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Unnamed Occurrence (ARDF - MH039; west of Clearwater Creek), Valdez Creek Mining District, Matanuska-Susitna Borough, Alaska, USAi
Regional Level Types
Unnamed Occurrence (ARDF - MH039; west of Clearwater Creek)- not defined -
Valdez Creek Mining DistrictMining District
Matanuska-Susitna BoroughBorough
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
63° 8' 7'' North , 146° 59' 52'' West
Latitude & Longitude (decimal):
KΓΆppen climate type:
Mindat Locality ID:
201187
Long-form identifier:
mindat:1:2:201187:8
GUID (UUID V4):
8d8d8116-dcbe-4d10-ba45-5f73ede4b78b


Copper values are locally very high, but the occurrences are small and there is a low potential for copper (Kurtak and others, 1992).
Location: This occurrence is at an elevation of about 4,500 feet about 1.6 miles south-southwest of the junction of Clearwater and Pass Creeks, in the NW1/4SW1/4 section 33, T. 20 S., R. 4 E., Fairbanks Meridian. The occurrence corresponds to locality A41 of Kurtak and others (1992), to locality 2 in figure 4 of Cobb (1979 [OFR 79-238]), and to locality 41 in table 2 of Nokleberg and others (1991).
Geology: Bedrock in the area consists of Nikolai Greenstone of Late Triassic age that is locally sheared and silicified and cut by quartz veinlets (Nokleberg and others, 1991; Kurtak and others, 1992, table A41). The deposits consist of copper minerals, including chalcocite, chrysocolla, native copper, azurite, and malachite, in quartz veins, in vesicles, and on joint and fracture surfaces of propylitized and locally silicified basalt (Smith and others, 1973; Kurtak and others, 1992). Copper content of three samples of basalt with visible copper minerals assayed from 2.52 to 4.9 percent copper and 1.2 to 5.2 parts per million silver; gold was not reported (Kurtak and others, 1992).
Workings: Several zones stained by copper oxides were sampled by the U.S. Bureau of Mines (Kurtak and others, 1992, table A41). Samples contained as much as 4.9 percent copper; a placer sample collected one mile south of the occurrence contained no gold.
Age: The copper deposits are probably either Cretaceous or early Tertiary in age (see see MH060 and MH100).
Alteration: Basalt is propylitized and locally silicified.

Commodities (Major) - Cu; (Minor) - Ag
Development Status: None
Deposit Model: Basaltic Cu (Cox and Singer, 1986; model 23).

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


6 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
β“˜Copper1.AA.05Cu
Group 2 - Sulphides and Sulfosalts
β“˜Chalcocite2.BA.05Cu2S
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
Group 9 - Silicates
β“˜Chrysocolla9.ED.20Cu2-xAlx(H2-xSi2O5)(OH)4 Β· nH2O, x < 1

List of minerals for each chemical element

HHydrogen
Hβ“˜ AzuriteCu3(CO3)2(OH)2
Hβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
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“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Oβ“˜ MalachiteCu2(CO3)(OH)2
Oβ“˜ QuartzSiO2
AlAluminium
Alβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
SiSilicon
Siβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Siβ“˜ QuartzSiO2
SSulfur
Sβ“˜ ChalcociteCu2S
CuCopper
Cuβ“˜ AzuriteCu3(CO3)2(OH)2
Cuβ“˜ ChalcociteCu2S
Cuβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Cuβ“˜ CopperCu
Cuβ“˜ MalachiteCu2(CO3)(OH)2

Other Databases

Link to USGS - Alaska:MH039

Other Regions, Features and Areas containing this locality


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