWEEN THE HIGHLAND PEAK LIMESTONE AND CHISHOLM SHALE. PRESENCE OF GOSSAN BRECCIA SUPPORTS A FAULT-RELATED ORIGIN. SHAFT NO. 1 (WESTERNMOST) EXPOSES A 2 FT WIDE REPLACEMENT VEIN WHICH PARALLELS THE BEDDING OF THE HOST LIMESTONE. THE VEIN STRIKES N40E, DIPS 60SE AND HAS A SHARP CONTACT WITH ENCLOSING HOST ROCK, WHICH APPEARS LITTLE ALTERED. VEIN IS COMPLETELY OXIDIZED, AND CONSISTS OF LIMONITIC AND MN-RICH GOSSAN WITH SOME CALCITE AND SILICA VEINING AND VUG FILLINGS. CALCITE (AND PROBABLY SOME SMITHSONITE) ALSO CEMENTS GOSSAN BRECCIA FOUND ON THE DUMP. THE GOSSAN IS QUITE DENSE AND MAY CONTAIN PB OR ZN MINERALS, BUT NO UNOXIDIZED MINERALS WERE OBSERVED. SHAFT NO. 2, (SOUTHERNMOST): UPPER SHAFT EXPLORES SIMILAR REPLACEMENT VEIN 5-6 FT WIDE STRIKING N30E, DIP 80SE. THE VEIN POSSIBLY PARALLELS THE BEDDING OR CROSSCUTS THE BEDDING AT A LOW ANGLE. THE GOSSAN "VEIN" IS NOT AS PURE OR HIGHGRADE AS THAT

Comment (Deposit): OBSERVED IN NO. 1. INSTEAD, IT IS SPOTTY, PINCHES OUT AND CONTAINS LIMESTONE LENSES ALONG FRACTURES PARALLEL TO BEDDING. SHAFT NO. 3 (NORTHERNMOST): LOWER SHAFT IS INCLINED ALONG STRIKE OF N10-20E (POORLY EXPOSED) TRENDING GOSSAN REPLACEMENT VEIN WHICH IS PROBABLY A CONTINUATION OF THE VEIN OBSERVED IN NO. 2. ADIT (OR INCLINE) LOCATED BELOW AND INTERSECTING THE SHAFT IS CAVED. DUMP CONSISTS OF LIMESTONE WASTE ROCK AND LIMONITIC MN-GOSSAN WHICH IN GENERAL IS LIGHT-WEIGHT, PUNKY, AND IN PART SILICEOUS. SAMPLE 1745 WAS TAKEN FROM THIS SHAFT.

Comment (Development): NORTH STAR CLAIMS LOCATED 1974 BY 2 PERSONS FROM CALIENTE (NAMES ILLEGIBLE). NO ACTIVITY AT TIME OF EXAMINATION IN 1983

Comment (Commodity): ORE MINERALS NOT GIVEN IN THE REFERENCE


References

Reference (Deposit): TSCHANZ, C.M., AND PAMPEYAN, E.H., 1970, GEOLOGY AND MINERAL DEPOSITS OF LINCOLN CO, NEV. NEV BUR MINES BULL 73 P. 141

Reference (Deposit): CALLAGHAN, E., 1937, GEOLOGY OF THE DELAMAR DISTRICT, LINCOLN CO., NEV BUR MINES V. 31 NO. 5

Reference (Deposit): BENTZ, J. AND SMITH, P., 1983, FIELD EXAMINATION REPORT, SEPT 22, 1983


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 at Gold Districts of Nevada.