Reynolds; Butte Creek Copper Group Prospect, Chisana Mining District, Southeast Fairbanks Census Area, Alaska, USAi
Regional Level Types | |
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Reynolds; Butte Creek Copper Group Prospect | Prospect |
Chisana Mining District | Mining District |
Southeast Fairbanks Census Area | Census Area |
Alaska | State |
USA | Country |
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Latitude & Longitude (WGS84):
62° 10' 58'' North , 141° 25' 40'' West
Latitude & Longitude (decimal):
Type:
KΓΆppen climate type:
Mindat Locality ID:
199678
Long-form identifier:
mindat:1:2:199678:7
GUID (UUID V4):
11f9a1d8-a5d4-4c1f-9338-0d6dd67c7834
The prospect is in the Wrangell-St. Elias National Preserve.
Location: This prospect is 2,000 feet west of upper Reynolds Creek, a south tributary to the East Fork, Snag Creek. It is at an elevation of about 5,300 feet, 5,000 feet northeast of peak 6827. The site is 0.2 mile east of the center of section 25, T. 5 N., R. 21 E. of the Copper River Meridian. This is locality 2 of Richter and others (1973) and locality 48 of Richter and others (1975). Cobb and Richter (1980) included this prospect under the name 'Reynolds'. It is located to within a few hundred feet.
Geology: Small veins of bornite, chalcocite, specularite, malachite, and calcite cut amygdaloidal basalt of the Triassic, Nikolai Greenstone (Moffit, 1943). The deposits were explored by several open cuts. A chip sample across 5 feet of iron-stained greenstone contained 50 parts per million (ppm) boron, 150 ppm copper, 70 ppm nickel, and 200 ppm vanadium (Matson and Richter, 1971 [OFR 71-202]). Copper mineralization is locally common in Nikolai Greenstone and is thought to have accompanied regional deformation and low-grade metamorphism in the Late Jurassic to Early Cretaceous (MacKevett and others, 1997).
Workings: The deposits were explored by several open cuts.
Age: Cretaceous? Copper mineralization is locally common in Nikolai Greenstone and is thought to have accompanied regional deformation and low-grade metamorphism in the Late Jurassic to Early Cretaceous (MacKevett and others, 1997).
Alteration: Low-grade metamorphic assemblages including quartz, calcite, epidote, zeolites, and some native copper replace basalt or fill amygdules (Richter and others, 1973).
Commodities (Major) - Cu
Development Status: None
Deposit Model: Basaltic copper (Cox and Singer, 1986; model 23)
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
5 valid minerals.
Detailed Mineral List:
β Bornite Formula: Cu5FeS4 |
β Calcite Formula: CaCO3 |
β Chalcocite Formula: Cu2S |
β Hematite Formula: Fe2O3 |
β Hematite var. Specularite Formula: Fe2O3 |
β Malachite Formula: Cu2(CO3)(OH)2 |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
Group 2 - Sulphides and Sulfosalts | |||
---|---|---|---|
β | Chalcocite | 2.BA.05 | Cu2S |
β | Bornite | 2.BA.15 | Cu5FeS4 |
Group 4 - Oxides and Hydroxides | |||
β | Hematite | 4.CB.05 | Fe2O3 |
β | var. Specularite | 4.CB.05 | Fe2O3 |
Group 5 - Nitrates and Carbonates | |||
β | Calcite | 5.AB.05 | CaCO3 |
β | Malachite | 5.BA.10 | Cu2(CO3)(OH)2 |
List of minerals for each chemical element
H | Hydrogen | |
---|---|---|
H | β Malachite | Cu2(CO3)(OH)2 |
C | Carbon | |
C | β Calcite | CaCO3 |
C | β Malachite | Cu2(CO3)(OH)2 |
O | Oxygen | |
O | β Calcite | CaCO3 |
O | β Hematite | Fe2O3 |
O | β Malachite | Cu2(CO3)(OH)2 |
O | β Hematite var. Specularite | Fe2O3 |
S | Sulfur | |
S | β Bornite | Cu5FeS4 |
S | β Chalcocite | Cu2S |
Ca | Calcium | |
Ca | β Calcite | CaCO3 |
Fe | Iron | |
Fe | β Bornite | Cu5FeS4 |
Fe | β Hematite | Fe2O3 |
Fe | β Hematite var. Specularite | Fe2O3 |
Cu | Copper | |
Cu | β Bornite | Cu5FeS4 |
Cu | β Chalcocite | Cu2S |
Cu | β Malachite | Cu2(CO3)(OH)2 |
Other Databases
Link to USGS - Alaska: | NB095 |
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Other Regions, Features and Areas containing this locality
North America
- Wrangell MountainsMountain Range
North America PlateTectonic Plate
- Wrangellia DomainDomain
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