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

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Latitude & Longitude (WGS84):
65° 47' 12'' North , 164° 58' 50'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Mindat Locality ID:
197206
Long-form identifier:
mindat:1:2:197206:4
GUID (UUID V4):
0


Location: Dick Creek, located along the southwest border of the Bendeleben D-6 quadrangle, is a north-flowing tributary to Bryan Creek. Bryan Creek is a northeast-flowing drainage with some headwater tributaries on the northeast flank of the Kougarok Mountain upland (TE070, Hudson, 1998). The continental divide separates the Dick Creek drainage from that of Mascot Gulch (BN044) to the south (in the Bendeleben C-6 quadrangle). Sainsbury and others (1969) show 9,000 feet of placer workings along the channel of Dick Creek in its headwater reaches. This is locality 19 of Cobb (1972; MF 417; 1975; OFR 75-429).

Geology: Sainsbury and others (1969) show 9,000 feet of placer workings along the channel of Dick Creek in its headwater reaches. This location is across the continental divide (about 1,140 feet high here) and about 2.3 miles north of the placer workings on Mascot Gulch (BN044). Because there is indication that placer mining took place near the mouth of Dick Creek (locality TE070, Hudson, 1998), the area of mining here may be more extensive than that shown by Sainsbury and others (1969). The presence of stream tin (cassiterite) in the gravels was reported in 1906 (Hess, 1906, p. 157) and mining took place at least by 1908 (Collier and others, 1908). Anderson (1947) reported that both scheelite and cassiterite were present in this drainage. Mining was continuous from 1927 to 1940 and included some dredging (Cobb, 1975, OFR 75-429). Some mining took place as recently as 1952 (Cobb, 1973, B 1374)). The character of the placer deposits has not been described but all mining appears to have been in the main channel and floodplain of Dick Creek; bench placers are apparently not present. Bedrock in the area is part of a Lower Paleozoic metasedimentary assemblage (Sainsbury and others, 1969; Till and others, 1986).

Workings: Sainsbury and others (1969) show 9,000 feet of placer workings in the headwater reaches of Dick Creek. However, because mining is also indicated near the mouth (locality TE070, Hudson, 1998) and because there is a long history of mining of this creek (including dredging, Cobb, 1975), the area of placer mine workings may be more extensive than that shown by Sainsbury and others (1969).

Age: Quaternary.

Commodities: (Major) Au; (Minor) - Sn, W.

Development Status: Yes; small.

Deposit Model: Placer Au-PGE (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


3 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
Native Gold1.AA.05Au
Group 4 - Oxides and Hydroxides
Cassiterite4.DB.05SnO2
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
Scheelite7.GA.05Ca(WO4)

List of minerals for each chemical element

OOxygen
O CassiteriteSnO2
O ScheeliteCa(WO4)
CaCalcium
Ca ScheeliteCa(WO4)
SnTin
Sn CassiteriteSnO2
WTungsten
W ScheeliteCa(WO4)
AuGold
Au Native GoldAu

Other Databases

Link to USGS - Alaska:BN046

Other Regions, Features and Areas containing this locality

North AmericaContinent
North America PlateTectonic Plate

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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