Uranium 4 (in Selawik Hills)

The Uranium 4 (in Selawik Hills) is a uranium and thorium 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: Uranium 4 (in Selawik Hills)

State:  Alaska

County:  na

Elevation:

Commodity: Uranium, Thorium

Lat, Long: 66.15806, -160.21389

Map: View on Google Maps

Satelite View

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Satelite image of the Uranium 4 (in Selawik Hills)

Uranium 4 (in Selawik Hills) MRDS details

Site Name

Primary: Uranium 4 (in Selawik Hills)


Commodity

Primary: Uranium
Primary: Thorium


Location

State: Alaska
District: Selawik


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

Alteration Type: L
Alteration Text: Biotization.


Rocks

Not available


Analytical Data

Not available


Materials

Ore: Xenotime


Comments

Comment (Deposit): Model Name = Radioactive shear zone in alkaline igneous complex.

Comment (Workings): Workings / Exploration = A grab sample from this site was analyzed by the U.S. Bureau of Mines (Barker, 1985).

Comment (Reference): Primary Reference = Barker, 1985

Comment (Geology): Geologic Description = The country rock in the area of this occurrence is the mid-Cretaceous Selawik Hills alkaline intrusive complex. The occurrence is one of several areas of anomalous radioactivity within the complex. According to Barker (1985), at location I, quartz veinlets associated with lineaments tentatively identified as shear zones cut foliated syenite and monzonite. The syenite and monzonite have been partially replaced by silica and chlorite. The margins of the presumed shear zones are more intensely altered and are host to quartz veinlets up to 0.5 inch thick. Accessory xenotime was observed in a thin section of this rock. Secondary biotite is locally present. Grab sample 59R, from the biotite alteration, contained 220 ppm U3O8 and 36 ppm Th. Radiometric readings over the presumed shear zones were 1.5 to 2 times background.

Comment (Geology): Age = Cretaceous.

Comment (Exploration): Status = Inactive


References

Reference (Deposit): Barker, J.C., 1985, Sampling and analytical results of a mineral reconnaissance in the Selawik Hills area, northwestern Alaska: U.S. Bureau of Mines Open-File Report 43-85, 67 p.


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