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Big Mike Mine, Tobin and Sonoma Range Mining District, Pershing County, Nevada, USAi
Regional Level Types
Big Mike MineMine
Tobin and Sonoma Range Mining DistrictMining District
Pershing CountyCounty
NevadaState
USACountry

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Latitude & Longitude (WGS84):
40° 32' 31'' North , 117° 33' 24'' West
Latitude & Longitude (decimal):
Type:
Nearest Settlements:
PlacePopulationDistance
Golconda214 (2011)46.0km
Winnemucca7,887 (2017)50.2km
Mindat Locality ID:
58783
Long-form identifier:
mindat:1:2:58783:0
GUID (UUID V4):
0


Sec 23 T31N R39E.
Volcanogenic massive sulfide deposit.
Discovered in the 1930s, mining was done from the late 1960s to the 1970s.

Commodity: Ore Materials: chalcopyrite, bornite, digenite, tenorite, cuprite, sphalerite; Gangue Materials: pyrite, iron oxide

Deposit: Big Mike is a high-grade, low tonnage, cupriferous pyrite volcanogenic stratiform massive sulfide deposit. It consists of a massive lens that occurs entirely within a thin cherty carbonaceous argillite. A stringer zone occurs in the footwall pillow basalt, and a minor stringer zone occurs north of the massive lens in the hanging wall pillow basalt. Much of the dump material and pit wall consists of pillow lava, chert, and argillite with varying amounts of limonite gossan and oxide copper minerals. The main deposit is volcanogenic massive sulfide of the hot springs type, which occurs in the Havallah sequence. This is a thick greenstone complex in the Pumpernickel formation. When discovered, the deposit consisted of a secondarily enriched pod of nearly massive copper and iron sulfides enveloped by altered rock containing zones and disseminations of secondary copper mineralization. The mineralogy is complex, as various secondary effects are apparent. The structure of the area is also complex, though the deformation of the Big Mike area is not so severe as other parts of the Havallah sequence. A shear zone runs through the Big Mike pit and extends approximately 1,000 feet in the southeast and northwest directions away from the pit. This is also the general strike of the area with dips 40 to 60 degrees to the northeast. This shear zone may be an indicator of further deposits. Five target areas have been identified for additional exploration on and adjacent to the Big Mike property. These targets show potential to extend the existing ore zone and for additional ore bodies.

Deposit type: Massive sulfide, Cyprus

Development: Copper occurrences were known in the area at about the turn of the last century. The project area was claimed in the early 1900s by the Foster family, but very little exploration was done and no development work was done. In 1966, Mr. Clair Chamberlain optioned the property and undertook a sampling program. As a result of the sampling, some copper oxide ore was shipped to ASARCO in Tacoma, Washington. From this work the Big Mike Corporation was formed to develop and exploit the copper oxide ore by heap leaching. A small pad was developed, and copper precipitate was produced. In 1967, the Big Mike Corporation entered into a joint venture with Cerro Corporation to explore the property further, and this led to the discovery of a high-grade copper sulfide ore body. By 1970, Ranchers Exploration and Development Corporation acquired the property from Cerro Corporation and confirmed the sulfide orebody, which was rapidly developed via an open pit. In fact, all the high-grade ore was mined and directly shipped to smelters in 1970. The remaining oxide ore and the mixed and low-grade sulfide ore were crushed for heap leaching. In the pit, similar low-grade ore was blasted from the walls of the pit for leaching in the bottom of the pit. Heap leaching was carried out during two periods, from 1971 to 1974 and then 1978 to 1979. Both periods were curtailed by low copper prices. In 1979, Ranchers abandoned the claims. The claims were subsequently staked and reclaimed by WR & A. Big Mike Limited Partnership (BMLP) purchased the claims from WR & A. in 1988. During the period from 1988 to 1992, BMLP undertook project studies to establish reserves, identify a treatment method, and gain environmental permits to develop the project. A considerable amount of work was done, but the project did not get underway. John Cook and Dan Mackie examined data from the project in the spring of 1997 and concluded that it would be suitable for continuous vat leaching with the EcoVat. After this work an option agreement was entered into. GoldSpring, Inc. acquired 100% of this project. The current Big Mike project is an oxide copper recovery project with the copper oxides remaining from a previous rich sulfide operation. The property also has exploration potential for further copper oxides and copper sulfides. In 2005, GoldSpring Inc. signed a memorandum of understanding with MBMI Resources Inc. to acquire a 50% interest in the 310-acre Big Mike copper property located 32 miles south of Winnemucca. Big Mike is a volcanogenic massive sulfide deposit that consists of a secondarily enriched pod of massive copper and iron sulfides enveloped by altered rock containing zones and disseminations of secondary copper mineralization. Ranchers Exploration and Development Co. produced 25 million pounds of copper from direct-shipping, high-grade copper sulfide ore from this property in 1970. Five target areas have been identified for additional exploration on and adjacent to the Big Mike property.

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


29 valid minerals. 1 (TL) - type locality of valid minerals.

Rock Types Recorded


Select Rock List Type

Alphabetical List Tree Diagram

Detailed Mineral List:

Alpersite (TL)
Formula: (Mg,Cu2+)(H2O)6(SO4) · H2O
Type Locality:
Alunogen
Formula: Al2(SO4)3 · 17H2O
Antlerite
Formula: Cu3(SO4)(OH)4
Baryte
Formula: BaSO4
Bornite
Formula: Cu5FeS4
Calcite
Formula: CaCO3
Chalcocite
Formula: Cu2S
Chalcopyrite
Formula: CuFeS2
'Chlorite Group'
Chrysocolla
Formula: Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Covellite
Formula: CuS
Cuprite
Formula: Cu2O
Digenite
Formula: Cu9S5
Djurleite
Formula: Cu31S16
Epsomite
Formula: MgSO4 · 7H2O
Goethite
Formula: Fe3+O(OH)
Graphite
Formula: C
Gypsum
Formula: CaSO4 · 2H2O
Hematite
Formula: Fe2O3
Heterogenite
Formula: Co3+O(OH)
Jarosite
Formula: KFe3+3(SO4)2(OH)6
'Limonite'
Malachite
Formula: Cu2(CO3)(OH)2
Muscovite
Formula: KAl2(AlSi3O10)(OH)2
Muscovite var. Sericite
Formula: KAl2(AlSi3O10)(OH)2
Native Copper
Formula: Cu
Native Gold
Formula: Au
Pickeringite
Formula: MgAl2(SO4)4 · 22H2O
Pyrite
Formula: FeS2
Quartz
Formula: SiO2
Sphalerite
Formula: ZnS
Tenorite
Formula: CuO

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
Native Copper1.AA.05Cu
Native Gold1.AA.05Au
Graphite1.CB.05aC
Group 2 - Sulphides and Sulfosalts
Chalcocite2.BA.05Cu2S
Djurleite2.BA.05Cu31S16
Digenite2.BA.10Cu9S5
Bornite2.BA.15Cu5FeS4
Covellite2.CA.05aCuS
Sphalerite2.CB.05aZnS
Chalcopyrite2.CB.10aCuFeS2
Pyrite2.EB.05aFeS2
Group 4 - Oxides and Hydroxides
Cuprite4.AA.10Cu2O
Tenorite4.AB.10CuO
Hematite4.CB.05Fe2O3
Quartz4.DA.05SiO2
Goethite4.FD.10Fe3+O(OH)
Heterogenite4.FE.20Co3+O(OH)
Group 5 - Nitrates and Carbonates
Calcite5.AB.05CaCO3
Malachite5.BA.10Cu2(CO3)(OH)2
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
Baryte7.AD.35BaSO4
Antlerite7.BB.15Cu3(SO4)(OH)4
Jarosite7.BC.10KFe3+3(SO4)2(OH)6
Alpersite (TL)7.CB.35(Mg,Cu2+)(H2O)6(SO4) · H2O
Epsomite7.CB.40MgSO4 · 7H2O
Alunogen7.CB.45Al2(SO4)3 · 17H2O
Pickeringite7.CB.85MgAl2(SO4)4 · 22H2O
Gypsum7.CD.40CaSO4 · 2H2O
Group 9 - Silicates
Muscovite9.EC.15KAl2(AlSi3O10)(OH)2
var. Sericite9.EC.15KAl2(AlSi3O10)(OH)2
Chrysocolla9.ED.20Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Unclassified
'Chlorite Group'-
'Limonite'-

List of minerals for each chemical element

HHydrogen
H AlunogenAl2(SO4)3 · 17H2O
H AntleriteCu3(SO4)(OH)4
H ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
H EpsomiteMgSO4 · 7H2O
H GoethiteFe3+O(OH)
H GypsumCaSO4 · 2H2O
H HeterogeniteCo3+O(OH)
H JarositeKFe33+(SO4)2(OH)6
H MalachiteCu2(CO3)(OH)2
H MuscoviteKAl2(AlSi3O10)(OH)2
H PickeringiteMgAl2(SO4)4 · 22H2O
H Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
H Alpersite(Mg,Cu2+)(H2O)6(SO4) · H2O
CCarbon
C CalciteCaCO3
C GraphiteC
C MalachiteCu2(CO3)(OH)2
OOxygen
O AlunogenAl2(SO4)3 · 17H2O
O AntleriteCu3(SO4)(OH)4
O BaryteBaSO4
O CalciteCaCO3
O ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
O CupriteCu2O
O EpsomiteMgSO4 · 7H2O
O GoethiteFe3+O(OH)
O GypsumCaSO4 · 2H2O
O HematiteFe2O3
O HeterogeniteCo3+O(OH)
O JarositeKFe33+(SO4)2(OH)6
O MalachiteCu2(CO3)(OH)2
O MuscoviteKAl2(AlSi3O10)(OH)2
O PickeringiteMgAl2(SO4)4 · 22H2O
O QuartzSiO2
O TenoriteCuO
O Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
O Alpersite(Mg,Cu2+)(H2O)6(SO4) · H2O
MgMagnesium
Mg EpsomiteMgSO4 · 7H2O
Mg PickeringiteMgAl2(SO4)4 · 22H2O
Mg Alpersite(Mg,Cu2+)(H2O)6(SO4) · H2O
AlAluminium
Al AlunogenAl2(SO4)3 · 17H2O
Al ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Al MuscoviteKAl2(AlSi3O10)(OH)2
Al PickeringiteMgAl2(SO4)4 · 22H2O
Al Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
SiSilicon
Si ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Si MuscoviteKAl2(AlSi3O10)(OH)2
Si QuartzSiO2
Si Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
SSulfur
S AlunogenAl2(SO4)3 · 17H2O
S AntleriteCu3(SO4)(OH)4
S BaryteBaSO4
S BorniteCu5FeS4
S ChalcopyriteCuFeS2
S ChalcociteCu2S
S CovelliteCuS
S DigeniteCu9S5
S DjurleiteCu31S16
S EpsomiteMgSO4 · 7H2O
S GypsumCaSO4 · 2H2O
S JarositeKFe33+(SO4)2(OH)6
S PickeringiteMgAl2(SO4)4 · 22H2O
S PyriteFeS2
S SphaleriteZnS
S Alpersite(Mg,Cu2+)(H2O)6(SO4) · H2O
KPotassium
K JarositeKFe33+(SO4)2(OH)6
K MuscoviteKAl2(AlSi3O10)(OH)2
K Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
CaCalcium
Ca CalciteCaCO3
Ca GypsumCaSO4 · 2H2O
FeIron
Fe BorniteCu5FeS4
Fe ChalcopyriteCuFeS2
Fe GoethiteFe3+O(OH)
Fe HematiteFe2O3
Fe JarositeKFe33+(SO4)2(OH)6
Fe PyriteFeS2
CoCobalt
Co HeterogeniteCo3+O(OH)
CuCopper
Cu AntleriteCu3(SO4)(OH)4
Cu BorniteCu5FeS4
Cu ChalcopyriteCuFeS2
Cu ChalcociteCu2S
Cu ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Cu CovelliteCuS
Cu CupriteCu2O
Cu Native CopperCu
Cu DigeniteCu9S5
Cu DjurleiteCu31S16
Cu MalachiteCu2(CO3)(OH)2
Cu TenoriteCuO
Cu Alpersite(Mg,Cu2+)(H2O)6(SO4) · H2O
ZnZinc
Zn SphaleriteZnS
BaBarium
Ba BaryteBaSO4
AuGold
Au Native GoldAu

Other Databases

Link to USGS MRDS:10310578

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