Wiehl Mountain

The Wiehl Mountain is a antimony mine located in Alaska.

About the MRDS Data:

All mine locations were obtained from the USGS Mineral Resources Data System. The locations and other information in this database have not been verified for accuracy. It should be assumed that all mines are on private property.

Mine Info

Name: Wiehl Mountain

State:  Alaska

County:  na

Elevation:

Commodity: Antimony

Lat, Long: 67.62, -149.64000

Map: View on Google Maps

Satelite View

MRDS mine locations are often very general, and in some cases are incorrect. Some mine remains have been covered or removed by modern industrial activity or by development of things like housing. The satellite view offers a quick glimpse as to whether the MRDS location corresponds to visible mine remains.


Satelite image of the Wiehl Mountain

Wiehl Mountain MRDS details

Site Name

Primary: Wiehl Mountain


Commodity

Primary: Antimony
Secondary: Iron


Location

State: Alaska
District: Koyukuk


Land Status

Not available


Holdings

Not available


Workings

Not available


Ownership

Not available


Production

Not available


Deposit

Record Type: Site
Operation Category: Occurrence
Operation Type: Unknown
Years of Production:
Organization:
Significant:


Physiography

Not available


Mineral Deposit Model

Not available


Orebody

Not available


Structure

Not available


Alterations

Not available


Rocks

Not available


Analytical Data

Not available


Materials

Ore: Hematite
Ore: Pyrite
Ore: Stibnite


Comments

Comment (Exploration): Status = Inactive

Comment (Deposit): Other Comments = Possibly related to quartz-stibnite veins at Sukakpak Mountain (CH076).

Comment (Geology): Geologic Description = This occurrence is described as a vein containing fine-grained pyrite, hematite, and possibly a little stibnite in a carbonate gangue (Dillon, 1982). No other descriptive information is available for this occurrence. The country rocks near the occurrence are Devonian to Silurian(?) marble overlying and in fault contact with Ordovician black phyllite and marble and Ordovician to Cambrian(?) marble (Dillon and Reifenstuhl, 1995). The host for the mineralization was not specified.

Comment (Reference): Primary Reference = Dillon, 1982


References

Reference (Deposit): Dillon, J.T., 1982, Source of lode and placer gold deposits of the Chandalar and upper Koyukuk Districts: Alaska Division of Geological and Geophysical Surveys Open-File Report 158, 25 p., 1 sheet, scale 1:250,000.


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