Wattamuse Creek (lode)

The Wattamuse Creek (lode) 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: Wattamuse Creek (lode)

State:  Alaska

County:  na

Elevation:

Commodity: Gold

Lat, Long: 59.345, -161.33200

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 Wattamuse Creek (lode)

Wattamuse Creek (lode) MRDS details

Site Name

Primary: Wattamuse Creek (lode)


Commodity

Primary: Gold
Secondary: Tungsten
Secondary: Mercury
Secondary: Antimony
Secondary: Silver


Location

State: Alaska
District: Goodnews Bay


Land Status

Not available


Holdings

Not available


Workings

Not available


Ownership

Not available


Production

Not available


Deposit

Record Type: Site
Operation Category: Prospect
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: Silicification.


Rocks

Role: Host
Age Type: Host Rock
Age in Years: 71.300000+-2.100000
Material Analyzed: Biotite
Age Young: Early Cretaceous


Analytical Data

Not available


Materials

Ore: Stibnite
Ore: Pyrrhotite
Ore: Pyrite
Ore: Gold
Ore: Chalcopyrite
Ore: Arsenopyrite
Gangue: Quartz


Comments

Comment (Exploration): Status = Active?

Comment (Geology): Geologic Description = An Upper Cretaceous granitic stock underlies the head of Granite and Wattamuse Creeks (Hoare and Coonrad, 1978). This granodiorite to diorite stock hosts 1 inch- to 1-foot-thick quartz veins containing arsenopyrite, stibnite, pyrite, and some chalcopyrite. A soil-geochemical grid over about a 1/4- by 1/2-mile area straddling the ridge crest showed large areas of soil containing more than 100 ppb gold, and several areas containing more than 1,000 ppb gold (Calista Corporation, unpublished data). Individual grab samples collected for Calista Corporation contain up to 9.5 ppm Au, 14.9 ppm Ag, 17 percent As, 22 percent Sb, and 1,500 ppm Hg (Fechner, 1988, p. 58). The U. S. Bureau of Mines collected 19 grab samples of rocks in the headwaters of Wattamuse Creek. One of these, a composite grab sample collected in this prospect area, assayed 2.18 ounces of gold per ton, 6.6 ppm Ag, 2,850 ppm As, 400 ppm Bi, 40 ppm Sb, and 184 ppm W (Fechner, 1988, p. 58). Grab samples of quartz veins contained 1.25 to 5.3 ppm Au. The country rocks to the granitic stock locally include mafic rocks; a sample of mafic rock containing arsenopyrite, pyrrhotite, and chalcopyrite assayed 17.4 ppm Ag, 3.3 ppm Au, 0.13 percent As, 30 ppm Bi, and 0.19 percent Cu (Fechner, 1988, p. 58).

Comment (Reference): Primary Reference = Fechner, 1988

Comment (Workings): Workings / Exploration = A soil geochemistry grid, selected rock sampling, and probably surface mapping has been completed on the prospect (Calista Corporation, unpublished data).

Comment (Deposit): Model Name = Granitic rock-hosted epithermal gold/silver

Comment (Geology): Age = Late Cretaceous or younger. A K/Ar age for the host granitic stock is 71.3 +/- 2.1 Ma on biotite (Hoare and Coonrad, 1978).


References

Reference (Deposit): Fechner, S.A., 1988, Bureau of Mines mineral investigation of the Goodnews Bay mining district, Alaska: U.S. Bureau of Mines Open-File Report 1-88, 230 p.

Reference (Deposit): Hoare, J.M., and Coonrad, W.L., 1978, Geologic map of the Goodnews and Hagemeister Island quadrangles region, southwestern Alaska: U.S. Geological Survey Open-File Report 78-9-B, two sheets, scale 1:250,000.


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