Steese Highway

The Steese Highway is a gold 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: Steese Highway  

State:  Alaska

County:  na

Elevation:

Commodity: Gold

Lat, Long: 65.02, -147.48111

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 Steese Highway

Steese Highway MRDS details

Site Name

Primary: Steese Highway
Secondary: Mile 17.5


Commodity

Primary: Gold


Location

State: Alaska
District: Fairbanks


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: Gold


Comments

Comment (Exploration): Status = Inactive

Comment (Deposit): Model Name = Gold in altered quartz diorite adjacent to a quartz vein.

Comment (Geology): Geologic Description = The following is an excerpt from Forbes and others (1968):? 'A small pluton of quartz diorite is exposed in road cuts along the Steese Highway south of Granite Creek. The south border of the quartz diorite mass is strongly sheared, altered and iron-stained. Vein quartz, 0.5 feet thick, occurs in the gouge zone which trends N 87 W and dips steeply to the south. Gold values up to 2.70 ppm occur in the altered quartz diorite adjacent to the quartz vein, but decrease progressively away from the vein.'

Comment (Workings): Workings / Exploration = Surface samples taken.

Comment (Reference): Primary Reference = Forbes and others, 1968


References

Reference (Deposit): Forbes, R.B., Pilkington, H.D., and Hawkins, D.B., 1968, Gold gradients and anomalies in the Pedro Dome-Cleary Summit area, Fairbanks District, Alaska: U.S. Geological Survey Open-File Report 324, 43 p.

Reference (Deposit): Cobb, E.H., 1976, Summary of references to mineral occurrences (other than mineral fuels and construction materials) in the Circle quadrangle, Alaska: U.S. Geological Survey Open-File Report 76-633, 72 p.

Reference (Deposit): Cobb, E.H., 1976, Summary of references to mineral occurrences (other than mineral fuels and construction materials) in the Livengood quadrangle, Alaska: U.S. Geological Survey Open-File Report 76-819, 241 p.


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