Olsen Tunnel

The Olsen Tunnel 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: Olsen Tunnel

State:  Alaska

County:  na

Elevation:

Commodity: Antimony

Lat, Long: 64.57722, -165.40000

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 Olsen Tunnel

Olsen Tunnel MRDS details

Site Name

Primary: Olsen Tunnel


Commodity

Primary: Antimony
Secondary: Silver
Secondary: Gold


Location

State: Alaska


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: N
Deposit Size: S


Physiography

Not available


Mineral Deposit Model

Not available


Orebody

Not available


Structure

Not available


Alterations

Not available


Rocks

Name: Schist
Role: Host
Age Type: Host Rock Unit
Age Young: Late Permian


Analytical Data

Analytical Data: 50% SB, $21.60/TON IN AU, $2.05/TON IN AG, 1916 PRICES, USGS BULLETIN 662, P. 430.


Materials

Ore: Gold
Ore: Stibnite
Gangue: Quartz


Comments

Comment (Deposit): SEE ALSO: OLSEN PROSPECT ; INFO.SRC : 1 PUB LIT; 2 UNPUB REPT

Comment (Location): ABOUT 800 FT DOWNSTREAM (ALONG ANVIL CR.) FROM MCINTOSH PROSPECT (NEAR BOUTH OF QUARTZ GULCH). LAND STATUS VALUE CALCULATED 6-94 USING GIS OVERLAY ANALYSIS WITH BLM 1:2,500,000 SCALE OWNERSHIP STATUS MAP (1991).

Comment (Development): ACTIVE BEFORE 1916.

Comment (Deposit): QUARTZ STRINGERS AND STIBNITE OCCUR ALONG E-TRENDING FAULT IN SCHIST.

Comment (Workings): EXPLORED BY OPEN CUT AND SHORT TUNNEL.


References

Reference (Deposit): USGS BULLETIN 662, P. 430.

Reference (Other Database): BAG-MF-463-48


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