North Tintic Mining District, Utah County, Utah, USAi
Regional Level Types | |
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North Tintic Mining District | Mining District |
Utah County | County |
Utah | State |
USA | Country |
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Type:
Mindat Locality ID:
417963
Long-form identifier:
mindat:1:2:417963:7
GUID (UUID V4):
7e7ad6c1-814a-4dc1-a48b-3eb5aae9b310
The North Tintic district lies north of the much larger Main and East Tintic districts of the greater Tintic district in the East Tintic Mountains of southeastern Tooele County. The North Tintic district is a geographically large, but modest Zn-Pb producer. Total district metal production at modern metal prices is estimated at $34 million. The Scranton underground mine is the only notable producer (Disbrow and Morris, 1957).
The East Tintic Mountains are one of the easternmost ranges in the Basin and Range Province in central Utah. The late Proterozoic- and Paleozoic-age strata of the North Tintic district have been broadly folded about the north-plunging, North Tintic anticline and Tintic syncline, which have been disrupted by numerous northeast-striking, right-lateral, strike-slip faults (Clark and others, 2012). While mineralization in the Main Tintic district to the south appears to be related to Eocene intrusives, Clark and others (2012) report Oligocene ages (29 to 25 Ma) on mafic intrusions and volcanics in the North Tintic district.
North Tintic has the smallest historical production of the four Tintic subdistricts, but, on average has the highest Zn ore grades (Krahulec and Briggs, 2006). The North Tintic district also has several Mn deposits. The Scranton mine, by far the largest operation in the North Tintic district, developed Zn-Pb mantos hosted in the Mississippian-age carbonate section. Average grades at the Scranton are 16.7% Zn, 9.5% Pb, 23.7 ppm Ag, and some minor Cu and Au which may not have been recovered (Disbrow and Morris, 1957). Nearly all historical production was derived from oxidized ores.
The East Tintic Mountains are one of the easternmost ranges in the Basin and Range Province in central Utah. The late Proterozoic- and Paleozoic-age strata of the North Tintic district have been broadly folded about the north-plunging, North Tintic anticline and Tintic syncline, which have been disrupted by numerous northeast-striking, right-lateral, strike-slip faults (Clark and others, 2012). While mineralization in the Main Tintic district to the south appears to be related to Eocene intrusives, Clark and others (2012) report Oligocene ages (29 to 25 Ma) on mafic intrusions and volcanics in the North Tintic district.
North Tintic has the smallest historical production of the four Tintic subdistricts, but, on average has the highest Zn ore grades (Krahulec and Briggs, 2006). The North Tintic district also has several Mn deposits. The Scranton mine, by far the largest operation in the North Tintic district, developed Zn-Pb mantos hosted in the Mississippian-age carbonate section. Average grades at the Scranton are 16.7% Zn, 9.5% Pb, 23.7 ppm Ag, and some minor Cu and Au which may not have been recovered (Disbrow and Morris, 1957). Nearly all historical production was derived from oxidized ores.
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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-localities19 valid minerals.
Rock Types Recorded
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Rock list contains entries from the region specified including sub-localities
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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 | Galena | 2.CD.10 | PbS |
β | Pyrite | 2.EB.05a | FeS2 |
Group 3 - Halides | |||
β | Fluorite | 3.AB.25 | CaF2 |
Group 4 - Oxides and Hydroxides | |||
β | Hematite | 4.CB.05 | Fe2O3 |
β | Quartz | 4.DA.05 | SiO2 |
β | Pyrolusite | 4.DB.05 | Mn4+O2 |
β | Diaspore | 4.FD.10 | AlO(OH) |
Group 5 - Nitrates and Carbonates | |||
β | Calcite | 5.AB.05 | CaCO3 |
β | Dolomite | 5.AB.10 | CaMg(CO3)2 |
β | Cerussite | 5.AB.15 | PbCO3 |
β | Aragonite | 5.AB.15 | CaCO3 |
Group 7 - Sulphates, Chromates, Molybdates and Tungstates | |||
β | Anglesite | 7.AD.35 | PbSO4 |
Group 8 - Phosphates, Arsenates and Vanadates | |||
β | Fluellite | 8.DE.10 | Al2(PO4)F2(OH) Β· 7H2O |
Group 9 - Silicates | |||
β | Zunyite | 9.BJ.55 | Al13Si5O20(OH,F)18Cl |
β | Muscovite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
β | var. Sericite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
β | Montmorillonite | 9.EC.40 | (Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 Β· nH2O |
β | Kaolinite | 9.ED.05 | Al2(Si2O5)(OH)4 |
β | Halloysite | 9.ED.10 | Al2(Si2O5)(OH)4 |
Unclassified | |||
β | 'Limonite' | - | |
β | 'Jasper' | - |
List of minerals for each chemical element
H | Hydrogen | |
---|---|---|
H | β Diaspore | AlO(OH) |
H | β Fluellite | Al2(PO4)F2(OH) · 7H2O |
H | β Halloysite | Al2(Si2O5)(OH)4 |
H | β Kaolinite | Al2(Si2O5)(OH)4 |
H | β Muscovite | KAl2(AlSi3O10)(OH)2 |
H | β Montmorillonite | (Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O |
H | β Zunyite | Al13Si5O20(OH,F)18Cl |
H | β Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
C | Carbon | |
C | β Aragonite | CaCO3 |
C | β Calcite | CaCO3 |
C | β Cerussite | PbCO3 |
C | β Dolomite | CaMg(CO3)2 |
O | Oxygen | |
O | β Anglesite | PbSO4 |
O | β Aragonite | CaCO3 |
O | β Calcite | CaCO3 |
O | β Cerussite | PbCO3 |
O | β Diaspore | AlO(OH) |
O | β Dolomite | CaMg(CO3)2 |
O | β Fluellite | Al2(PO4)F2(OH) · 7H2O |
O | β Halloysite | Al2(Si2O5)(OH)4 |
O | β Hematite | Fe2O3 |
O | β Kaolinite | Al2(Si2O5)(OH)4 |
O | β Muscovite | KAl2(AlSi3O10)(OH)2 |
O | β Montmorillonite | (Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O |
O | β Pyrolusite | Mn4+O2 |
O | β Quartz | SiO2 |
O | β Zunyite | Al13Si5O20(OH,F)18Cl |
O | β Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
F | Fluorine | |
F | β Fluellite | Al2(PO4)F2(OH) · 7H2O |
F | β Fluorite | CaF2 |
F | β Zunyite | Al13Si5O20(OH,F)18Cl |
Na | Sodium | |
Na | β Montmorillonite | (Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O |
Mg | Magnesium | |
Mg | β Dolomite | CaMg(CO3)2 |
Mg | β Montmorillonite | (Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O |
Al | Aluminium | |
Al | β Diaspore | AlO(OH) |
Al | β Fluellite | Al2(PO4)F2(OH) · 7H2O |
Al | β Halloysite | Al2(Si2O5)(OH)4 |
Al | β Kaolinite | Al2(Si2O5)(OH)4 |
Al | β Muscovite | KAl2(AlSi3O10)(OH)2 |
Al | β Montmorillonite | (Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O |
Al | β Zunyite | Al13Si5O20(OH,F)18Cl |
Al | β Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
Si | Silicon | |
Si | β Halloysite | Al2(Si2O5)(OH)4 |
Si | β Kaolinite | Al2(Si2O5)(OH)4 |
Si | β Muscovite | KAl2(AlSi3O10)(OH)2 |
Si | β Montmorillonite | (Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O |
Si | β Quartz | SiO2 |
Si | β Zunyite | Al13Si5O20(OH,F)18Cl |
Si | β Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
P | Phosphorus | |
P | β Fluellite | Al2(PO4)F2(OH) · 7H2O |
S | Sulfur | |
S | β Anglesite | PbSO4 |
S | β Galena | PbS |
S | β Pyrite | FeS2 |
Cl | Chlorine | |
Cl | β Zunyite | Al13Si5O20(OH,F)18Cl |
K | Potassium | |
K | β Muscovite | KAl2(AlSi3O10)(OH)2 |
K | β Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
Ca | Calcium | |
Ca | β Aragonite | CaCO3 |
Ca | β Calcite | CaCO3 |
Ca | β Dolomite | CaMg(CO3)2 |
Ca | β Fluorite | CaF2 |
Ca | β Montmorillonite | (Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O |
Mn | Manganese | |
Mn | β Pyrolusite | Mn4+O2 |
Fe | Iron | |
Fe | β Hematite | Fe2O3 |
Fe | β Pyrite | FeS2 |
Au | Gold | |
Au | β Gold | Au |
Pb | Lead | |
Pb | β Anglesite | PbSO4 |
Pb | β Cerussite | PbCO3 |
Pb | β Galena | PbS |
Fossils
This region is too big or complex to display the fossil list, try looking at smaller subregions.Localities in this Region
- Utah
- Utah County
- North Tintic Mining District
- Albert Claims
- Bingham Mines Company Adits
- Bismark Peak South Prospects
- Bismark Peak SW Prospects
- Black Rock Canyon Pass Prospects
- Bluff Shaft Occurrence
- Central Standard Consol. Mining Company (Copper Leaf Shaft; Central Standard Shaft; Helen Adit; White Star Adit)
- Chief Lime Quarry (Homansville; Saddle Quarry)
- Chiulos Canyon Shale Locality Occurrence
- Copper Leaf Shaft Occurrence
- Deprezin Property
- Drill Holes North of Burgin Occurrence (Kennecott Holes)
- East Standard Prospect
- Eureka Comstock Prospects (North Colorado Shaft)
- Farragut Prospect (Admiral Farragut Claims)
- Fremont Canyon Adits Occurrence (Graphite and Hermione Claims)
- Helen Adits Occurrence
- Homansville Shaft Occurrence
- Hot Stuff Prospect
- Lehi-Tintic Mine (Gold Blossom Mine; Nichols Adit; Lehi Tintic Mining Company)
- M. E. Whitely Shaft Occurrence
- North Tintic Mining District
- Utah County
- Utah
- Utah County
- North Tintic Mining District
- Mary E. Whitely Prospects
- Norman Tintic Group
- North Standard Mine (North Standard Clay Pit)
- Northwest Gardison Ridge Prospects
- Pinyon Queen Shaft Occurrence
- Prospects North of Burgin
- R. G. Wilson Adit Occurrence
- Rattlesnake Canyon Northwest Workings Prospect
- Selma Fault Zone prospects
- Shea Group
- Silver Dollar Mine Prospect
- Silver Shield Shaft Occurrence
- Stroud Prospect
- Swanson Spring Prospect
- Tintic Davis Mining Company Prospects
- Tintic Humbolt Occurrence
- Unidentified Occurrence
- Upper Rattlesnake Canyon Workings Occurrence
- Vanadium Company Spec. Info. Occurrence
- Water Lily Shaft Occurrence (Water Lillie)
- White Star Adit Occurrence
- North Tintic Mining District
- Utah County
Other Regions, Features and Areas that Intersect
North America PlateTectonic Plate
- Basin and Range BasinsBasin
- Mojave DomainDomain
- Oquirrh BasinBasin
USA
- Utah
- East Tintic MountainsMountain Range
- Tintic Mining DistrictMining District
- North Tintic Mining DistrictMining District
- Tintic Mining DistrictMining District
- East Tintic MountainsMountain Range
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Water Lily Shaft Occurrence, North Tintic Mining District, Utah County, Utah, USA