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Unnamed Occurrence (ARDF - CA027; on Bear Creek), Fairhaven Mining District, Northwest Arctic Borough, Alaska, USAi
Regional Level Types
Unnamed Occurrence (ARDF - CA027; on Bear Creek)- not defined -
Fairhaven Mining DistrictMining District
Northwest Arctic BoroughBorough
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
65° 32' 24'' North , 161° 3' 35'' West
Latitude & Longitude (decimal):
KΓΆppen climate type:
Nearest Settlements:
PlacePopulationDistance
Buckland431 (2017)48.9km
Mindat Locality ID:
200589
Long-form identifier:
mindat:1:2:200589:1
GUID (UUID V4):
6f9bad87-b20d-4a8d-9720-35fcbc3246d7


Not well enough exposed to evaluate potential of deposit.
Location: This occurrence is on Bear Creek, about a half-mile above the junction of Bob Creek. The map site is 200 feet north of the north end of the airstrip, in section 25, T. 2 N., R. 12 W., of the Kateel River Meridian. Cobb (1972, MF-389), location 15.
Geology: Miller and Elliott (1969) report that galena, sphalerite and pyrite occur in andesite at the north end of the airstrip on Bear Creek. The sulfides occur in quartz-calcite veinlets and as disseminated grains in the andesite near a mafic syenite dike. The mineralized zone is about 200 feet wide and trends northwest. Gold can be panned from the limonite cap over the mineralized rock. Stream-sediment samples downstream from the mineralized zone indicate a lead-zinc-copper anomaly extending for about a mile. Soil samples from a drainage ditch above the deposit contain anomalous lead and zinc. Placer gold has been intermittently mined on Bear Creek, mostly downstream from the mineralized area. A polished section shows that arsenopyrite, bournonite and a little gold are present in the sulfide aggregate. This occurrence occurs entirely in Jurassic-Cretaceous andesite and has anomalously high values of antimony and gold. Seven rock samples were collected and analyzed by Miller and Elliot (1969). Gold values were all anomalous and varied from 0.4 to 3.0 ppm; silver varied from 1.5 to 150 ppm; arsenic varied from 500 to greater than 10,000 ppm; copper ranged from 50 to 1,000 ppm; lead ranged from 200 to greater than 20,000 ppm; and zinc varied from 700 to greater than 10,000 ppm.
Workings: The site has been visited and sampled by U.S. Geological Survey and ADGGS geologists. Several exploration companies have also visited the occurrence.
Age: Jurassic - Cretaceous or younger.
Alteration: Limonite alteration.

Commodities (Major) - Au, Cu, Pb, Zn
Development Status: None
Deposit Model: Sulfides in altered andesite.

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


7 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
β“˜Gold1.AA.05Au
Group 2 - Sulphides and Sulfosalts
β“˜Sphalerite2.CB.05aZnS
β“˜Galena2.CD.10PbS
β“˜Pyrite2.EB.05aFeS2
β“˜Bournonite2.GA.50PbCuSbS3
Group 4 - Oxides and Hydroxides
β“˜Quartz4.DA.05SiO2
Group 5 - Nitrates and Carbonates
β“˜Calcite5.AB.05CaCO3
Unclassified
β“˜'Limonite'-

List of minerals for each chemical element

CCarbon
Cβ“˜ CalciteCaCO3
OOxygen
Oβ“˜ CalciteCaCO3
Oβ“˜ QuartzSiO2
SiSilicon
Siβ“˜ QuartzSiO2
SSulfur
Sβ“˜ BournonitePbCuSbS3
Sβ“˜ GalenaPbS
Sβ“˜ PyriteFeS2
Sβ“˜ SphaleriteZnS
CaCalcium
Caβ“˜ CalciteCaCO3
FeIron
Feβ“˜ PyriteFeS2
CuCopper
Cuβ“˜ BournonitePbCuSbS3
ZnZinc
Znβ“˜ SphaleriteZnS
SbAntimony
Sbβ“˜ BournonitePbCuSbS3
AuGold
Auβ“˜ GoldAu
PbLead
Pbβ“˜ BournonitePbCuSbS3
Pbβ“˜ GalenaPbS

Other Databases

Link to USGS - Alaska:CA027

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

Anderson, Eskil, 1947, Mineral occurrences other than gold deposits in northwestern Alaska: Alaska Territorial Division of Mines Pamphlet 5-R, 48 p. Berg, H.C., and Cobb, E.H., 1967, Metalliferous lode deposits of Alaska: U.S. Geological Survey Bulletin 1246, 254 p. Brooks, A.H., 1918, Mineral resources of Alaska, 1916: U.S. Geological Survey Bulletin 662, 469 p. Brooks, A.H., 1921, The future of Alaska mining, in Martin, G.C., and others, Mineral resources of Alaska, 1917: U.S. Geological Survey Bulletin 714-A, p. 5-57. Brooks, A.H., 1923, The Alaska mining industry in 1921: U.S. Geological Survey Bulletin 739-A, p. 1-50. Brooks, A.H., and Martin, G. C., 1921, The Alaska mining industry in 1919: U.S. Geological Survey Bulletin 714-A, p. 59-95. Bundtzen, T.K., Green, C.B., Deagen, J.R., and Daniels, C.L., 1987, Alaska's mineral industry, 1986: Alaska Division of Geological and Geophysical Surveys Special Report 40, 68 p. Cass, J.T., 1959, Reconnaissance geologic map of the Candle quadrangle, Alaska: U.S. Geological Survey Miscellaneous Investigations Series Map I-287, 1 sheet, scale 1:250,000. Cathcart, S.H., 1920, Mining in northwestern Alaska: U.S. Geological Survey Bulletin 712-G, p. 185-198. Cobb, E.H., 1972, Metallic mineral resources map of the Candle Quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-389, 1 sheet, scale 1:250,000. Cobb, E.H., 1973, Placer deposits of Alaska: U.S. Geological Survey Bulletin 1374, 213 p. Cobb, E.H., 1976, Summary of references to mineral occurrences (other than mineral fuels and construction materials) in the Candle, Holy Cross, Norton Bay, Nulato, and Unalakleet quadrangles, Alaska: U.S. Geological Survey Open-File Report 76-866, 102 p. Eakin, H.M., 1915, Placer mining in Seward Peninsula: U.S. Geological Survey Bulletin 622-I, p. 366-373. Gault, H.R., Killeen, P.L., West, W.S., and others, 1953, Reconnaissance for radioactive deposits in the northeastern part of the Seward
 
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