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Dry Gulch Mine, Goodnews Bay, Bethel Census Area, Alaska, USAi
Regional Level Types
Dry Gulch MineMine
Goodnews BayBay
Bethel Census AreaCensus Area
AlaskaState
USACountry

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PhotosMapsSearch
Latitude & Longitude (WGS84):
58° 55' 12'' North , 161° 44' 24'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Goodnews Bay256 (2017)23.8km
Mindat Locality ID:
197274
Long-form identifier:
mindat:1:2:197274:3
GUID (UUID V4):
dfc661f1-683f-4435-aa33-4e256802c7f0


Location: Dry Gulch is a small north tributary to Platinum Creek (HG014). Dry Gulch is between Fox Gulch and Squirrel Creek and its confluence with Platinum Creek is about 1 mile upstream of the mouth of Platinum Creek. The map site is at the approximate midpoint of placer tailings in the drainage. It is included in locality 12 of Cobb (1972 [MF 362]; 1980 [OF 80-909]).
Geology: The headwaters of Dry Gulch are in the southeast border zone of the Red Mountain ultramafic pluton, where clinopyroxenite and hornblende-bearing rocks are dominant (Alaska Earth Sciences, 2000). Dry Gulch is only about 1/2 mile long, and placer tailings are present along about 1/4 mile of its lower length. Small-scale mining took place as early as 1927 or 1928, and continued intermittently until 1934, when the Goodnews Bay Mining Company started larger-scale dragline operations in the area (Mertie, 1940; 1976). The placer deposit probably has general characteristics like those on nearby Platinum Creek (HG014) and Fox Gulch (HG028). Locally derived gravels were coarse and bouldery, up to 12 feet thick but thinning upstream; PGMs were concentrated on or near bedrock. Bedrock along the mined part of Dry Gulch is part of an assemblage that includes sheared argillite, graywacke, and mafic to intermediate, fine-grained igneous rocks that are difficult to identify because of their decomposed character where exposed in mining cuts (Mertie, 1940). These rocks are included in a regional sedimentary and volcanic assemblage that ranges in age from Paleozoic to Mesozoic (Hoare and Coonrad, 1978). Platinum in Dry Gulch was probably discovered at about the same time that mining started on Platinum Creek (1928, Mertie, 1940). Dry Gulch was probably worked out by 1941.
Workings: Placer tailings are present along about 1/4 mile of lower Dry Gulch. Small-scale mining took place as early as 1927 or 1928 and continued intermittently until 1934, when the Goodnews Bay Mining Company started larger-scale dragline operations in the area (Mertie, 1940). Dry Gulch was probably worked out by 1941.
Age: Quaternary.

Commodities (Major) - PGM; (Minor) - Au
Development Status: Yes; small
Deposit Model: Placer PGE-Au (Cox and Singer, 1986; model 39b)

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


5 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
Gold1.AA.05Au
Platinum1.AF.10Pt
Group 4 - Oxides and Hydroxides
Chromite4.BB.05Fe2+Cr3+2O4
Magnetite4.BB.05Fe2+Fe3+2O4
Ilmenite4.CB.05Fe2+TiO3

List of minerals for each chemical element

OOxygen
O ChromiteFe2+Cr23+O4
O IlmeniteFe2+TiO3
O MagnetiteFe2+Fe23+O4
TiTitanium
Ti IlmeniteFe2+TiO3
CrChromium
Cr ChromiteFe2+Cr23+O4
FeIron
Fe ChromiteFe2+Cr23+O4
Fe IlmeniteFe2+TiO3
Fe MagnetiteFe2+Fe23+O4
PtPlatinum
Pt PlatinumPt
AuGold
Au GoldAu

Other Databases

Link to USGS - Alaska:HG027

Other Regions, Features and Areas containing this locality


This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.

References

 
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