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 District | Mining District |
| Valdez-Cordova Census Area | Census Area |
| Alaska | State |
| USA | Country |
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Latitude & Longitude (WGS84):
63° 1' 12'' North , 144° 15' 28'' West
Latitude & Longitude (decimal):
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Mentasta Lake | 112 (2011) | 27.0km |
| Slana | 147 (2011) | 37.9km |
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 ElementsCommodity List
This is a list of exploitable or exploited mineral commodities recorded at this locality.Mineral List
5 valid minerals.
Detailed Mineral List:
| ⓘ Azurite Formula: Cu3(CO3)2(OH)2 |
| ⓘ Chalcopyrite Formula: CuFeS2 |
| ⓘ Malachite Formula: Cu2(CO3)(OH)2 |
| ⓘ Pyrite Formula: FeS2 |
| ⓘ Quartz Formula: SiO2 |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 2 - Sulphides and Sulfosalts | |||
|---|---|---|---|
| ⓘ | Chalcopyrite | 2.CB.10a | CuFeS2 |
| ⓘ | Pyrite | 2.EB.05a | FeS2 |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| Group 5 - Nitrates and Carbonates | |||
| ⓘ | Azurite | 5.BA.05 | Cu3(CO3)2(OH)2 |
| ⓘ | Malachite | 5.BA.10 | Cu2(CO3)(OH)2 |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Azurite | Cu3(CO3)2(OH)2 |
| H | ⓘ Malachite | Cu2(CO3)(OH)2 |
| C | Carbon | |
| C | ⓘ Azurite | Cu3(CO3)2(OH)2 |
| C | ⓘ Malachite | Cu2(CO3)(OH)2 |
| O | Oxygen | |
| O | ⓘ Azurite | Cu3(CO3)2(OH)2 |
| O | ⓘ Malachite | Cu2(CO3)(OH)2 |
| O | ⓘ Quartz | SiO2 |
| Si | Silicon | |
| Si | ⓘ Quartz | SiO2 |
| S | Sulfur | |
| S | ⓘ Chalcopyrite | CuFeS2 |
| S | ⓘ Pyrite | FeS2 |
| Fe | Iron | |
| Fe | ⓘ Chalcopyrite | CuFeS2 |
| Fe | ⓘ Pyrite | FeS2 |
| Cu | Copper | |
| Cu | ⓘ Azurite | Cu3(CO3)2(OH)2 |
| Cu | ⓘ Chalcopyrite | CuFeS2 |
| Cu | ⓘ Malachite | Cu2(CO3)(OH)2 |
Other Databases
| Link to USGS - Alaska: | MH362 |
|---|
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