Perry Creek Mine, Fairhaven Mining District, Northwest Arctic Borough, Alaska, USAi
| Regional Level Types | |
|---|---|
| Perry Creek Mine | Mine |
| Fairhaven Mining District | Mining District |
| Northwest Arctic Borough | Borough |
| Alaska | State |
| USA | Country |
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Latitude & Longitude (WGS84):
65° 49' 8'' North , 163° 5' 16'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Deering | 127 (2017) | 33.0km |
Location: Perry Creek is a southwest tributary to Pinnell River. Its mouth is about 5 miles upstream of the confluence of the Pinnell and Inmachuk Rivers. This location includes terrace gravels on both the north and south sides of Perry Creek overlooking Pinnell River. The terrace gravels are capped by basalt flows about 200 to 250 feet vertically above the Pinnell River. This is location 74 of Cobb (1972; MF 417; 1975; OFR 75-429).
Geology: This location includes terrace gravels on both the north and south sides of Perry Creek overlooking Pinnell River. The terrace gravels are capped by basalt flows about 200 to 250 feet vertically above the Pinnell River (Henshaw, 1910). One terrace sequence includes (bottom to top); 3 to 9 feet of gold-bearing gravel on schist bedrock, 20 feet of muck including wood fragments near the base (a 3 foot-diameter log is reported to have been encountered somewhere in the Perry Creek mine workings), 25 feet of basalt, an indeterminate thickness of nonauriferous gravel, and an indeterminate thickness of basalt (Hopkins, 1963, p. C32). Henshaw (1910) indicates that one terrace level is 52 feet higher than another in the area. The fine, bright gold here -- some nuggets worth $0.15 at $20/ounce -- was in quartz-rich gravel (Moffit, 1905). Most of the bedrock in the area is a metasedimentary schist and marble sequence of Lower Paleozoic age (Till and others, 1986). The basalt flows are part of the Pleistocene Imuruk Volcanics and the terrace gravels may be correlative with the Pliocene-Pleistocene Kougarok gravels (Hopkins, 1963).
Workings: These basalt-covered terrace gravels are old channels that required underground drift mining; the extent and nature of these workings are not known.
Age: Late Tertiary to Pleistocene; the age of the Kougarok gravels (Hopkins, 1963).
Commodities (Major) - Au
Development Status: Yes; small
Deposit Model: Placer Au-PGE (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
1 valid mineral.
Detailed Mineral List:
| ⓘ Native Gold Formula: Au |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 1 - Elements | |||
|---|---|---|---|
| ⓘ | Native Gold | 1.AA.05 | Au |
List of minerals for each chemical element
| Au | Gold | |
|---|---|---|
| Au | ⓘ Native Gold | Au |
Other Databases
| Link to USGS - Alaska: | BN062 |
|---|
Other Regions, Features and Areas containing this locality
North AmericaContinent
North America PlateTectonic Plate
- Brooks-Seward DomainDomain
- Nome ComplexAccretionary Complex
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