Gravel Pit Occurrence, Chistochina Mining District, Valdez-Cordova Census Area, Alaska, USAi
Regional Level Types | |
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Gravel Pit Occurrence | Occurrence |
Chistochina Mining District | Mining District |
Valdez-Cordova Census Area | Census Area |
Alaska | State |
USA | Country |
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Latitude & Longitude (WGS84):
63° 3' 21'' North , 145° 45' 0'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Mindat Locality ID:
197798
Long-form identifier:
mindat:1:2:197798:4
GUID (UUID V4):
92b2ab5f-4c44-4521-a753-48ae5a061540
Location: This occurrence is in a gravel pit at an elevation of 3,650 feet on the north side of the Denali Highway, 1.9 miles southeast of Fourteenmile Lake. It is in the NW1/4NW1/4 section 36, T. 21 S., R. 10 E., Fairbanks Meridian.
Geology: Peridotite in a borrow pit on the side of the Denali Highway contains as much as 1 percent disseminated pyrrhotite and traces of platinum group elements (L.D. Hulbert, oral communication, 2001). The peridotite probably is part of the Tangle ultramafic-mafic complex of Late Triassic age. Two grab samples collected by MAN Resources respectively contained 0.11 percent nickel, 0.01 percent copper, 67 ppb palladium, and 146 ppb platinum and 0.27 percent nickel, 0.09 percent copper, 58 parts per billion (ppb) palladium, 51 ppb platinum, and 51 ppb gold (L.D. Hulbert, oral communication, 2001). The Tangle complex is a north-dipping layered intrusion of dunite, peridotite, and gabbro that varies from less than 2,000 feet thick to more than 4,000 feet thick and extends for more than 12 miles in length (W.T. Ellis, oral communication, 2001). The complex is believed to be a lopolithic feeder of the Nikolai basalt flows of the Wrangellia Terrane (W.T. Ellis, oral communication, 2001). The complex intrudes the Tangle Formation of Permian age (Nokleberg and others, 1991). It may connect with the Fish Lake complex at depth below the Amphitheater synform. Magmatic mineralization is synchronous with emplacement of the Tangle complex, which is part of a 120-mile-long belt of mafic-ultramafic and associated rocks in the east-central Alaska Range.
Workings: Two grab samples collected by MAN Resources respectively contained 0.11 percent nickel, 0.01 percent copper, 67 parts per billion (ppb) palladium, and 146 ppb platinum and 0.27 percent nickel, 0.09 percent copper, 58 ppb palladium, 51 ppb platinum, and 51 ppb gold. The occurrence is on active claims of MAN Resources.
Age: Late Triassic.
Alteration: The peridotite is locally serpentinized.
Commodities (Major) - Cu, Ni, Pd, Pt; (Minor) - Au
Development Status: None
Deposit Model: Ni-Cu-PGE in differentiated mafic-ultramafic sill.
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
1 valid mineral.
Detailed Mineral List:
ⓘ 'Fayalite-Forsterite Series' |
ⓘ Pyrrhotite Formula: Fe1-xS |
ⓘ 'Serpentine Subgroup' Formula: D3[Si2O5](OH)4 |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
Group 2 - Sulphides and Sulfosalts | |||
---|---|---|---|
ⓘ | Pyrrhotite | 2.CC.10 | Fe1-xS |
Unclassified | |||
ⓘ | 'Fayalite-Forsterite Series' | - | |
ⓘ | 'Serpentine Subgroup' | - | D3[Si2O5](OH)4 |
List of minerals for each chemical element
H | Hydrogen | |
---|---|---|
H | ⓘ Serpentine Subgroup | D3[Si2O5](OH)4 |
O | Oxygen | |
O | ⓘ Serpentine Subgroup | D3[Si2O5](OH)4 |
Si | Silicon | |
Si | ⓘ Serpentine Subgroup | D3[Si2O5](OH)4 |
S | Sulfur | |
S | ⓘ Pyrrhotite | Fe1-xS |
Fe | Iron | |
Fe | ⓘ Pyrrhotite | Fe1-xS |
Other Databases
Link to USGS - Alaska: | MH193 |
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Other Regions, Features and Areas containing this locality
North America PlateTectonic Plate
- Wrangellia DomainDomain
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