Black Hat Mine, La Sal Creek Mining District, San Juan County, Utah, USAi
| Regional Level Types | |
|---|---|
| Black Hat Mine | Mine |
| La Sal Creek Mining District | Mining District |
| San Juan County | County |
| Utah | State |
| USA | Country |
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Latitude & Longitude (WGS84):
38° 20' 15'' North , 109° 3' 37'' West
Latitude & Longitude (decimal):
Type:
Deposit first discovered:
1953
Age:
152.1 ± 0.9 to ~145.0 Ma
Geologic Time:
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| La Sal | 395 (2011) | 16.6km |
| Spanish Valley | 491 (2011) | 38.7km |
| Naturita | 528 (2017) | 44.9km |
| Castle Valley | 342 (2017) | 45.2km |
| Moab | 5,235 (2017) | 50.0km |
Mindat Locality ID:
38564
Long-form identifier:
mindat:1:2:38564:9
GUID (UUID V4):
caa0b90e-7e50-476b-bef1-dab5031ebcc2
A former U-V occurrence/mine located in sec. 28, T28S, R26E, SLM, on National Forest land and/or Bureau of Land Management administered land (located claim) (0.75 miles (1.21 km) N of highway 46 crossing the Utah-Colorado state line). Discovered in 1953. Owned by Lark Washburn, Colorado (1974); owned by William McCormick (1977); Owned and operated by Geo Energy Res.; owned by Truman Goode (1977). MRDS database stated accuracy for this location is 100 meters. Part of this mine is in Utah and part is in Colorado. The haulage portal is on Bureau of Land Management administered land, while the mine enters the national forest.
Mineralization is hosted in Late Jurassic mudstone and sandstone of the Salt Wash Member of the Morrison Formation. Local rocks include Jurassic (2) sedimentary rocks in southeastern Utah.
NOTE: The 2 USGS MRDS files provide discrepant data regarding the orebody(ies):
The orebody is sedimentary lenticular and tabular-irregular in form, strikes N45W and dips 02N. Primary ore control was lithology. The average thickness of unconsolidated materials is 1.5 meters.
OR
The orebody is lenticular, tabular & irregular, strikes E-W, dips 7S at a thickness of 1.83 meters, a width of 18.29 meters and a depth-to-top of 9.14 meters. Controls for ore emplacement included paleochannels.
Local geologic structures include the La Sal Creek Syncline.
Workings include underground openings with a length of 6,098 meters. The workings are very extensive, some are flooded and caved. Mine was not fully examined.
Reserve-resources data are found in Jones, H. (1977).
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
9 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:
| ⓘ Carnotite Formula: K2(UO2)2(VO4)2 · 3H2O |
| ⓘ Coffinite Formula: U(SiO4) · nH2O |
| ⓘ Corvusite Formula: (Na,K,Ca,Mg)2(V5+,V4+,Fe2+)8O20 · 6-10H2O |
| ⓘ Melanovanadite Formula: Ca(V5+,V4+)4O10 · 5H2O |
| ⓘ Montroseite Formula: (V3+,Fe3+)O(OH) |
| ⓘ Postite Formula: Mg(H2O)6Al2(OH)2(H2O)8(V10O28) · 13H2O |
| ⓘ Pyrite Formula: FeS2 |
| ⓘ Roscoelite Formula: K(V3+,Al)2(AlSi3O10)(OH)2 |
| ⓘ Uraninite Formula: UO2 |
| ⓘ Uraninite var. Pitchblende Formula: UO2 |
List of minerals arranged by Strunz 10th Edition classification
| Group 2 - Sulphides and Sulfosalts | |||
|---|---|---|---|
| ⓘ | Pyrite | 2.EB.05a | FeS2 |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Uraninite var. Pitchblende | 4.DL.05 | UO2 |
| ⓘ | 4.DL.05 | UO2 | |
| ⓘ | Montroseite | 4.FD.10 | (V3+,Fe3+)O(OH) |
| ⓘ | Carnotite | 4.HB.05 | K2(UO2)2(VO4)2 · 3H2O |
| ⓘ | Postite | 4.HC.55 | Mg(H2O)6Al2(OH)2(H2O)8(V10O28) · 13H2O |
| ⓘ | Melanovanadite | 4.HE.05 | Ca(V5+,V4+)4O10 · 5H2O |
| ⓘ | Corvusite | 4.HE.20 | (Na,K,Ca,Mg)2(V5+,V4+,Fe2+)8O20 · 6-10H2O |
| Group 9 - Silicates | |||
| ⓘ | Coffinite | 9.AD.30 | U(SiO4) · nH2O |
| ⓘ | Roscoelite | 9.EC.15 | K(V3+,Al)2(AlSi3O10)(OH)2 |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Carnotite | K2(UO2)2(VO4)2 · 3H2O |
| H | ⓘ Coffinite | U(SiO4) · nH2O |
| H | ⓘ Corvusite | (Na,K,Ca,Mg)2(V5+,V4+,Fe2+)8O20 · 6-10H2O |
| H | ⓘ Melanovanadite | Ca(V5+,V4+)4O10 · 5H2O |
| H | ⓘ Montroseite | (V3+,Fe3+)O(OH) |
| H | ⓘ Roscoelite | K(V3+,Al)2(AlSi3O10)(OH)2 |
| H | ⓘ Postite | Mg(H2O)6Al2(OH)2(H2O)8(V10O28) · 13H2O |
| O | Oxygen | |
| O | ⓘ Carnotite | K2(UO2)2(VO4)2 · 3H2O |
| O | ⓘ Coffinite | U(SiO4) · nH2O |
| O | ⓘ Corvusite | (Na,K,Ca,Mg)2(V5+,V4+,Fe2+)8O20 · 6-10H2O |
| O | ⓘ Melanovanadite | Ca(V5+,V4+)4O10 · 5H2O |
| O | ⓘ Montroseite | (V3+,Fe3+)O(OH) |
| O | ⓘ Uraninite var. Pitchblende | UO2 |
| O | ⓘ Roscoelite | K(V3+,Al)2(AlSi3O10)(OH)2 |
| O | ⓘ Uraninite | UO2 |
| O | ⓘ Postite | Mg(H2O)6Al2(OH)2(H2O)8(V10O28) · 13H2O |
| Na | Sodium | |
| Na | ⓘ Corvusite | (Na,K,Ca,Mg)2(V5+,V4+,Fe2+)8O20 · 6-10H2O |
| Mg | Magnesium | |
| Mg | ⓘ Corvusite | (Na,K,Ca,Mg)2(V5+,V4+,Fe2+)8O20 · 6-10H2O |
| Mg | ⓘ Postite | Mg(H2O)6Al2(OH)2(H2O)8(V10O28) · 13H2O |
| Al | Aluminium | |
| Al | ⓘ Roscoelite | K(V3+,Al)2(AlSi3O10)(OH)2 |
| Al | ⓘ Postite | Mg(H2O)6Al2(OH)2(H2O)8(V10O28) · 13H2O |
| Si | Silicon | |
| Si | ⓘ Coffinite | U(SiO4) · nH2O |
| Si | ⓘ Roscoelite | K(V3+,Al)2(AlSi3O10)(OH)2 |
| S | Sulfur | |
| S | ⓘ Pyrite | FeS2 |
| K | Potassium | |
| K | ⓘ Carnotite | K2(UO2)2(VO4)2 · 3H2O |
| K | ⓘ Corvusite | (Na,K,Ca,Mg)2(V5+,V4+,Fe2+)8O20 · 6-10H2O |
| K | ⓘ Roscoelite | K(V3+,Al)2(AlSi3O10)(OH)2 |
| Ca | Calcium | |
| Ca | ⓘ Corvusite | (Na,K,Ca,Mg)2(V5+,V4+,Fe2+)8O20 · 6-10H2O |
| Ca | ⓘ Melanovanadite | Ca(V5+,V4+)4O10 · 5H2O |
| V | Vanadium | |
| V | ⓘ Carnotite | K2(UO2)2(VO4)2 · 3H2O |
| V | ⓘ Corvusite | (Na,K,Ca,Mg)2(V5+,V4+,Fe2+)8O20 · 6-10H2O |
| V | ⓘ Melanovanadite | Ca(V5+,V4+)4O10 · 5H2O |
| V | ⓘ Montroseite | (V3+,Fe3+)O(OH) |
| V | ⓘ Roscoelite | K(V3+,Al)2(AlSi3O10)(OH)2 |
| V | ⓘ Postite | Mg(H2O)6Al2(OH)2(H2O)8(V10O28) · 13H2O |
| Fe | Iron | |
| Fe | ⓘ Corvusite | (Na,K,Ca,Mg)2(V5+,V4+,Fe2+)8O20 · 6-10H2O |
| Fe | ⓘ Montroseite | (V3+,Fe3+)O(OH) |
| Fe | ⓘ Pyrite | FeS2 |
| U | Uranium | |
| U | ⓘ Carnotite | K2(UO2)2(VO4)2 · 3H2O |
| U | ⓘ Coffinite | U(SiO4) · nH2O |
| U | ⓘ Uraninite var. Pitchblende | UO2 |
| U | ⓘ Uraninite | UO2 |
Other Databases
| Link to USGS MRDS: | 10088021 |
|---|
Other Regions, Features and Areas containing this locality
North America PlateTectonic Plate
- Great Plains DomainDomain
- Paradox BasinBasin
USA
- Colorado PlateauPlateau
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References
