Vote for your favorite mineral in #MinCup26! - Quartz vs. Asagiite
It's a classic vs a newbie as the most common named mineral in the crust Quartz is up against an exceedingly-rare sea foam-green mineral discovered just a few years ago Asagiite.
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Kapon Creek Mine, Bethel Mining District, Bethel Census Area, Alaska, USAi
Regional Level Types
Kapon Creek MineMine
Bethel Mining DistrictMining District
Bethel Census AreaCensus Area
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
60° 6' 35'' North , 160° 9' 36'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Mindat Locality ID:
198305
Long-form identifier:
mindat:1:2:198305:3
GUID (UUID V4):
0


Location: Kapon Creek is an east tributary to the Eek River. The mouth of Kapon Creek is 9.5 miles downstream of the mouth of Rainy Creek (BH002) on the Eek River. This placer mine was referred to under the name 'Kapon Ck.' by Hoare and Cobb (1977). The map site is in the SE1/4 of section 6, T 1 S, R 63 W, of the Seward Meridian. It is approximately located, perhaps within miles, as the headwaters of this creek are about 4 miles further upstream from the map site.
Geology: Placer gold mining along Kapon Creek is reported to have taken place in 1914 and 1915 (Hoare and Cobb, 1977, p. 18). The lower part of the creek is in a glaciated area of outwash deposits. The upper reaches don't appear to have been occupied by glaciers but some outwash deposits may be present. The extreme headwaters of Kapon Creek are across a narrow saddle from the headwaters of Rainy Creek (BH002), where lode cinnabar mineralization has been identified (BH001). Coarse gravels in Kapon Creek were gound sluiced in 1914 and found to be of low grade (Maddren, 1915, p. 357). The gold was dark and flaky and accompanied by magnetite, arsenopyrite, and small cinnabar pebbles. Bedrock in the Kapon Creek drainage is clastic sedimentary rocks of the mid-Cretaceous Kuskokwim Group locally cut by felsic and mafic dikes (Hoare and Cobb, 1977; Box and others, 1993).
Workings: Kapon Creek has been prospected and some small surface workings are probably present locally along the creek.
Age: Quaternary.

Commodities (Major) - Au, Hg
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


4 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
Native Gold1.AA.05Au
Group 2 - Sulphides and Sulfosalts
Cinnabar2.CD.15aHgS
Arsenopyrite2.EB.20FeAsS
Group 4 - Oxides and Hydroxides
Magnetite4.BB.05Fe2+Fe3+2O4

List of minerals for each chemical element

OOxygen
O MagnetiteFe2+Fe23+O4
SSulfur
S ArsenopyriteFeAsS
S CinnabarHgS
FeIron
Fe ArsenopyriteFeAsS
Fe MagnetiteFe2+Fe23+O4
AsArsenic
As ArsenopyriteFeAsS
AuGold
Au Native GoldAu
HgMercury
Hg CinnabarHgS

Other Databases

Link to USGS - Alaska:BH020

Other Regions, Features and Areas containing this locality


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