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Sierra Madre Mining District, Box Elder County, Utah, USAi
| Regional Level Types | |
|---|---|
| Sierra Madre Mining District | Mining District |
| Box Elder County | County |
| Utah | State |
| USA | Country |
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The Sierra Madre mining district is a minor district in the Wasatch Range about 3 mi southeast of Willard and lying mostly in Box Elder County. The district stretches along the Wasatch Front for over 5 mi, including a few prospects in adjoining Weber County on the southwest face of Ben Lomond Peak. The district was developed in very steep terrain and some of the workings were connected by two long, aerial tramways in the early 1900s. However, despite splashy reports in the Salt Lake Mining Review, the district had very limited production of Cu-Au-Ag (205 tons of ore) and only a couple of car loads (less than 100 tons of ore) of Pb-Zn-Ag (Butler and others, 1920; Doelling, 1980). Total district metal production at modern metal prices is estimated at $16,000. None of the mines had any appreciable production.
The Wasatch Range is a part of the Middle Rocky Mountain province. The lower section of the Sierra Madre district is Paleoproterozoic (~1.8 Ga) Farmington Canyon Complex orthogneiss. The gneiss is a light-gray, medium-grained, massive to weakly foliated, biotite-hornblende quartz monzonite cut by narrow, ptygmatic pegmatite dikes and quartz veins. The gneiss is unconformably overlain by Lower and Middle Cambrian Tintic Quartzite, Ophir Formation shales and silty limestone, and Maxfield Limestone.
Mineralization occurs mostly as veins in Paleoproterozoic rocks and to a lesser extent as replacement deposits in the Middle Cambrian Ophir Formation and Maxfield Limestone. Narrow Cu-Ag fissures in the gneiss contain minor pyrite, chalcopyrite, and bornite with minor sericite replacing the original hornblende and biotite. Replacement mineralization is reported in a lower, white, coarse-grained dolomite in the Ophir Formation or basal Maxfield Limestone. Fine-grained galena, sphalerite, and pyrite occur with a gangue of quartz and sericite in small, irregular lenses (Butler and others, 1920; Doelling, 1980). Assays of ore from the upper El Dorado mine average about 5% Pb, 6% Zn, and 10 ppm Ag.
The Wasatch Range is a part of the Middle Rocky Mountain province. The lower section of the Sierra Madre district is Paleoproterozoic (~1.8 Ga) Farmington Canyon Complex orthogneiss. The gneiss is a light-gray, medium-grained, massive to weakly foliated, biotite-hornblende quartz monzonite cut by narrow, ptygmatic pegmatite dikes and quartz veins. The gneiss is unconformably overlain by Lower and Middle Cambrian Tintic Quartzite, Ophir Formation shales and silty limestone, and Maxfield Limestone.
Mineralization occurs mostly as veins in Paleoproterozoic rocks and to a lesser extent as replacement deposits in the Middle Cambrian Ophir Formation and Maxfield Limestone. Narrow Cu-Ag fissures in the gneiss contain minor pyrite, chalcopyrite, and bornite with minor sericite replacing the original hornblende and biotite. Replacement mineralization is reported in a lower, white, coarse-grained dolomite in the Ophir Formation or basal Maxfield Limestone. Fine-grained galena, sphalerite, and pyrite occur with a gangue of quartz and sericite in small, irregular lenses (Butler and others, 1920; Doelling, 1980). Assays of ore from the upper El Dorado mine average about 5% Pb, 6% Zn, and 10 ppm Ag.
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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-localities10 valid minerals.
Rock Types Recorded
Note: data is currently VERY limited. Please bear with us while we work towards adding this information!
Rock list contains entries from the region specified including sub-localities
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Alphabetical List Tree DiagramDetailed Mineral List:
| ⓘ Bornite Formula: Cu5FeS4 |
| ⓘ Chalcopyrite Formula: CuFeS2 |
| ⓘ Galena Formula: PbS |
| ⓘ Hematite Formula: Fe2O3 |
| ⓘ 'Limonite' |
| ⓘ Malachite Formula: Cu2(CO3)(OH)2 |
| ⓘ Native Copper Formula: Cu |
| ⓘ Native Silver Formula: Ag |
| ⓘ Pyrite Formula: FeS2 |
| ⓘ Quartz Formula: SiO2 |
| ⓘ Sphalerite Formula: ZnS |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 1 - Elements | |||
|---|---|---|---|
| ⓘ | Native Copper | 1.AA.05 | Cu |
| ⓘ | Native Silver | 1.AA.05 | Ag |
| Group 2 - Sulphides and Sulfosalts | |||
| ⓘ | Bornite | 2.BA.15 | Cu5FeS4 |
| ⓘ | Sphalerite | 2.CB.05a | ZnS |
| ⓘ | Chalcopyrite | 2.CB.10a | CuFeS2 |
| ⓘ | Galena | 2.CD.10 | PbS |
| ⓘ | Pyrite | 2.EB.05a | FeS2 |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Hematite | 4.CB.05 | Fe2O3 |
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| Group 5 - Nitrates and Carbonates | |||
| ⓘ | Malachite | 5.BA.10 | Cu2(CO3)(OH)2 |
| Unclassified | |||
| ⓘ | 'Limonite' | - | |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Malachite | Cu2(CO3)(OH)2 |
| C | Carbon | |
| C | ⓘ Malachite | Cu2(CO3)(OH)2 |
| O | Oxygen | |
| O | ⓘ Hematite | Fe2O3 |
| O | ⓘ Malachite | Cu2(CO3)(OH)2 |
| O | ⓘ Quartz | SiO2 |
| Si | Silicon | |
| Si | ⓘ Quartz | SiO2 |
| S | Sulfur | |
| S | ⓘ Bornite | Cu5FeS4 |
| S | ⓘ Chalcopyrite | CuFeS2 |
| S | ⓘ Galena | PbS |
| S | ⓘ Pyrite | FeS2 |
| S | ⓘ Sphalerite | ZnS |
| Fe | Iron | |
| Fe | ⓘ Bornite | Cu5FeS4 |
| Fe | ⓘ Chalcopyrite | CuFeS2 |
| Fe | ⓘ Hematite | Fe2O3 |
| Fe | ⓘ Pyrite | FeS2 |
| Cu | Copper | |
| Cu | ⓘ Bornite | Cu5FeS4 |
| Cu | ⓘ Chalcopyrite | CuFeS2 |
| Cu | ⓘ Native Copper | Cu |
| Cu | ⓘ Malachite | Cu2(CO3)(OH)2 |
| Zn | Zinc | |
| Zn | ⓘ Sphalerite | ZnS |
| Ag | Silver | |
| Ag | ⓘ Native Silver | Ag |
| Pb | Lead | |
| Pb | ⓘ 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
- Box Elder County
- Sierra Madre Mining District
- Box Elder County
Other Regions, Features and Areas that Intersect
North AmericaContinent
- Rocky MountainsMountain Range
North America PlateTectonic Plate
- Basin and Range BasinsBasin
- Farmington-Selway DomainDomain
- Middle Rocky MountainsOrogenic Belt
- Oquirrh BasinBasin
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References
services.arcgis.com (n.d.) https://services.arcgis.com/ZzrwjTRez6FJiOq4/arcgis/rest/services/Metal_Mineral_Resources_web_View/FeatureServer/6/117/attachments/114