Willard Mining District, Box Elder County, Utah, USAi
Regional Level Types | |
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Willard Mining District | Mining District |
Box Elder County | County |
Utah | State |
USA | Country |
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Type:
Mindat Locality ID:
37347
Long-form identifier:
mindat:1:2:37347:7
GUID (UUID V4):
6dca8069-494f-421b-9caf-625dd4453c0b
The Willard mining district is in extreme eastern Box Elder County just a few miles southeast of Brigham City. The district has produced a small amount of iron ore (about 4000 tons) and has some Cu, Pb, and Zn shows, albeit with no recorded base metal production (Bullock, 1970). Total district metal production at modern metal prices is estimated at $236,000. The Wasatch Iron and Gold Company property is the only recognized producer in the district.
The Willard district lies on the western face of the Wasatch Range of the Middle Rocky Mountain province. The district is underlain by Neoproterozoic Mineral Fork Tillite thrust over Cambrian quartzite, shale, and carbonate rocks by the Willard thrust. No intrusive igneous rocks are recognized in the Willard district.
Mineralization (Fe Β±Cu) occurs in northwest-trending fault zones associated with the Willard thrust and in its upper plate (Doelling, 1980). Bullock (1970) reported a few thousand tons of iron ore were shipped as smelter flux from the Wasatch Iron and Gold mine fissure fillings and replacement deposits along these northwest-trending faults. The main western orebody was reportedly about 20 ft wide by 160 ft long and averaged about 48% Fe. The ore was composed of hematite, magnetite, specularite, and had minor malachite (Bullock, 1970). Doelling (1980) reported that the remaining small, scattered Pb-Ag βpods and bunchesβ of ore in the mine workings are too discontinuous to be economically extracted. Most of the other base metal prospects in the district display minor Cu-staining along narrow veins, fractures, or local narrow replacements.
The Willard district lies on the western face of the Wasatch Range of the Middle Rocky Mountain province. The district is underlain by Neoproterozoic Mineral Fork Tillite thrust over Cambrian quartzite, shale, and carbonate rocks by the Willard thrust. No intrusive igneous rocks are recognized in the Willard district.
Mineralization (Fe Β±Cu) occurs in northwest-trending fault zones associated with the Willard thrust and in its upper plate (Doelling, 1980). Bullock (1970) reported a few thousand tons of iron ore were shipped as smelter flux from the Wasatch Iron and Gold mine fissure fillings and replacement deposits along these northwest-trending faults. The main western orebody was reportedly about 20 ft wide by 160 ft long and averaged about 48% Fe. The ore was composed of hematite, magnetite, specularite, and had minor malachite (Bullock, 1970). Doelling (1980) reported that the remaining small, scattered Pb-Ag βpods and bunchesβ of ore in the mine workings are too discontinuous to be economically extracted. Most of the other base metal prospects in the district display minor Cu-staining along narrow veins, fractures, or local narrow replacements.
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Standard Detailed Gallery Strunz Chemical ElementsCommodity List
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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 | |||
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β | Gold | 1.AA.05 | Au |
β | Silver | 1.AA.05 | Ag |
β | Copper | 1.AA.05 | Cu |
β | Graphite | 1.CB.05a | C |
Group 2 - Sulphides and Sulfosalts | |||
β | Chalcocite | 2.BA.05 | Cu2S |
β | Chalcopyrite | 2.CB.10a | CuFeS2 |
β | Galena | 2.CD.10 | PbS |
β | Stibnite | 2.DB.05 | Sb2S3 |
β | Pyrite | 2.EB.05a | FeS2 |
β | 'Tetrahedrite Subgroup' | 2.GB.05 | Cu6(Cu4C2+2)Sb4S12S |
Group 4 - Oxides and Hydroxides | |||
β | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
β | Hematite | 4.CB.05 | Fe2O3 |
β | var. Specularite | 4.CB.05 | Fe2O3 |
β | Quartz | 4.DA.05 | SiO2 |
β | 'Bindheimite' | 4.DH.20 | Pb2Sb2O6O |
β | Uraninite | 4.DL.05 | UO2 |
Group 5 - Nitrates and Carbonates | |||
β | Calcite | 5.AB.05 | CaCO3 |
β | Azurite | 5.BA.05 | Cu3(CO3)2(OH)2 |
β | Malachite | 5.BA.10 | Cu2(CO3)(OH)2 |
Group 7 - Sulphates, Chromates, Molybdates and Tungstates | |||
β | Anglesite | 7.AD.35 | PbSO4 |
Group 9 - Silicates | |||
β | Zircon | 9.AD.30 | Zr(SiO4) |
β | var. Cyrtolite | 9.AD.30 | Zr[(SiO4),(OH)4] |
β | Muscovite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
Unclassified | |||
β | 'Clay minerals' | - | |
β | 'Limonite' | - |
List of minerals for each chemical element
Fossils
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- Utah
- Box Elder County
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