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Unnamed Occurrence (ARDF - BT016; tributary to the Kanuti River), Koyukuk Mining District, Yukon-Koyukuk Census Area, Alaska, USAi
Regional Level Types
Unnamed Occurrence (ARDF - BT016; tributary to the Kanuti River)- not defined -
Koyukuk Mining DistrictMining District
Yukon-Koyukuk Census AreaCensus Area
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
66° 12' 38'' North , 151° 5' 27'' West
Latitude & Longitude (decimal):
Köppen climate type:
Mindat Locality ID:
200579
Long-form identifier:
mindat:1:2:200579:2
GUID (UUID V4):
0


Location: This placer occurrence is on an unnamed, north-flowing tributary to the Kanuti River about 0.5 mile upstream from its mouth. The creek is is about 6.2 miles north-northeast of the north end of Tokusatatquaten Lake in the SW1/4 section 14, T. 16 N., R. 17 W. of the Fairbanks Meridian. The location is accurate within 1 mile.
Geology: Two very fine gold flakes were noted in eight panned samples collected from this unnamed creek. The panned samples contain 2,119 ppb gold and 252 ppm chromium (Kurtak and others, 2002). The rocks in the area are chlorite schist and interbedded metagraywacke cut by quartz veinlets (Patton and Miller, 1973). Upstream, the creek passes over the contact of the Sithylemenkat Pluton. No other information is available.
Workings: Placer claims were located in the 1960's and 1970's.
Age: Quaternary.

Commodities (Major) - Au
Development Status: None
Deposit Model: Placer Au (Cox and Singer, 1986; model 39a)

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


1 valid mineral.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
ⓘGold1.AA.05Au

List of minerals for each chemical element

AuGold
Auⓘ GoldAu

Other Databases

Link to USGS - Alaska:BT016

Other Regions, Features and Areas containing this locality

North AmericaContinent
North America PlateTectonic Plate

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