Latitude & Longitude (WGS84):
58° 56' 23'' North , 161° 43' 47'' West
Latitude & Longitude (decimal):
Mindat Locality ID:
199637
Long-form identifier:
mindat:1:2:199637:4
The Red Mountain dunite is probably the major source of platinum metals in the placer deposits of the Salmon River drainage.
Location: This prospect is on the east side of Red Mountain on the ridge between Boulder and Squirrel Creek drainages. The map site is at the approximate center of a large soil geochemistry anomaly at an elevation of about 1,000 feet. It is accurately located.
Geology: Red Mountain is a large, composite ultramafic pluton of Jurassic age (Hoare and Coonrad, 1978). It is dominantly dunite with a thin border zone assemblage of peridotite, clinopyroxenite, and hornblende-bearing rocks (Southwith, 1986; Southwith and Foley, 1986; Alaska Earth Sciences, 2000). This prospect is in dunite between the crest of Red Mountain and the eastern border zone of the pluton. It is defined by a soil-geochemistry anomaly that is 1,700 meters (5,600 feet) long and 700 meters (2,300 feet) wide. Platinum values in this anomaly range from 60 to 3,300 ppb (Alaska Earth Sciences, 2000). Bird and Clark (1976, Table 4, p. 724) reported Red Mountain sample results of up to 1.4 ppm Pt, 0.020 ppm Pd, 0.0300 ppm Rh, and 0.300 ppm Ir. Fechner (1988, p. 43) reported Red Mountain sample results of up to 1.681 ppm Pt, 0.515 ppm Pd, 0.117 ppm Rh, and 0.823 ppm Ir. Chromite occurs as disseminations and layers in the dunite. Platinum-bearing alloys have been identified as inclusions in chromite (Bird and Clark, 1976) and as separate grains in heavy mineral concentrate from residual materials over dunite (Fechner, 1988). Three samples of heavy-mineral concentrate contained a trace to 0.0011 ounce of PGM per cubic yard and a trace to 0.0002 ounce of gold per cubic yard. Platinum was recovered from concentrates of residual materials over dunite sampled near the crest of Red Mountain by the Goodnews Bay Mining Company in 1965 (Mertie, 1969, p. 84). The platinum-bearing alloy inclusions in chromite comprise 20 percent platinum, 40 percent iridium, 25 percent iron and lesser amounts of rhodium, nickel, and chromium (Bird and Clark, 1976, p. 724).
Workings: A surface soil and rock geochemical survey has been completed over a large part of the Red Mountain dunite. An aeromagnetic survey was flown over the Salmon River (Goodnews) area in 1994, a gravity survey has been completed, and some controlled-source audio magneto-telluric lines have been run over selected parts of the ultramafic complex (Alaska Earth Sciences, 2000). A portable washing plant was used for trial placer prospecting of residual material on the crest of Red Mountain in 1965.
Age: Jurassic, the age of the Red Mountain ultramafic pluton. Hoare and Coonrad (1978) report K/Ar ages for two samples of amphibole from the southeast border of the Red Mountain pluton: 176.4 +/- 5.3 Ma and 186.9 +/- 5.6 Ma.
Alteration: Partial to complete serpentization of the dunite is common. Mertie (1969, p. 79) reports that 25 percent of the Red Mountain dunite is serpentine.
Commodities (Major) - Pt; (Minor) - Au, Cr
Development Status: None
Deposit Model: Alaskan PGE (Cox and Singer, 1986; model 9)
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
3 valid minerals.
Gallery:
List of minerals arranged by Strunz 10th Edition classification
List of minerals for each chemical element
Other Databases
| Link to USGS - Alaska: | HG006 |
|---|
Other Regions, Features and Areas containing this locality
This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please
register so you can add to our database. This locality information is for reference purposes only. You should never attempt to
visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders
for access and that you are aware of all safety precautions necessary.
References
Alaska Earth Sciences, 2000, The Goodnews Bay ultramafic complexes: Unpublished data, http://aes.alaska.com/UMAF/FIGURES/page4.html Bird, M.L., and Clark, A.L., 1976, Microprobe study of olivine chromitites of the Goodnews Bay ultramafic complex, Alaska, and the occurrence of platinum: U.S. Geological Survey Journal of Research, v. 4, p. 717-725. Fechner, S.A., 1988, Bureau of Mines mineral investigation of the Goodnews Bay mining district, Alaska: U.S. Bureau of Mines Open-File Report 1-88, 230 p., 3 sheets. Hoare, J.M., and Coonrad, W.L., 1978, Geologic map of the Goodnews and Hagemeister Island quadrangles region, southwestern Alaska: U.S. Geological Survey Open-File Report 78-9-B, 2 sheets, scale 1:250,000. Mertie, J.B., Jr., 1969, Economic geology of platinum minerals: U.S. Geological Survey Professional Paper 630, 120 p. Mertie, J.B., Jr., 1976, Platinum deposits in the Goodnews Bay district, Alaska: U.S. Geological Survey Professional Paper 938, 42 p. Southwith, D.P., 1986, Geology of the Goodnews Bay ultramafic complex: Fairbanks, University of Alaska, M.Sc. thesis, 115 p. Southworth, D.D., and Foley, J.Y., 1986, Lode platinum-group metals potential of the Goodnews Bay ultramafic complex, Alaska: U.S. Bureau of Mines Open-File Report 51-86, 82 p. 
