Gold King Creek Mine, Bonnifield Mining District, Denali Borough, Alaska, USAi
Regional Level Types | |
---|---|
Gold King Creek Mine | Mine |
Bonnifield Mining District | Mining District |
Denali Borough | Borough |
Alaska | State |
USA | Country |
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Latitude & Longitude (WGS84):
64° 4' 26'' North , 148° 0' 14'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Mindat Locality ID:
197688
Long-form identifier:
mindat:1:2:197688:8
GUID (UUID V4):
2d19e9bb-6d02-462d-85f8-dff36a4456e6
Location: The Gold King Creek mine is mostly in sec. 6, T. 10 S., R. 2 W., Fairbanks Meridian. Gold King Creek is a north-flowing tributary of the Wood River. The mine is localities 80, 81, and 82 of Cobb (1972 [MF 410]).
Geology: In 1990 and 1991, Gold King Creek was the largest placer mine in the district (Swainbank and others, 1991, p. 31; Bundtzen and others, 1991, p. 34). Gold is believed to be derived from the Tertiary Nenana Gravel (Bundtzen and others, 1991, p. 34). Placer gold is found in both the 4 to 5 feet of gravel overlying bedrock and on the clay-rich bedrock (Prindle, 1907, p. 212). Mining took place intermittently from 1903 to 1940 (Cobb, 1976 [OFR 76-662, p. 44]). In the 1920's, an attempt at large-scale hydraulic mining of Nenana Gravel was not financially successful (Capps, 1924, p. 138). The gold varies from 818 to 833 fine (Glover, 1950).
Workings: In 1990 and 1991, Gold King Creek was the largest placer mine in the district; it operated under the direction of Warren Taylor and Alaska Unlimited Inc. (Swainbank and others, 1991, p. 31; Bundtzen and others, 1991, p. 34). Mining from 1903 to 1916 was done by open-cut, pick-and-shovel methods and continued intermittently until 1940 (Maddren, 1918, p. 401). In 1924, a hydraulic operation was active in gravels 6 to 7 feet in depth (Wimmler, 1924, p. 43). An attempt at large-scale hydraulic mining of the Nenana Gravel was not financially successful (Capps, 1924, p. 138). This failed attempt consisted of 11 miles of ditches designed to convey 3,000 miner's inches of water from the upper part of Gold King Creek to a point on the eastern slopes of the valley, where it was to be delivered to a pipeline with a head of 700 feet (Maddren, 1918, p. 401).
Age: Quaternary placer.
Production: Information on gold production is not available.
Commodities (Major) - Au; (Minor) - W
Development Status: Yes; small
Deposit Model: Placer Au (Cox and Singer, 1986; model 39a)
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsCommodity 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 | |||
---|---|---|---|
ⓘ | Gold | 1.AA.05 | Au |
Group 7 - Sulphates, Chromates, Molybdates and Tungstates | |||
ⓘ | Scheelite | 7.GA.05 | Ca(WO4) |
List of minerals for each chemical element
O | Oxygen | |
---|---|---|
O | ⓘ Scheelite | Ca(WO4) |
Ca | Calcium | |
Ca | ⓘ Scheelite | Ca(WO4) |
W | Tungsten | |
W | ⓘ Scheelite | Ca(WO4) |
Au | Gold | |
Au | ⓘ Gold | Au |
Other Databases
Link to USGS - Alaska: | FB148 |
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Other Regions, Features and Areas containing this locality
North America PlateTectonic Plate
- Nenana BasinBasin
- Yukon-Tanana lower DomainDomain
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