Tatlawiksuk Springs

The Tatlawiksuk Springs 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: Tatlawiksuk Springs  

State:  Alaska

County:  na

Elevation:

Commodity: Gold

Lat, Long: 62.043, -155.76300

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 Tatlawiksuk Springs

Tatlawiksuk Springs MRDS details

Site Name

Primary: Tatlawiksuk Springs


Commodity

Primary: Gold
Secondary: Silver


Location

State: Alaska
District: McGrath


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

Model Name: Hot-spring Au-Ag


Orebody

Not available


Structure

Not available


Alterations

Alteration Type: L
Alteration Text: Siliceous sinter.


Rocks

Not available


Analytical Data

Not available


Materials

Ore: Gold


Comments

Comment (Geology): Geologic Description = Bundtzen and others (1991) first described Tatlawiksuk Hot Springs, a newly discovered geothermal system in western Alaska. Tatlawiksuk Hot Springs is a fairly alkaline, low-chlorine, sodium bicarbonate spring that is comparable to other Alaskan hot springs related to faulted granitic pluton-sedimentary rock contact zones. The four recognized Tatlawiksuk springs emit hot waters that reach a maximum temperature of 68 degrees Celsius; the springs plumbing system exhibits a north-south alignment parallel to high-angle faults mapped in the area (Bundtzen and others, 1991; Wilson and others, 1998). During State Land Selection resource investigations conducted by the reporter in 1992 (Division of Geological and Geophysical Surveys Staff, 1993), several grains of placer gold were detected in sinterous material at the northern end of the spring system.

Comment (Deposit): Model Name = Hot Springs gold-silver(?) (Cox and Singer, 1986; model 25a).

Comment (Workings): Workings / Exploration = During State Land Selection resource investigations conducted by the reporter in 1992 (Division of Geological and Geophysical Surveys Staff, 1993), several grains of placer gold were detected in sinterous material at the northern end of the spring system.

Comment (Geology): Age = Quaternary.

Comment (Reference): Primary Reference = Bundtzen and others, 1991

Comment (Exploration): Status = Inactive


References

Reference (Deposit): Bundtzen, T.K., Liss, S.E., and Harris, E.E., 1991, Geology and geochemistry of the Tatlawiksuk Hot Springs, a newly discovered geothermal area in western Alaska, in Reger, R.D., ed., Short Notes on Alaska Geology 1991: Alaska Division of Geological and Geophysical Surveys Professional Report 111, p. 21-27.

Reference (Deposit): Wilson, F.H., Dover, J.H., Bradley, D.C., Weber, F.R., Bundtzen, T.K., and Haeussler, P.J., 1998, Geologic map of central (interior) Alaska: U.S. Geological Survey Open-File Report 98-133, 17 p., 2 sheetsm, scale 1:500,000.


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