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Unnamed Occurrence (ARDF - SM035; east of upper Bear Creek), Aniak Mining District, Bethel Census Area, Alaska, USAi
Regional Level Types
Unnamed Occurrence (ARDF - SM035; east of upper Bear Creek)- not defined -
Aniak Mining DistrictMining District
Bethel Census AreaCensus Area
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
61° 38' 37'' North , 158° 29' 2'' West
Latitude & Longitude (decimal):
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Crooked Creek105 (2016)31.9km
Mindat Locality ID:
201635
Long-form identifier:
mindat:1:2:201635:4
GUID (UUID V4):
0


Location: This occurrence is on a west-facing slope about 0.5 mile west of hill 1379. It is at an elevation of about 750 feet in the SW1/4 sec. 14, T. 18 N., R. 51 W., of the Seward Meridian. The location is accurate.
Geology: This occurrence consists of a chalcedony-cemented breccia in a flow of fine-grained, dark gray basalt or basaltic andesite (Bundtzen and others, 1998). The breccia contains 1-2 percent, finely disseminated sulfides in both quartz veinlets and in mafic volcanic rock. One grab sample contained 880 parts per billion gold and 200 parts per million chromium (Bundtzen and others, 1998). The elevated chromium probably represent the background of the host rocks.
Workings: Surface sampling was conducted by the Alaska Division of Geological and Geophysical Surveys in 1992 (Bundtzen and others, 1998).
Alteration: Chalcedony.

Commodities (Major) - Au; (Minor) - Cr
Development Status: None

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


1 valid mineral.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 4 - Oxides and Hydroxides
ⓘQuartz4.DA.05SiO2

List of minerals for each chemical element

OOxygen
Oⓘ QuartzSiO2
SiSilicon
Siⓘ QuartzSiO2

Other Databases

Link to USGS - Alaska:SM035

Other Regions, Features and Areas containing this locality


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