Little Bell Mine (Daly West Group; Park Utah Consolidated Mines; United Park City Mines), Park City Mining District, Summit County, Utah, USAi
| Regional Level Types | |
|---|---|
| Little Bell Mine (Daly West Group; Park Utah Consolidated Mines; United Park City Mines) | Mine |
| Park City Mining District | City |
| Summit County | County |
| Utah | State |
| USA | Country |
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Latitude & Longitude (WGS84):
40° 36' 39'' North , 111° 30' 32'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Park City | 8,128 (2017) | 4.0km |
| Hideout | 718 (2017) | 8.8km |
| Snyderville | 5,612 (2011) | 9.7km |
| Alta | 390 (2017) | 11.2km |
| Midway | 4,646 (2017) | 11.4km |
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
Local clubs are the best way to get access to collecting localities
| Club | Location | Distance |
|---|---|---|
| Rockhounders Outreach for Community Knowledge | Sandy, Utah | 32km |
| Mineral Collectors of Utah | Salt Lake City, Utah | 36km |
| Wasatch Gem Society | Salt Lake City, Utah | 36km |
| Timpanogos Gem & Mineral Society | Provo, Utah | 44km |
Mindat Locality ID:
38746
Long-form identifier:
mindat:1:2:38746:1
GUID (UUID V4):
c8a6f355-1d01-4699-b172-b39b6bdeef6c
Structure: East-West Striking Faults Uinta-Cottonwood Arch, Sevier Overthrust Belt, Park City Anticline
Alteration: Oxidation
Tectonics: Basin And Range - Colorado Plateau Transition Zone, Cordilleran Hinge Line
Deposit: Ore found in three east-west striking fracture zones which dip vertically. The northly zone is nearly barren and the middle zone most productive. The southern zone may merge with the middle zone at depth. Ore was hit at the 300 ft and 500 ft levels. Ore generally occurs along the fault contact between quartzite and limestone amount of ore produced is unreported but said to be relatively small ; info.src : 1 pub lit
Development: Claims located in 1880 and tunnel driven at creek level. In 1901 systematic exploration was begun As the rich daly west and quincy ores were discovered. Little bell shaft was started in 1901. Rich lead ore struck in 1906 and 1909-1910. Ne W discoveries of ore made in 1911-1912. Property consolidated with park utah consolidated mines in 1920 and with united park city mines in 1953
Geology: Bedding dips 20 to 30 degrees to the northwest
Rock formation(s): Weber Quartzite;Park City Formation
Ore(s): East-West Striking Faults
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsCommodity List
This is a list of exploitable or exploited mineral commodities recorded at this locality.Mineral List
10 valid minerals.
Rock Types Recorded
Note: data is currently VERY limited. Please bear with us while we work towards adding this information!
Select Rock List Type
Alphabetical List Tree DiagramDetailed Mineral List:
| ⓘ Anglesite Formula: PbSO4 |
| ⓘ Calcite Formula: CaCO3 |
| ⓘ Cerussite Formula: PbCO3 |
| ⓘ Chrysocolla Formula: Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1 |
| ⓘ Cuprite Formula: Cu2O |
| ⓘ Galena Formula: PbS |
| ⓘ Gold Formula: Au |
| ⓘ Pyrite Formula: FeS2 |
| ⓘ Quartz Formula: SiO2 |
| ⓘ Sphalerite Formula: ZnS |
| ⓘ 'Tetrahedrite Subgroup' Formula: Cu6(Cu4C2+2)Sb4S12S |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 1 - Elements | |||
|---|---|---|---|
| ⓘ | Gold | 1.AA.05 | Au |
| Group 2 - Sulphides and Sulfosalts | |||
| ⓘ | Sphalerite | 2.CB.05a | ZnS |
| ⓘ | Galena | 2.CD.10 | PbS |
| ⓘ | Pyrite | 2.EB.05a | FeS2 |
| ⓘ | 'Tetrahedrite Subgroup' | 2.GB.05 | Cu6(Cu4C2+2)Sb4S12S |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Cuprite | 4.AA.10 | Cu2O |
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| Group 5 - Nitrates and Carbonates | |||
| ⓘ | Calcite | 5.AB.05 | CaCO3 |
| ⓘ | Cerussite | 5.AB.15 | PbCO3 |
| Group 7 - Sulphates, Chromates, Molybdates and Tungstates | |||
| ⓘ | Anglesite | 7.AD.35 | PbSO4 |
| Group 9 - Silicates | |||
| ⓘ | Chrysocolla | 9.ED.20 | Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1 |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Chrysocolla | Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1 |
| C | Carbon | |
| C | ⓘ Calcite | CaCO3 |
| C | ⓘ Cerussite | PbCO3 |
| O | Oxygen | |
| O | ⓘ Anglesite | PbSO4 |
| O | ⓘ Calcite | CaCO3 |
| O | ⓘ Cerussite | PbCO3 |
| O | ⓘ Chrysocolla | Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1 |
| O | ⓘ Cuprite | Cu2O |
| O | ⓘ Quartz | SiO2 |
| Al | Aluminium | |
| Al | ⓘ Chrysocolla | Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1 |
| Si | Silicon | |
| Si | ⓘ Chrysocolla | Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1 |
| Si | ⓘ Quartz | SiO2 |
| S | Sulfur | |
| S | ⓘ Anglesite | PbSO4 |
| S | ⓘ Galena | PbS |
| S | ⓘ Pyrite | FeS2 |
| S | ⓘ Sphalerite | ZnS |
| S | ⓘ Tetrahedrite Subgroup | Cu6(Cu4C22+)Sb4S12S |
| Ca | Calcium | |
| Ca | ⓘ Calcite | CaCO3 |
| Fe | Iron | |
| Fe | ⓘ Pyrite | FeS2 |
| Cu | Copper | |
| Cu | ⓘ Chrysocolla | Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1 |
| Cu | ⓘ Cuprite | Cu2O |
| Cu | ⓘ Tetrahedrite Subgroup | Cu6(Cu4C22+)Sb4S12S |
| Zn | Zinc | |
| Zn | ⓘ Sphalerite | ZnS |
| Sb | Antimony | |
| Sb | ⓘ Tetrahedrite Subgroup | Cu6(Cu4C22+)Sb4S12S |
| Au | Gold | |
| Au | ⓘ Gold | Au |
| Pb | Lead | |
| Pb | ⓘ Anglesite | PbSO4 |
| Pb | ⓘ Cerussite | PbCO3 |
| Pb | ⓘ Galena | PbS |
Other Databases
| Link to USGS MRDS: | 10101914 |
|---|
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References
