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Unnamed Occurrence (ARDF - MH362; on upper Alteration Creek), Chistochina Mining District, Valdez-Cordova Census Area, Alaska, USAi
Regional Level Types
Unnamed Occurrence (ARDF - MH362; on upper Alteration Creek)- not defined -
Chistochina Mining DistrictMining District
Valdez-Cordova Census AreaCensus Area
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
63° 1' 12'' North , 144° 15' 28'' West
Latitude & Longitude (decimal):
KΓΆppen climate type:
Nearest Settlements:
PlacePopulationDistance
Mentasta Lake112 (2011)27.0km
Slana147 (2011)37.9km
Mindat Locality ID:
201327
Long-form identifier:
mindat:1:2:201327:8
GUID (UUID V4):
7be7018c-7d1c-4b2c-9e0b-7fe7357a4ab6


Location: Alteration Creek is a south-southeast-flowing tributary of the Slana River, which it enters about 5 miles south of Gillett Pass. The occurrence is on the west side of Alteration Creek at an elevation of about 3,800 feet. It is near the center SW1/4 section 3, T. 14 N., R. 6 E., Copper River Meridian. The occurrence corresponds to locality 2 of Richter and others (1977) and locality 144 in table 2 of Nokleberg and others (1991) and is near locality 32 on figure 6 of Cobb (1979, [OFR 79-238)].
Geology: The rocks in the vicinity of this occurrence consist of intensely hydrothermally altered Tetelna Volcanics of Pennsylvanian age (Richter and others, 1977). (Richter [1967] originally mapped the country rocks as Slana basalt.) The Tetelna Volcanics are mainly composed of flows, avalanche deposits, and tuff interbedded with lesser amounts of fine-grained volcaniclastic rock. A granitic pluton of Cretaceous (?) age crops out about a mile east of the altered zone and could underlie it. The occurrence consists of azurite- and malachite-stained quartz veins that cut intensely iron stained silicified volcanic rocks. The veins contain small amounts of chalcopyrite and pyrite. A sample collected from a chalcopyrite-bearing vein assayed 1.5 percent copper, 0.02 ounce of gold per ton, and 0.54 ounce of silver per ton (Richter, 1967).
Workings: Only limited surface sampling.
Age: Possibly Pennsylvanian to Permian, on the basis of the age of the host rocks; may be related to a nearby Cretaceous (?) intrusion.
Alteration: Silicification and pyritization of Tetelna Volcanics. Oxidation of iron sulfides has been so extensive that primary rock textures are largely obliterated (Richter, 1967).

Commodities (Major) - Ag, Au, Cu
Development Status: None
Deposit Model: Porphyry Cu, distal (Cox and Singer, 1986; model 20c).

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Commodity List

This is a list of exploitable or exploited mineral commodities recorded at this locality.


Mineral List


5 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
β“˜Chalcopyrite2.CB.10aCuFeS2
β“˜Pyrite2.EB.05aFeS2
Group 4 - Oxides and Hydroxides
β“˜Quartz4.DA.05SiO2
Group 5 - Nitrates and Carbonates
β“˜Azurite5.BA.05Cu3(CO3)2(OH)2
β“˜Malachite5.BA.10Cu2(CO3)(OH)2

List of minerals for each chemical element

HHydrogen
Hβ“˜ AzuriteCu3(CO3)2(OH)2
Hβ“˜ MalachiteCu2(CO3)(OH)2
CCarbon
Cβ“˜ AzuriteCu3(CO3)2(OH)2
Cβ“˜ MalachiteCu2(CO3)(OH)2
OOxygen
Oβ“˜ AzuriteCu3(CO3)2(OH)2
Oβ“˜ MalachiteCu2(CO3)(OH)2
Oβ“˜ QuartzSiO2
SiSilicon
Siβ“˜ QuartzSiO2
SSulfur
Sβ“˜ ChalcopyriteCuFeS2
Sβ“˜ PyriteFeS2
FeIron
Feβ“˜ ChalcopyriteCuFeS2
Feβ“˜ PyriteFeS2
CuCopper
Cuβ“˜ AzuriteCu3(CO3)2(OH)2
Cuβ“˜ ChalcopyriteCuFeS2
Cuβ“˜ MalachiteCu2(CO3)(OH)2

Other Databases

Link to USGS - Alaska:MH362

Other Regions, Features and Areas containing this locality


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References

 
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