Free Coinage Mining District, Stansbury Mountains, Tooele County, Utah, USAi
Regional Level Types | |
---|---|
Free Coinage Mining District | Mining District (Abandoned) |
Stansbury Mountains | Mountain Range |
Tooele County | County |
Utah | State |
USA | Country |
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Type:
Mining District (Abandoned) - last checked 2021
Deposit first discovered:
1895
Mindat Locality ID:
37468
Long-form identifier:
mindat:1:2:37468:9
GUID (UUID V4):
ec359709-e9d3-424d-87a4-4f3f2020c6be
Other/historical names associated with this locality:
Timpie Canyon Mining District
The Free Coinage (Timpie Canyon) district is in the northern Stansbury Mountains in northeastern Tooele County, about 17 mi northwest of Tooele. The district is a small Pb-Ag producer organized in 1895 and operated sporadically from 1917 into the 1970s. Total district metal production at modern metal prices is estimated at $556,000. The Monte Carlo and Utah Bunker Hill underground mines in the upper reaches of Miners Canyon were the largest operations (Stein and others, 1989).
The Free Coinage district is situated on the north flank of the BinghamβPark City mineral belt in the Basin and Range Province of northwestern Utah. The district lies on the east limb of the north-northeast-trending Deseret anticline. An Eocene-age monzonite porphyry dike is present in the southeastern part of the district. The polymetallic vein and replacement deposits are hosted by faulted Lower Mississippian carbonates, particularly the Gardison Limestone (Rigby, 1958). In addition to Pb-Zn-Ag, the replacement ores may be anomalous in As, Au, Cd, and Cu (USGS Model 19a).
Furthermore, a small quantity of cinnabar was reportedly mined in the 1950s from the Halladay Hg property south of Timpie Valley. The unusual coarse-grained cinnabar occurs as stringers along a fault breccia in nearly vertical, north-striking, Lower Mississippian Gardison Limestone (Rigby, 1958). Limited geochemistry suggests that the Hg ore has associated Ag, As, Au, Cu, Pb, Sb, and Zn.
The most economically important mining operations in the district are industrial mineral quarries that produced substantial quantities of limestone and dolomite (USGS Model 32g) for lime production, for use as flux in Cu smelting, and for cement raw material (Tripp and others, 1989).
The Free Coinage district is situated on the north flank of the BinghamβPark City mineral belt in the Basin and Range Province of northwestern Utah. The district lies on the east limb of the north-northeast-trending Deseret anticline. An Eocene-age monzonite porphyry dike is present in the southeastern part of the district. The polymetallic vein and replacement deposits are hosted by faulted Lower Mississippian carbonates, particularly the Gardison Limestone (Rigby, 1958). In addition to Pb-Zn-Ag, the replacement ores may be anomalous in As, Au, Cd, and Cu (USGS Model 19a).
Furthermore, a small quantity of cinnabar was reportedly mined in the 1950s from the Halladay Hg property south of Timpie Valley. The unusual coarse-grained cinnabar occurs as stringers along a fault breccia in nearly vertical, north-striking, Lower Mississippian Gardison Limestone (Rigby, 1958). Limited geochemistry suggests that the Hg ore has associated Ag, As, Au, Cu, Pb, Sb, and Zn.
The most economically important mining operations in the district are industrial mineral quarries that produced substantial quantities of limestone and dolomite (USGS Model 32g) for lime production, for use as flux in Cu smelting, and for cement raw material (Tripp and others, 1989).
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Standard Detailed Gallery Strunz Chemical ElementsCommodity 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-localities17 valid minerals.
Rock Types Recorded
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Alphabetical List Tree DiagramDetailed Mineral List:
Gallery:
List of minerals arranged by Strunz 10th Edition classification
Group 1 - Elements | |||
---|---|---|---|
β | Gold | 1.AA.05 | Au |
Group 2 - Sulphides and Sulfosalts | |||
β | Metacinnabar | 2.CB.05a | HgS |
β | Galena | 2.CD.10 | PbS |
β | Cinnabar | 2.CD.15a | HgS |
β | Pyrite | 2.EB.05a | FeS2 |
β | 'Tetrahedrite Subgroup' | 2.GB.05 | Cu6(Cu4C2+2)Sb4S12S |
Group 4 - Oxides and Hydroxides | |||
β | Goethite | 4.00. | Ξ±-Fe3+O(OH) |
β | Quartz | 4.DA.05 | SiO2 |
Group 5 - Nitrates and Carbonates | |||
β | Calcite | 5.AB.05 | CaCO3 |
β | Smithsonite | 5.AB.05 | ZnCO3 |
β | Dolomite | 5.AB.10 | CaMg(CO3)2 |
β | Cerussite | 5.AB.15 | PbCO3 |
β | Malachite | 5.BA.10 | Cu2(CO3)(OH)2 |
Group 7 - Sulphates, Chromates, Molybdates and Tungstates | |||
β | Anglesite | 7.AD.35 | PbSO4 |
β | Jarosite | 7.BC.10 | KFe3+3(SO4)2(OH)6 |
β | Plumbojarosite | 7.BC.10 | Pb0.5Fe3+3(SO4)2(OH)6 |
Group 9 - Silicates | |||
β | Chrysocolla | 9.ED.20 | Cu2-xAlx(H2-xSi2O5)(OH)4 Β· nH2O, x < 1 |
β | Anorthite var. Labradorite | 9.FA.35 | (Ca,Na)[Al(Al,Si)Si2O8] |
β | 9.FA.35 | Ca(Al2Si2O8) | |
Unclassified | |||
β | 'Limonite' | - | |
β | 'Fayalite-Forsterite Series' | - |
List of minerals for each chemical element
H | Hydrogen | |
---|---|---|
H | β Chrysocolla | Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1 |
H | β Goethite | Ξ±-Fe3+O(OH) |
H | β Jarosite | KFe33+(SO4)2(OH)6 |
H | β Malachite | Cu2(CO3)(OH)2 |
H | β Plumbojarosite | Pb0.5Fe33+(SO4)2(OH)6 |
C | Carbon | |
C | β Calcite | CaCO3 |
C | β Cerussite | PbCO3 |
C | β Dolomite | CaMg(CO3)2 |
C | β Malachite | Cu2(CO3)(OH)2 |
C | β Smithsonite | ZnCO3 |
O | Oxygen | |
O | β Anglesite | PbSO4 |
O | β Anorthite | Ca(Al2Si2O8) |
O | β Calcite | CaCO3 |
O | β Cerussite | PbCO3 |
O | β Chrysocolla | Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1 |
O | β Dolomite | CaMg(CO3)2 |
O | β Goethite | Ξ±-Fe3+O(OH) |
O | β Jarosite | KFe33+(SO4)2(OH)6 |
O | β Anorthite var. Labradorite | (Ca,Na)[Al(Al,Si)Si2O8] |
O | β Malachite | Cu2(CO3)(OH)2 |
O | β Plumbojarosite | Pb0.5Fe33+(SO4)2(OH)6 |
O | β Quartz | SiO2 |
O | β Smithsonite | ZnCO3 |
Na | Sodium | |
Na | β Anorthite var. Labradorite | (Ca,Na)[Al(Al,Si)Si2O8] |
Mg | Magnesium | |
Mg | β Dolomite | CaMg(CO3)2 |
Al | Aluminium | |
Al | β Anorthite | Ca(Al2Si2O8) |
Al | β Chrysocolla | Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1 |
Al | β Anorthite var. Labradorite | (Ca,Na)[Al(Al,Si)Si2O8] |
Si | Silicon | |
Si | β Anorthite | Ca(Al2Si2O8) |
Si | β Chrysocolla | Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1 |
Si | β Anorthite var. Labradorite | (Ca,Na)[Al(Al,Si)Si2O8] |
Si | β Quartz | SiO2 |
S | Sulfur | |
S | β Anglesite | PbSO4 |
S | β Cinnabar | HgS |
S | β Galena | PbS |
S | β Jarosite | KFe33+(SO4)2(OH)6 |
S | β Metacinnabar | HgS |
S | β Plumbojarosite | Pb0.5Fe33+(SO4)2(OH)6 |
S | β Pyrite | FeS2 |
S | β Tetrahedrite Subgroup | Cu6(Cu4C22+)Sb4S12S |
K | Potassium | |
K | β Jarosite | KFe33+(SO4)2(OH)6 |
Ca | Calcium | |
Ca | β Anorthite | Ca(Al2Si2O8) |
Ca | β Calcite | CaCO3 |
Ca | β Dolomite | CaMg(CO3)2 |
Ca | β Anorthite var. Labradorite | (Ca,Na)[Al(Al,Si)Si2O8] |
Fe | Iron | |
Fe | β Goethite | Ξ±-Fe3+O(OH) |
Fe | β Jarosite | KFe33+(SO4)2(OH)6 |
Fe | β Plumbojarosite | Pb0.5Fe33+(SO4)2(OH)6 |
Fe | β Pyrite | FeS2 |
Cu | Copper | |
Cu | β Chrysocolla | Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1 |
Cu | β Malachite | Cu2(CO3)(OH)2 |
Cu | β Tetrahedrite Subgroup | Cu6(Cu4C22+)Sb4S12S |
Zn | Zinc | |
Zn | β Smithsonite | ZnCO3 |
Sb | Antimony | |
Sb | β Tetrahedrite Subgroup | Cu6(Cu4C22+)Sb4S12S |
Au | Gold | |
Au | β Gold | Au |
Hg | Mercury | |
Hg | β Cinnabar | HgS |
Hg | β Metacinnabar | HgS |
Pb | Lead | |
Pb | β Anglesite | PbSO4 |
Pb | β Cerussite | PbCO3 |
Pb | β Galena | PbS |
Pb | β Plumbojarosite | Pb0.5Fe33+(SO4)2(OH)6 |
Fossils
This region is too big or complex to display the fossil list, try looking at smaller subregions.Localities in this Region
- Utah
- Tooele County
- Stansbury Mountains
- Tooele County
- Utah
- Tooele County
- Stansbury Mountains
- Free Coinage Mining District
- Stansbury Mountains
- Tooele County
Other Regions, Features and Areas that Intersect
North America PlateTectonic Plate
- Basin and Range BasinsBasin
- Mojave DomainDomain
- Oquirrh BasinBasin
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