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Goldfield Mine, Goldfield Mining District, Esmeralda County, Nevada, USAi
Regional Level Types
Goldfield MineMine
Goldfield Mining DistrictMining District
Esmeralda CountyCounty
NevadaState
USACountry

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Latitude & Longitude (WGS84):
37° 43' 29'' North , 117° 13' 14'' West
Latitude & Longitude (decimal):
Locality type:
KΓΆppen climate type:
Nearest Settlements:
PlacePopulationDistance
Goldfield268 (2011)2.3km
Silver Peak107 (2011)36.6km
Tonopah2,478 (2011)38.0km
Other/historical names associated with this locality:
Coulmbia Mtn. West Tunnel; Goldfield; Goldfield Consolidated Main Vein; Goldfield Project; Check Out These Properties:; Goldfield Mill 0320099018; Goldfield Vector 0320090727; Goldfield Geochen 0320090744; Columbia 0320090273; Columbia Mt. Alunite 0320090030; Columbia Mtn. East Tunnel


Deposit: THIS PROPERTY COVERS PORTIONS OF SECTIONS 25, 26, 35, AND 36, T. 2 S., R. 42 E, AND SEC. 1, T. 3 S, R. 42 E.

Geology: General size of ore body is large. The project is primarily located in the milltown andesite pit area geology unavailable, data describes area of dist. And the overlying dacite, which are more or less concentrically surrounded by ashflow tuffs and lacustrine tuffaceous beds. Both the milltown and overlying dacite are highly bleached and altered. The bleached rocks have been argillized, alunitized, and silicified, and both are host for ore deposits. The ore deposits are closely allied to fissure veins. Structurally the deposits are irregular masses of altered and mineralized rock traversed by irregular intersecting fractures, with the fractures passing into places of thorough becciation. Typically, the ore masses are called ledges. Within the zone of oxidation the ledges are silicified into fractured and porous jasperiod. Below this zone, the ledges become less silileous and less porous. The mineralized ledges range from a few feet to hundreds of feet in length. The ore bodies within the ledges vary in shape from pipes to equidimensional bodies. The dips vary but are generally greater than 49 degrees to the east and appear to align themselves downdip. The overall dimensions of the gold -field ore body is estimated to be 30 meters deep, 460 meters in length, and nearly 45 meters wide.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Commodity List

This is a list of exploitable or exploited mineral commodities recorded at this locality.


Mineral List


14 valid minerals.

Detailed Mineral List:

β“˜ Bismuthinite
Formula: Bi2S3
Reference: U.S. Geological Survey (2005) Mineral Resources Data System: U.S. Geological Survey, Reston, Virginia.
β“˜ Calaverite
Formula: AuTe2
Reference: U.S. Geological Survey (2005) Mineral Resources Data System: U.S. Geological Survey, Reston, Virginia.
β“˜ Chalcopyrite
Formula: CuFeS2
Reference: U.S. Geological Survey (2005) Mineral Resources Data System: U.S. Geological Survey, Reston, Virginia.
β“˜ Famatinite
Formula: Cu3SbS4
Reference: U.S. Geological Survey (2005) Mineral Resources Data System: U.S. Geological Survey, Reston, Virginia.
β“˜ Galena
Formula: PbS
Reference: U.S. Geological Survey (2005) Mineral Resources Data System: U.S. Geological Survey, Reston, Virginia.
β“˜ Gold
Formula: Au
Reference: U.S. Geological Survey (2005) Mineral Resources Data System: U.S. Geological Survey, Reston, Virginia.
β“˜ Gypsum
Formula: CaSO4 · 2H2O
Reference: U.S. Geological Survey (2005) Mineral Resources Data System: U.S. Geological Survey, Reston, Virginia.
β“˜ Halloysite
Formula: Al2(Si2O5)(OH)4
Reference: U.S. Geological Survey (2005) Mineral Resources Data System: U.S. Geological Survey, Reston, Virginia.
β“˜ Hessite
Formula: Ag2Te
Reference: U.S. Geological Survey (2005) Mineral Resources Data System: U.S. Geological Survey, Reston, Virginia.
β“˜ 'Limonite'
Reference: U.S. Geological Survey (2005) Mineral Resources Data System: U.S. Geological Survey, Reston, Virginia.
β“˜ Petzite
Formula: Ag3AuTe2
Reference: U.S. Geological Survey (2005) Mineral Resources Data System: U.S. Geological Survey, Reston, Virginia.
β“˜ Pyrite
Formula: FeS2
Reference: U.S. Geological Survey (2005) Mineral Resources Data System: U.S. Geological Survey, Reston, Virginia.
β“˜ Quartz
Formula: SiO2
Reference: U.S. Geological Survey (2005) Mineral Resources Data System: U.S. Geological Survey, Reston, Virginia.
β“˜ Quartz var. Jasper
Reference: U.S. Geological Survey (2005) Mineral Resources Data System: U.S. Geological Survey, Reston, Virginia.
β“˜ Sphalerite
Formula: ZnS
Reference: U.S. Geological Survey (2005) Mineral Resources Data System: U.S. Geological Survey, Reston, Virginia.
β“˜ Sylvanite
Formula: AgAuTe4
Reference: U.S. Geological Survey (2005) Mineral Resources Data System: U.S. Geological Survey, Reston, Virginia.
β“˜ 'Tennantite Subgroup'
Formula: Cu6(Cu4C2+2)As4S12S
Reference: U.S. Geological Survey (2005) Mineral Resources Data System: U.S. Geological Survey, Reston, Virginia.
β“˜ 'Tetrahedrite Subgroup'
Formula: Cu6(Cu4C2+2)Sb4S12S
Reference: U.S. Geological Survey (2005) Mineral Resources Data System: U.S. Geological Survey, Reston, Virginia.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
β“˜Gold1.AA.05Au
Group 2 - Sulphides and Sulfosalts
β“˜Bismuthinite2.DB.05Bi2S3
β“˜Calaverite2.EA.10AuTe2
β“˜Chalcopyrite2.CB.10aCuFeS2
β“˜Famatinite2.KA.10Cu3SbS4
β“˜Galena2.CD.10PbS
β“˜Hessite2.BA.60Ag2Te
β“˜Petzite2.BA.75Ag3AuTe2
β“˜Pyrite2.EB.05aFeS2
β“˜Sphalerite2.CB.05aZnS
β“˜Sylvanite2.EA.05AgAuTe4
β“˜'Tennantite Subgroup'2.GB.05Cu6(Cu4C2+2)As4S12S
β“˜'Tetrahedrite Subgroup'2.GB.05Cu6(Cu4C2+2)Sb4S12S
Group 4 - Oxides and Hydroxides
β“˜Quartz4.DA.05SiO2
β“˜var. Jasper4.DA.05SiO2
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
β“˜Gypsum7.CD.40CaSO4 Β· 2H2O
Group 9 - Silicates
β“˜Halloysite9.ED.10Al2(Si2O5)(OH)4
Unclassified Minerals, Rocks, etc.
β“˜'Limonite'-

List of minerals for each chemical element

HHydrogen
Hβ“˜ GypsumCaSO4 · 2H2O
Hβ“˜ HalloysiteAl2(Si2O5)(OH)4
OOxygen
Oβ“˜ GypsumCaSO4 · 2H2O
Oβ“˜ HalloysiteAl2(Si2O5)(OH)4
Oβ“˜ QuartzSiO2
AlAluminium
Alβ“˜ HalloysiteAl2(Si2O5)(OH)4
SiSilicon
Siβ“˜ HalloysiteAl2(Si2O5)(OH)4
Siβ“˜ QuartzSiO2
SSulfur
Sβ“˜ BismuthiniteBi2S3
Sβ“˜ ChalcopyriteCuFeS2
Sβ“˜ FamatiniteCu3SbS4
Sβ“˜ GalenaPbS
Sβ“˜ GypsumCaSO4 · 2H2O
Sβ“˜ PyriteFeS2
Sβ“˜ SphaleriteZnS
Sβ“˜ Tennantite SubgroupCu6(Cu4C22+)As4S12S
Sβ“˜ Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
CaCalcium
Caβ“˜ GypsumCaSO4 · 2H2O
FeIron
Feβ“˜ ChalcopyriteCuFeS2
Feβ“˜ PyriteFeS2
CuCopper
Cuβ“˜ ChalcopyriteCuFeS2
Cuβ“˜ FamatiniteCu3SbS4
Cuβ“˜ Tennantite SubgroupCu6(Cu4C22+)As4S12S
Cuβ“˜ Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
ZnZinc
Znβ“˜ SphaleriteZnS
AsArsenic
Asβ“˜ Tennantite SubgroupCu6(Cu4C22+)As4S12S
AgSilver
Agβ“˜ HessiteAg2Te
Agβ“˜ PetziteAg3AuTe2
Agβ“˜ SylvaniteAgAuTe4
SbAntimony
Sbβ“˜ FamatiniteCu3SbS4
Sbβ“˜ Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
TeTellurium
Teβ“˜ CalaveriteAuTe2
Teβ“˜ HessiteAg2Te
Teβ“˜ PetziteAg3AuTe2
Teβ“˜ SylvaniteAgAuTe4
AuGold
Auβ“˜ CalaveriteAuTe2
Auβ“˜ GoldAu
Auβ“˜ PetziteAg3AuTe2
Auβ“˜ SylvaniteAgAuTe4
PbLead
Pbβ“˜ GalenaPbS
BiBismuth
Biβ“˜ BismuthiniteBi2S3

References

Sort by

Year (asc) Year (desc) Author (A-Z) Author (Z-A)
In Nevada. U.S. Geol. Surv. Prof. Paper 700-c, (1970),
78, (1972), 80 Pp.
Geol. and Bull. Soc. Econ. Geol., V. 67, (1972), P.1002.
In Central Nevada. Nv Bureau of Mines and Geol. Rep. 19, (1974),
Field Studies Map Mf-681, (1975), Scale 1:24,000
And Geol. Rep. 33, (1979), Pp. 77-86.
Paper 843-b, (1976), 17 Pp.
Geol., V. 71, (1976), Pp. 904-924.
Mar. 25-28, (1984), Pp. Ft4 1-27.
Mar. 25-28, (1984), Pp. Ft3 1-31.
Volume 72. No. 5, (1964), Pp. 564-579.
Geol. and Bull. Soc. Econ. Geol., V. 66, (1971),
Geol. Surv. Prof. Paper (1124)-c, 1979, Pp. C1-c5.
V. 7, No. 3, (1983), P. 18.
Paper 66, (1909), 258 Pp.
V. 65, No. 3, (1970), Pp. 352-354. 628. Silberman, M. L., B.
No. 5, (1974), Pp. 646-656.
Rep. 19, (1974), Pp. 67-72.
Las Vegas Nv, Feb. (1976). Soc. Min. Eng. Pre-
No. 6, (1973), Pp. 747-764.
Memoir 77, (1960), 117 Pp.
Calendar Year (1987). Nv Division of Mine Inspection,
May (1988).
National Assessment, (1995), U.S. Deposit Data Base, #124.

Other Databases

Link to USGS MRDS:10173919


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