The Lucky Chief is a lead and silver mine located in Lincoln county, Nevada at an elevation of 5,801 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
Elevation: 5,801 Feet (1,768 Meters)
Commodity: Lead, Silver
Lat, Long: 37.69528, -114.52222
Map: View on Google Maps
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Lucky Chief MRDS details
Site Name
Primary: Lucky Chief
Secondary: Part of Soa Lode Claims 1983
Commodity
Primary: Lead
Primary: Silver
Secondary: Zinc
Secondary: Gold
Tertiary: Manganese
Tertiary: Barium-Barite
Location
State: Nevada
County: Lincoln
District: Chief
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
Not available
Production
Year: 1926
Material type: ORE
Description: Ap_Grade: ^18% Pb, Negligible Au And Ag
Deposit
Record Type: Site
Operation Category: Past Producer
Operation Type: Unknown
Years of Production:
Organization:
Significant: N
Deposit Size: S
Physiography
Not available
Mineral Deposit Model
Not available
Orebody
Form: IRREGULAR TO TABULAR WITH PINCH AND SWELL
Structure
Type: L
Description: Fault, N-S Trend, Fracture Zone
Alterations
Not available
Rocks
Name: Diorite
Role: Associated
Age Type: Associated Rock
Age Young: Pliocene
Name: Diorite
Role: Associated
Age Type: Host Rock
Age Young: Late Cambrian
Analytical Data
Analytical Data: SAMPLE 121 CONTAINS 10% FE, 20% CA, GREATER THAN 5000 PPM MN, 150 PPM AG, 500 PPM AS, 3000 PPM 3A, 100 PPM CD, 2000 PPM PB, 200 PPM SB, 500 PPM SR, GREATER THAN 10 000 PPM ZN.
Materials
Ore: Plumbojarosite
Gangue: Jasper
Gangue: Calcite
Gangue: Opal
Gangue: Quartz
Gangue: Pyrite
Gangue: Sericite
Comments
Comment (Geology): IRREGULAR ORE BODY IN THRUST (?) BRECCIA ZONE BETWEEN ISOLATED BLOCKS OF THE LIMESTONE AND QUARTZITE. ORE CONSISTS OF GRAINS AND NODULES OF CERUSSITE, POWDERY OPAL, PLUMBOJAROSITE & LUMPS OF FE & MN OXIDES IN FINE GRAINED QUARTZ INTENSE FRACTURING HAS OCCURRED THROUGHOUT THE AREA DUE TO MOVEMENT ALONG THE MAJOR FAULT. ROCKS ARE BRECCIATED AND IRON-STAINED. QUARTZITE AND SILTY SANDSTONE AT PORTAL ARE VEINED BY FE AND WHITE TO GREY CALCITE. GOSSANY BRECCIA CEMENTED WITH CALCITE ON DUMP CONTAINS LENSES AND VEINS OF BLADED SILVERY PYROLUSITE (?) AND WHITE BARITE CRYSTALS. THE GOSSAN IS SLIGHTLY YUGGY AND HEAVY. IRON-STAINED JASPER IS COMMON ALONG THE FAULT ZONE AND IN THE GOSSAN. QUARTZITE WALLROCK CONTAINS SOME OXIDIZED PYRITE AND SERICITE. FAULT ZONE AT LOWER PORTAL IS STRONGLY FE-MN-STAINED WITH ATTITUDE OF ABOUT N80E, 15SE. UPSLOPE FROM THIS ADIT ARE SHAFTS AND SHORT ADITS WHICH EXPLORE THE SAME IRON-STAINED BRECCIATED THRUST ZONE. CLOTS OF HEMATITE, LIMONITE, AND MANGANESE OCCUR IN
Comment (Geology): LIMONITE, AND MANGANESE OCCUR IN THE LIGHT GREY FINE-GRAINED QUARTZITE WALLROCK. FAULT ZONE IS ALTERED TO CLAY AND FE-MN OXIDES, BUT BELOW THE THRUST, THE QUARTZITE BEDS ARE FRACTURED AND HIGHLY MN-STAINED. MOST OF THE WORKINGS ARE IN QUARTZITE, BUT LIMESTONE OUTCROPS JUST SW OF THE WORKINGS.
Comment (Geology): THE LIGHT GREY FINE-GRAINED QUARTZITE WALLROCK. FAULT ZONE IS ALTERED TO CLAY AND FE-MN OXIDES, BUT BELOW THE THRUST, THE QUARTZITE BEDS ARE FRACTURED AND HIGHLY MN-STAINED. MOST OF THE WORKINGS ARE IN QUARTZITE, BUT LIMESTONE OUTCROPS JUST SW OF THE WORKINGS. INTENSE FRACTURING HAS OCCURRED THROUGHOUT THE AREA DUE TO MOVEMENT ALONG THE MAJOR FAULT. ROCKS ARE BRECCIATED AND IRON-STAINED. QUARTZITE AND SILTY SANDSTONE AT PORTAL ARE VEINED BY FE AND WHITE TO GREY CALCITE. GOSSANY BRECCIA CEMENTED WITH CALCITE ON DUMP CONTAINS LENSES AND VEINS OF BLADED SILVERY PYROLUSITE (?) AND WHITE BARITE CRYSTALS. THE GOSSAN IS SLIGHTLY YUGGY AND HEAVY. IRON-STAINED JASPER IS COMMON ALONG THE FAULT ZONE AND IN THE GOSSAN. QUARTZITE WALLROCK CONTAINS SOME OXIDIZED PYRITE AND SERICITE. FAULT ZONE AT LOWER PORTAL IS STRONGLY FE-MN-STAINED WITH ATTITUDE OF ABOUT N80E, 15SE. UPSLOPE FROM THIS ADIT ARE SHAFTS AND SHORT ADITS WHICH EXPLORE THE SAME IRON-STAINED BRECCIATED THRUST ZONE. CLOTS OF HEMATITE,
Comment (Location): SE PART OF SECTION ; INFO FROM LAND.ST :(1972)
Comment (Development): 3 CLAIMS. NO ACTIVITY AT TIME OF EXAMINATION IN 1983, BUT PROPERTY WAS STAKED FAIRLY RECENTLY.
Comment (Workings): TUNNEL, INACCESSIBLE DEEP PITS OR SHAFTS. IN 1983, A VERTICAL SHAFT AND A N30W-TRENDING ADIT WERE THE MAIN WORKINGS, WITH SHALLOW TRENCHES AND PROSPECTS AND SHORT ADITS SCATTERED ALONG THE FAULT ZONE.. IN 1983, A VERTICAL SHAFT AND A N30W-TRENDING ADIT WERE THE MAIN WORKINGS, WITH SHALLOW TRENCHES AND PROSPECTS AND SHORT ADITS SCATTERED ALONG THE FAULT ZONE.
References
Reference (Deposit): TSCHANTZ CM & PAMPEYAN EH, 1970, GEOLOGY AND MINERAL DEPOSITS OF LINCOLN COUNTY, NEV BUR MINES BULL 73
Reference (Deposit): BENTZ, J. AND SMITH, P., 1983, FIELD EXAMINATION REPORT, AUGUST 17, 1983.
Reference (Production): TSCHANTZ AND PAMPEYAN, 1970
Reference (Deposit): CALLAGHAN, E., 1936, UNR BULL VOL 30, NO 2, P.28.
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.
