Archibald Creek; Archibald Gulch Mine, Koyukuk Mining District, Yukon-Koyukuk Census Area, Alaska, USAi
Regional Level Types | |
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Archibald Creek; Archibald Gulch Mine | Mine |
Koyukuk Mining District | Mining District |
Yukon-Koyukuk Census Area | Census Area |
Alaska | State |
USA | Country |
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Latitude & Longitude (WGS84):
67° 28' 56'' North , 150° 12' 28'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Mindat Locality ID:
196307
Long-form identifier:
mindat:1:2:196307:9
GUID (UUID V4):
2743d85e-f3ea-4607-a66f-aad9e15cd293
See also Nolan Creek (WI101).
Location: Archibald Creek is a west-flowing tributary to Nolan Creek. Its mouth is about 1.75 miles above the mouth of Nolan Creek on Wiseman Creek. Most of the mining activity on Archibald Creek has been along the lower 0.5 mile of the creek; the coordinates are about at the center of mining. The location is accurate.
Geology: Placer gold has been mined both from the modern channel and a deep channel on Archibald Creek. The modern channel was mined near the mouth of the creek in the early 1900's and was being mined about 3/8 mile upstream in 1937. The gravel in the modern channel is coarse and subangular; it contains many boulders. Five to twelve feet of frozen gravel, covered by 3 feet of muck and a foot of moss, overlie soft, schist bedrock. The gold is distributed throughout the gravel and occurs both as fine particles worn flat and smooth, and as coarse particles that are rough and porous. The average fineness of the gold is 905 and the value of the ground is about $0.44 per square foot of bedrock (gold at $35 per ounce) (Reed, 1938). The deep channel which is 5 to to 14 feet wide is on the north side of the creek at a depth of about 25 feet near the mouth of the creek; it rises upstream to coalesce with the modern channel. Seven to nine feet of frozen, coarse, subangular gravel overlies bedrock described as alternating bands of black graphitic and yellow schist (Reed, 1938). The gravel is overlain by 16 to 18 feet of muck and a foot of moss. Unlike the modern channel, the deep channel is free of large boulders. The gold in the deep channel occurs both as coarse, worn and rounded particles, and as coarse, porous and unworn particles. Reed (1938) reports values of approximately $2.11 per square foot of bedrock (gold at $35 per ounce) and an average fineness of 904. A stibnite vein was reported during drift mining on Archibald Creek (Ebbley and Wright, 1948.
Workings: The creek and bench placers have been mined by hand and hydraulic methods, and the deep channel by drifting. Mulligan (1974) reported hand mining in 1974.
Age: Quaternary.
Production: Maddren (1913) reported $6,000 of gold (about 300 ounces) was produced from 1900 to 1909 . Eden (2000) reports a total of 5429.90 ounces of gold were produced from Archibald Creek between 1904 and 1999. Most of the production from Archibald Creek has been from the buried channels. Tri-Con Mining mined on Archibald Creek as late as 1991 (Bundtzen and others, 1992).
Commodities (Major) - Au; (Minor) - Sb(?)
Development Status: Yes; small
Deposit Model: Placer Au (Cox and Singer, 1986; model 39a)
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsGallery:
List of minerals arranged by Strunz 10th Edition classification
Group 1 - Elements | |||
---|---|---|---|
ⓘ | Gold | 1.AA.05 | Au |
Group 2 - Sulphides and Sulfosalts | |||
ⓘ | Stibnite | 2.DB.05 | Sb2S3 |
List of minerals for each chemical element
S | Sulfur | |
---|---|---|
S | ⓘ Stibnite | Sb2S3 |
Sb | Antimony | |
Sb | ⓘ Stibnite | Sb2S3 |
Au | Gold | |
Au | ⓘ Gold | Au |
Other Databases
Link to USGS - Alaska: | WI113 |
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Other Regions, Features and Areas containing this locality
North America
- Brooks RangeMountain Range
- Rocky MountainsMountain Range
North America PlateTectonic Plate
- Brooks Range DomainDomain
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