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Salmon River Occurrence, Kiana Mining District, Northwest Arctic Borough, Alaska, USAi
Regional Level Types
Salmon River OccurrenceOccurrence
Kiana Mining DistrictMining District
Northwest Arctic BoroughBorough
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
67° 40' 48'' North , 159° 49' 11'' West
Latitude & Longitude (decimal):
Köppen climate type:
Mindat Locality ID:
199820
Long-form identifier:
mindat:1:2:199820:0
GUID (UUID V4):
0


This occurrence is located in Kobuk Valley National Park.
Location: This occurrence is on the Salmon River at an elevation of about 650 feet. It is in section 5, T. 26 N ., R. 5 W., of the Kateel River Meridian. Cobb (1972, MF-386), location 3, and Schmidt and Allegro (1988), location 123.
Geology: The area of this occurrence is underlain by north-trending, lower to mid-Paleozoic sedimentary and metamorphic rocks (Schmidt and Allegro, 1988). Stream float and bedrock consist of graphitic schist, chloritic schist, light-colored quartz-mica schist and abundant quartz. The mineral occurrence consists of chalcopyrite-bearing quartz veins in graphite-chlorite phyllite. The veins are from 3 inches to 3 feet thick and 100 to 250 feet long. Stringers and blebs of pyrite and chalcopyrite, along with some malachite occur in the quartz veins. A sample of quartz stream float contained more than 20,000 ppm Cu, 6 ppm Ag, and 80 ppb Au. Another sample of chalcopyrite-bearing stream float contained 8,200 ppm Cu, 11 ppm Ag, and 5 ppb Au. Twelve stream silt samples were analyzed and no significant metal values were found (Degenhart and others, 1978). Rock samples collected in the mid-1960's contain from 60 ppm to 2% Cu, 12 to 94 ppm Pb, 6 to 11 ppm Ag, and 5 to 80 ppb Au (Brosge and others, 1967).
Workings: Some evidence of placer exploration in the area was noted by Degenhart and others (1978). The U.S. Bureau of Mines investigated the area in the mid-1970's (Degenhart and others, 1978). They collected two rock samples and 12 stream silt samples. The area was also mapped and sampled by the U.S. Geological Survey (Brosge and others, 1967).
Age: Mid-Paleozoic?

Commodities (Major) - Cu; (Minor) - Ag
Development Status: None
Deposit Model: Chalcopyrite-bearing quartz veins in a graphite-chlorite phyllite.

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


4 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

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

List of minerals for each chemical element

HHydrogen
Hⓘ MalachiteCu2(CO3)(OH)2
CCarbon
Cⓘ MalachiteCu2(CO3)(OH)2
OOxygen
Oⓘ MalachiteCu2(CO3)(OH)2
Oⓘ QuartzSiO2
SiSilicon
Siⓘ QuartzSiO2
SSulfur
Sⓘ ChalcopyriteCuFeS2
Sⓘ PyriteFeS2
FeIron
Feⓘ ChalcopyriteCuFeS2
Feⓘ PyriteFeS2
CuCopper
Cuⓘ ChalcopyriteCuFeS2
Cuⓘ MalachiteCu2(CO3)(OH)2

Other Databases

Link to USGS - Alaska:BM014

Other Regions, Features and Areas containing this locality

North AmericaContinent
North America PlateTectonic Plate

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