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Grouse Creek Mine, Nome Mining District, Nome Census Area, Alaska, USAi
Regional Level Types
Grouse Creek MineMine
Nome Mining DistrictMining District
Nome Census AreaCensus Area
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
64° 45' 1'' North , 165° 21' 39'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Nome3,806 (2018)27.8km
Mindat Locality ID:
197838
Long-form identifier:
mindat:1:2:197838:7
GUID (UUID V4):
1ec60b59-3068-4823-81d9-954a6681fb32


Location: Grouse Creek is a small, south-flowing stream on the southeast side of Mount Distin. It is a north tributary to Goldbottom Creek; its confluence with Goldbottom Creek is in the Nome C-1 quadrangle. The creek is auriferous about 1 mile above its mouth (Collier and others, 1908, p. 197-198) and upstream near its confluence with Cold Creek, which is on the Nome C-1 quadrangle (NM100). This is locality 86 of Cobb (1972 [MF-463], 1978 [OFR 78-93]).
Geology: Small-scale placer mining for gold took place as early as 1903 on Grouse Creek (Collier and others, 1908). This early mining was about 1 mile upstream from its confluence with Goldbottom Creek. The pay along this part of the creek was 1 to 3 feet thick and 40 feet wide. The gold was bright and rough, with nuggets as much as 2 pennyweights. Concentrates at this locality were mostly hematite pebbles. Near the mouth of Cold Creek (in the Nome C-1 quadrangle), an east tributary to Grouse Creek, gravels averaged about 5 feet deep, and the gold occured in the gravel and in crevices in marble bedrock (Moffit, 1913, p. 88). This mined area is near a contact between marble and metasedimentary schist. Hummel (locality 28, 1962 [MF-248]) reported copper-bearing minerals in float in upper Grouse Creek (NM089) and copper in the form of tetrahedrite was reported in a quartz vein from the Grouse Creek drainage (Anderson, 1947, p. 11). The headwaters of Grouse Creek are in the area of an extensive gold and arsenic soil anomaly reported by BHP (written communication, 1995). The headwaters of Grouse Creek cross massive marble with intercalated metasedimentary schist (Hummel, 1962 [MF 248]; Bundtzen and others, 1994). Lower Grouse Creek is in pelitic schist, local graphitic quartz schist, and a sill-like body of orthogneiss (C.C. Hawley, written communication, 1999).
Workings: Grouse Creek was prospected and mined at least as early as 1903. It carried a considerable flow of water and was active during some dry years when other creeks were inactive. Mining was on a small scale and mostly hand operations.
Age: Quaternary.

Commodities (Major) - Au
Development Status: Yes; small
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


2 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
Gold1.AA.05Au
Group 4 - Oxides and Hydroxides
Hematite4.CB.05Fe2O3

List of minerals for each chemical element

OOxygen
O HematiteFe2O3
FeIron
Fe HematiteFe2O3
AuGold
Au GoldAu

Other Databases

Link to USGS - Alaska:NM099

Other Regions, Features and Areas containing this locality


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