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Hayes Glacier West Prospect, Delta River Mining District, Southeast Fairbanks Census Area, Alaska, USAi
Regional Level Types
Hayes Glacier West ProspectProspect
Delta River Mining DistrictMining District
Southeast Fairbanks Census AreaCensus Area
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
63° 40' 54'' North , 146° 38' 49'' West
Latitude & Longitude (decimal):
Köppen climate type:
Mindat Locality ID:
197923
Long-form identifier:
mindat:1:2:197923:0
GUID (UUID V4):
01164170-1f14-4ba9-9648-45c69edcd0d4


Location: The prospect is about 2.5 miles northeast of peak 8376, a northern spur of Mount Hayes, at an elevation of 5,100 feet. The prospect is in the SE1/4SE1/4 section 19, T. 14 S., R. 6 E., Fairbanks Meridian, and corresponds to locality N6 in table 2 of Nokleberg and others (1991).
Geology: This prospect is part of a belt of massive sulfide deposits that is about 8 miles long and as much as one-third mile wide. Deposits in the belt consist of massive sulfide lenses, pods, and disseminations of pyrrhotite and pyrite, along with less abundant galena, sphalerite, and chalcopyrite. Individual lenses and pods are as much as 3 feet thick. The host rocks of the Hayes Glacier West deposit are derived from Devonian felsic to intermediate volcanic rocks, mainly andesite, dacite, and quartz keratophyre flows and tuffs, and from Devonian or older shale, marl, and marble (Nokleberg and Aleinikoff, 1985; Lange and others, 1993). The rocks are intensely deformed and feature abundant mylonite schist; they were first metamorphosed to lower amphibolite facies and then retrograded to lower greenschist facies. Samples collected during reconnaissance sampling by the U.S. Geological Survey in the 1980's contained as much as 0.72 percent lead, 0.69 percent zinc, 0.5 percent arsenic, and 0.11 percent copper (Nokleberg and others, 1991).
Workings: Grab samples contained as much as 0.11 percent copper 0.72 percent lead, 0.69 percent zinc, 0.2 part per million (ppm) gold, and 5 ppm silver (Nokleberg and others, 1991). Trace elements characteristic of the deposit include gold (to 0.2 ppm), silver (to 5 ppm), and tin (to 100 ppm). American Copper and Nickel Company sampled the prospect in 1993 (W.T. Ellis, unpublished data, 1993) and concluded that the mineralization consists mainly of pyrrhotite and has generally low base metals values.
Age: Devonian, the age of the host strata.

Commodities (Major) - Pb, Zn; (Minor) - Ag, As, Au, Cu, Sn
Development Status: None
Deposit Model: Kuroko massive sulfide (Cox and Singer, 1986; model 28a).

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
Sphalerite2.CB.05aZnS
Chalcopyrite2.CB.10aCuFeS2
Galena2.CD.10PbS
Pyrite2.EB.05aFeS2

List of minerals for each chemical element

SSulfur
S ChalcopyriteCuFeS2
S GalenaPbS
S PyriteFeS2
S SphaleriteZnS
FeIron
Fe ChalcopyriteCuFeS2
Fe PyriteFeS2
CuCopper
Cu ChalcopyriteCuFeS2
ZnZinc
Zn SphaleriteZnS
PbLead
Pb GalenaPbS

Other Databases

Link to USGS - Alaska:MH007

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

 
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