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Erickson Mining District, Utah, USAi
Regional Level Types
Erickson Mining DistrictMining District
UtahState
USACountry

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Mindat Locality ID:
37509
Long-form identifier:
mindat:1:2:37509:5
GUID (UUID V4):
0
Other/historical names associated with this locality:
Black Crook Mining District; Indian Springs


The Erickson (Indian Spring) mining district covers the southern and western Simpson Mountains of southern Tooele County about 32 mi west of Eureka. The district was organized in 1894 and became a modest Mn-Pb-Ag-Zn producer. Total district metal production at modern metal prices is estimated at $3.8 million. The Erickson district is the third largest Mn producer in Utah. The Bar X mine is probably the largest producer.
The Simpson Mountains are a small desert mountain range in the Basin and Range Province of western Utah. The range is composed of three structural blocks: (1) a northern block composed of Proterozoic and Lower Cambrian clastic meta- sedimentary rocks; (2) a central, easterly trending graben of Paleozoic sedimentary rocks; (3) and a southern block of folded Proterozoic clastic meta-sedimentary rocks. Mineralization is confined to the two southern blocks. The mineralization in the central graben is dominantly gently-dipping, epithermal Ag-Au veins (USGS Model 25c) with pyrite-tetrahedrite-chalcopyrite that constitute a small percentage of the district’s overall production (Thomas, 1958).
Mineralization in the southern block consists of Mn-Pb-Zn-Ag polymetallic veins (USGS Model 22c) in Neoproterozoic quartzites, metaconglomerates, and shales. These metasedimentary rocks are broadly folded into a large northerly trending and plunging anticline centered on Death Canyon. Locally these veins have strongly anomalous Mo and Sn. The southern block also has some small, Miocene-age high-silica rhyolitic intrusive bodies (~16 Ma).
The southern Erickson district mineralization occurs primarily as veins occupying northwesterly and easterly trending fault zones. The northwest-trending faults show greater brecciation and throw (Fry and Wilson, 1949). Mineralization is predominantly Pb-Zn-Ag in the middle reaches of Death Canyon near the Bar X mine, and Mn becomes more dominant in the mines/prospects to the north and east. The veins, generally south and west of the Bar X, have strongly anomalous Mo (1000 ppm), Sn (200 ppm), and weakly anomalous Cu in U.S. Geological Survey National Geochemical Database samples.

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Standard Detailed Gallery Strunz Chemical Elements

Commodity List

This is a list of exploitable or exploited mineral commodities recorded from this region.


Mineral List

Mineral list contains entries from the region specified including sub-localities

15 valid minerals.

Rock Types Recorded

Note: data is currently VERY limited. Please bear with us while we work towards adding this information!

Rock list contains entries from the region specified including sub-localities

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Alphabetical List Tree Diagram

Detailed Mineral List:

Chalcopyrite
Formula: CuFeS2
Chrysocolla
Formula: Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Dolomite
Formula: CaMg(CO3)2
Galena
Formula: PbS
Hematite
Formula: Fe2O3
Hemimorphite
Formula: Zn4Si2O7(OH)2 · H2O
Jarosite
Formula: KFe3+3(SO4)2(OH)6
'Limonite'
Localities: Reported from at least 6 localities in this region.
Malachite
Formula: Cu2(CO3)(OH)2
Native Silver
Formula: Ag
Pyrite
Formula: FeS2
Localities: Reported from at least 6 localities in this region.
Quartz
Formula: SiO2
Rhodochrosite
Formula: MnCO3
Rhodonite
Formula: CaMn3Mn[Si5O15]
Smithsonite
Formula: ZnCO3
Sphalerite
Formula: ZnS
'Tetrahedrite Subgroup'
Formula: Cu6(Cu4C2+2)Sb4S12S

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
Native Silver1.AA.05Ag
Group 2 - Sulphides and Sulfosalts
Sphalerite2.CB.05aZnS
Chalcopyrite2.CB.10aCuFeS2
Galena2.CD.10PbS
Pyrite2.EB.05aFeS2
'Tetrahedrite Subgroup'2.GB.05Cu6(Cu4C2+2)Sb4S12S
Group 4 - Oxides and Hydroxides
Hematite4.CB.05Fe2O3
Quartz4.DA.05SiO2
Group 5 - Nitrates and Carbonates
Rhodochrosite5.AB.05MnCO3
Smithsonite5.AB.05ZnCO3
Dolomite5.AB.10CaMg(CO3)2
Malachite5.BA.10Cu2(CO3)(OH)2
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
Jarosite7.BC.10KFe3+3(SO4)2(OH)6
Group 9 - Silicates
Hemimorphite9.BD.10Zn4Si2O7(OH)2 · H2O
Rhodonite9.DK.05CaMn3Mn[Si5O15]
Chrysocolla9.ED.20Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Unclassified
'Limonite'-

List of minerals for each chemical element

HHydrogen
H ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
H HemimorphiteZn4Si2O7(OH)2 · H2O
H JarositeKFe33+(SO4)2(OH)6
H MalachiteCu2(CO3)(OH)2
CCarbon
C DolomiteCaMg(CO3)2
C MalachiteCu2(CO3)(OH)2
C RhodochrositeMnCO3
C SmithsoniteZnCO3
OOxygen
O ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
O DolomiteCaMg(CO3)2
O HematiteFe2O3
O HemimorphiteZn4Si2O7(OH)2 · H2O
O JarositeKFe33+(SO4)2(OH)6
O MalachiteCu2(CO3)(OH)2
O QuartzSiO2
O RhodochrositeMnCO3
O RhodoniteCaMn3Mn[Si5O15]
O SmithsoniteZnCO3
MgMagnesium
Mg DolomiteCaMg(CO3)2
AlAluminium
Al ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
SiSilicon
Si ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Si HemimorphiteZn4Si2O7(OH)2 · H2O
Si QuartzSiO2
Si RhodoniteCaMn3Mn[Si5O15]
SSulfur
S ChalcopyriteCuFeS2
S GalenaPbS
S JarositeKFe33+(SO4)2(OH)6
S PyriteFeS2
S SphaleriteZnS
S Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
KPotassium
K JarositeKFe33+(SO4)2(OH)6
CaCalcium
Ca DolomiteCaMg(CO3)2
Ca RhodoniteCaMn3Mn[Si5O15]
MnManganese
Mn RhodochrositeMnCO3
Mn RhodoniteCaMn3Mn[Si5O15]
FeIron
Fe ChalcopyriteCuFeS2
Fe HematiteFe2O3
Fe JarositeKFe33+(SO4)2(OH)6
Fe PyriteFeS2
CuCopper
Cu ChalcopyriteCuFeS2
Cu ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Cu MalachiteCu2(CO3)(OH)2
Cu Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
ZnZinc
Zn HemimorphiteZn4Si2O7(OH)2 · H2O
Zn SmithsoniteZnCO3
Zn SphaleriteZnS
AgSilver
Ag Native SilverAg
SbAntimony
Sb Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
PbLead
Pb GalenaPbS

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