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Archibald Creek; Archibald Gulch Mine, Koyukuk Mining District, Yukon-Koyukuk Census Area, Alaska, USAi
Regional Level Types
Archibald Creek; Archibald Gulch MineMine
Koyukuk Mining DistrictMining District
Yukon-Koyukuk Census AreaCensus Area
AlaskaState
USACountry

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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 Elements

Mineral List


2 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
Gold1.AA.05Au
Group 2 - Sulphides and Sulfosalts
Stibnite2.DB.05Sb2S3

List of minerals for each chemical element

SSulfur
S StibniteSb2S3
SbAntimony
Sb StibniteSb2S3
AuGold
Au GoldAu

Other Databases

Link to USGS - Alaska:WI113

Other Regions, Features and Areas containing this locality

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North America PlateTectonic Plate

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References

Armstrong, E., 1985, The placer geology of the Wiseman area, in Walsh, D.E.,and Wray, M.S., eds., 1985, Sixth Annual Conference on Alaskan Placer Mining: March 28-29, 1984, Fairbanks, Alaska: Mineral Industry Research Laboratory Report 69, 77 p. Bundtzen, T.K., Eakins, G.R., Clough, J.G., Lueck, L.L., Green, C.B., Robinson, M.S., and Coleman, D.A., 1984, Alaska's mineral industry, 1983: Alaska Division of Geological and Geophysical Surveys Special Report 33, 56 p. Bundtzen, T.K., Eakins, G.R., Green, C.B., and Lueck, L.L., 1986, Alaska's mineral industry, 1985: Alaska Division of Geological and Geophysical Surveys Special Report 39, 68 p. Bundtzen, T.K., Green, C.B., Peterson, R.J., and Seward, A.F., 1988, Alaska's mineral industry, 1987: Alaska Division of Geological and Geophysical Surveys Special Report 41, 69 p. Bundtzen, T.K., Swainbank, R.C., Wood, J.E., Clough, A.H., 1991 (1992), Alaska's Mineral Industry 1991: Alaska Division of Geological & Geophysical Surveys, Special Report 46, 89 p. Dillon, J.T., 1982, Source of lode and placer gold deposits of the Chandalar and upper Koyukuk Districts: Alaska Division of Geological and Geophysical Surveys Open-File Report AOF-158, 25 p., 1 sheet, scale 1:250,000. Eakins, G.R., Bundtzen, T.K., Lueck, L.L. Green, C.B., Gallagher, J.L., and Robinson, M.S., 1985, Alaska mineral industry, 1984: Alaska Division of Geological and Geophysical Surveys Special Report 38, 57 p. Eakins, G.R., Bundtzen, T.K., Robinson, M.S., Clough, J.G., Green, C.B., Clautice, K.H., and Albanese M.A., 1983, Alaska's mineral industry, 1982: Alaska Division of Geological and Geophysical Surveys Special Report 31, 63 p. Ebbley, Norman, Jr., and Wright, W.S., 1948, Antimony deposits in Alaska: U.S. Bureau of Mines Report of Investigations 4173, 41 p. Eden, K., 2000, Geology and gold mineralization of the Nolan area in the Brooks Range, Alaska: U.S. Bureau of Land Management Open-File Report 78, 87 p. Heiner, L.E., and Wolff, E.N., ed
 
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