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Moosehead Rack Prospect, Hot Springs Mining District, Yukon-Koyukuk Census Area, Alaska, USAi
Regional Level Types
Moosehead Rack ProspectProspect
Hot Springs Mining DistrictMining District
Yukon-Koyukuk Census AreaCensus Area
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
65° 15' 0'' North , 151° 16' 33'' West
Latitude & Longitude (decimal):
Köppen climate type:
Mindat Locality ID:
198985
Long-form identifier:
mindat:1:2:198985:7
GUID (UUID V4):
0


Although this prospect is not on Doyon, Ltd., lands, mineral exploration of the ground is reported in documents held by Doyon, Ltd., Native Corporation. For more information, contact Doyon, Ltd., at 1 Doyon Place, Suite 300, Fairbanks, Alaska, 99701-2941.
Location: Moosehead Rack, on the south bank of the Yukon River opposite the mouth of Morelock Creek, consists of a four-square-mile terrace rising abruptly more than 200 feet above the river to an elevation of about 900 feet. The site of this approximately located prospect is at an elevation of 600 feet at the west end of Moosehead Rack, in the northwest quarter of section 21, T. 5 N., R. 18 W., of the Fairbanks Meridian. The location is accurate to within a half-mile.
Geology: The country rocks in the area of this prospect include a Cretaceous or Tertiary quartz monzonite stock, Paleozoic limestone, greenstone, and chert, and undated conglomerate, sandstone, shale, and lignite (Chapman and others, 1982). Moosehead Rack is a bedrock terrace cut by the Kaltag fault, a regional east-northeast-trending, right-lateral structure. Bedrock in the area is partly covered by Quaternary loess. The prospect consists of pyritized hornfelsed slate and highly siliceous zones of breccia adjacent to megacrystic granite porphyry (WGM, Inc., 1998). Pyrite, pyrrhotite, and chalcopyrite locally constitute up to 6 percent of the host rock(s). Panning of some of the material yielded colors of gold. The prospect is marked by a red and yellow-white color anomaly, visible from the Yukon River.
Workings: The area has been explored by WGM, Inc. (1998). Details of their work have not been made public.
Age: Cretaceous or younger, inferred from age of granitic pluton.
Alteration: Oxidation of sulfide minerals.

Commodities (Major) - Au
Development Status: None
Deposit Model: Porphyry Cu-Au(?) (Cox and Singer, 1986; model 20c).

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 1 - Elements
ⓘNative Gold1.AA.05Au
Group 2 - Sulphides and Sulfosalts
ⓘChalcopyrite2.CB.10aCuFeS2
ⓘPyrrhotite2.CC.10Fe1-xS
ⓘPyrite2.EB.05aFeS2

List of minerals for each chemical element

SSulfur
Sⓘ ChalcopyriteCuFeS2
Sⓘ PyriteFeS2
Sⓘ PyrrhotiteFe1-xS
FeIron
Feⓘ ChalcopyriteCuFeS2
Feⓘ PyriteFeS2
Feⓘ PyrrhotiteFe1-xS
CuCopper
Cuⓘ ChalcopyriteCuFeS2
AuGold
Auⓘ Native GoldAu

Other Databases

Link to USGS - Alaska:TN039

Other Regions, Features and Areas containing this locality

North AmericaContinent
North America PlateTectonic Plate

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