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Fairview Prospect, Aniak Mining District, Bethel Census Area, Alaska, USAi
Regional Level Types
Fairview ProspectProspect
Aniak Mining DistrictMining District
Bethel Census AreaCensus Area
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
61° 45' 26'' North , 157° 22' 30'' West
Latitude & Longitude (decimal):
Köppen climate type:
Mindat Locality ID:
197442
Long-form identifier:
mindat:1:2:197442:6
GUID (UUID V4):
0


Location: The Fairview prospect is along the the crest of a northwest-trending ridge, about 1.8 miles southwest of the mouth of McCally Creek. It is at an elevation of about 1,000 feet in the NE1/4 sec. 11, T. 19 N., R. 45 W., of the Seward Meridian. The prospect is locality 17 of Miller and others (1989). The location is accurate.
Geology: The Fairview prospect is unusual because it is one of the few cinnabar prospects in the Kuskokwim mineral belt that is wholly in intrusive rock. The host rock is an altered, sericitized, quartz-feldspar-porphyry sill about 120 feet thick and 1,000 feet long that trends northwest, parallel to the strike of the shale and sandstone of the Upper Cretaceous, Kuskokwim Group that contains the sill (Cady and others, 1955; Sainsbury and MacKevett, 1965). The Fairview deposit has a 40Ar/39Ar isochron age of 72.6 Ma (Gray, Gent, and others, 1997); it is the only mercury deposit in the Red Devil area that has been dated. The mineralization consists of cinnabar, stibnite, and quartz that fills several parallel fractures in the central part of the altered felsic sill. In the early 1940s, three trenches were sampled by the U.S. Bureau of Mines (Webber and others (1947). One 50-foot zone in trench 1 averaged 0.15 percent mercury ; one 5-foot zone in trench 2 averaged 0.40 percent mercury.
Workings: The property was discovered in the 1920s by tracing cinnabar-bearing float up slope from a stream below it. The Fairview prospect was staked in 1935 or 1936 (Webber and others, 1947). The U.S. Bureau of Mines trenched the property in 1943, but by 1959, the trenches were largely filled by vegetation (Sainsbury and MacKevett, 1965). Three trenches were cut normal to the felsic sill. In the early 1940s, the trenches were sampled by the U.S. Bureau of Mines (Webber and others (1947).
Age: The Fairview prospect has a 40Ar/39Ar age of 72.6 Ma (Gray, Gent, and others, 1997).
Alteration: Sericitic alteration in quartz-feldspar porphyry.

Commodities (Major) - Hg; (Minor) - Sb
Development Status: None
Deposit Model: Silica-carbonate mercury (Cox and Singer, 1986; model 27c).

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

Group 2 - Sulphides and Sulfosalts
ⓘCinnabar2.CD.15aHgS
ⓘStibnite2.DB.05Sb2S3
Group 4 - Oxides and Hydroxides
ⓘQuartz4.DA.05SiO2

List of minerals for each chemical element

OOxygen
Oⓘ QuartzSiO2
SiSilicon
Siⓘ QuartzSiO2
SSulfur
Sⓘ CinnabarHgS
Sⓘ StibniteSb2S3
SbAntimony
Sbⓘ StibniteSb2S3
HgMercury
Hgⓘ CinnabarHgS

Other Databases

Link to USGS - Alaska:SM019

Other Regions, Features and Areas containing this locality


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References

Cady, W.M., Wallace, R.E., Hoare, J.M., and Webber, E.J., 1955, The central Kuskokwim region, Alaska: U.S. Geological Survey Professional Paper 268, 132 p. Cobb, E.H., 1972, Metallic mineral resources map of the Sleetmute quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-368, 1 sheet, scale 1:250,000. Cobb, E.H., 1976, Summary of references to mineral occurrences (other than mineral fuels and construction materials) in the Dillingham, Sleetmute, and Taylor Mountains quadrangles, Alaska: U.S. Geological Survey Open-File Report 76-606, 92 p. Gray, J.E., Gent, C.A., Snee, L.W., and Wilson, F.H., 1997, Epithermal mercury-antimony and gold-bearing vein lodes of southwest Alaska, in Goldfarb, R.J., and Miller, L.D., eds., Mineral Deposits of Alaska: Economic Geology Monograph 9, p. 287-305. MacKevett, E.M., Jr., and Berg, H.C., 1963, Geology of the Red Devil quicksilver mine, Alaska: U.S. Geological Survey Bulletin 1142-G, p. G1-G16. Miller, M.L., Belkin, H.E., Blodgett, R.B., Bundtzen, T.K., Cady, J.W., Goldfarb, R.J., Gray, J.E., McGimsey, R.G., and Simpson, S.L., 1989, Pre-field study and mineral resource assessment of the Sleetmute quadrangle, southwestern Alaska: U.S. Geological Survey Open-File Report 89-363, 115 p., 3 plates, scale 1:250,000. Roedder, E., 1972, Compositions of fluid inclusions: U.S. Geological Survey Professional Paper 440-JJ, 164 p. Sainsbury, C.L. and MacKevett, E.M., Jr., 1965, Quicksilver deposits of southwestern Alaska: U.S. Geological Survey Bulletin 1187, 89 p. Webber, B.S., Bjorklund, S.C., Rutledge, F.A., Thomas, B.I., and Wright, W.S., 1947, Mercury deposits of southwestern Alaska: U.S. Bureau of Mines Report of Investigations 4065, 57 p. Wells, J.T., and Ghiorso, M.S., 1988, Rock alteration, mercury transport, and metal deposition at Sulphur Bank, California: Economic Geology, vol. 83, p. 606-618. White, D. E., and Robinson, C. E., 1962, Sulphur Bank, California, a major hot spring quick
 
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