Unnamed (Brady Glacier outwash)

The Unnamed (Brady Glacier outwash) is a gold, titanium, and zirconium 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: Unnamed (Brady Glacier outwash)  

State:  Alaska

County:  na

Elevation:

Commodity: Gold, Titanium, Zirconium

Lat, Long: 58.35, -136.61000

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 Unnamed (Brady Glacier outwash)

Unnamed (Brady Glacier outwash) MRDS details

Site Name

Primary: Unnamed (Brady Glacier outwash)


Commodity

Primary: Gold
Primary: Titanium
Primary: Zirconium
Secondary: PGE


Location

State: Alaska
District: Juneau


Land Status

Not available


Holdings

Not available


Workings

Not available


Ownership

Not available


Production

Not available


Deposit

Record Type: Site
Operation Category: Past Producer
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

Name: Till
Role: Host
Age Type: Host Rock
Age Young: Holocene


Analytical Data

Not available


Materials

Ore: Ilmenite
Ore: Zircon
Ore: Gold


Comments

Comment (Workings): Workings / Exploration = Small, transient placers on the outwash plain were worked during the early years of the twentieth century (Rossman, 1963, B 1121-K, p. K51-52). The U.S. Bureau of Mines (Kimball and others, 1978, p. C126) detected gold content in stream-sediment-type samples of up to 0.15 ppm (0.004 oz/ton) along with traces of silver, copper, cobalt, and nickel. The gold is extremely fine-grained, but local concentrations could have been rich. The gold is so fine that recovery is difficult.? Foley and others (1995, sample no. 319) determined that ilmenite (titanium) and zircon (zirconium) were present in one sample in anomalous amounts. The sample contained 4.95 percent and 6.15 percent titanium, respectively, in a head split and a spiral concentrate. Zirconium was reported as 720 ppm in the head split and 1084 ppm in the spiral concentrate.

Comment (Exploration): Status = Inactive

Comment (Commodity): Ore Material = Gold (native)

Comment (Commodity): Ore Material = Gold (native)

Comment (Commodity): Ore Material = PGE

Comment (Geology): Geologic Description = Brady Glacier occupies a major north-northwest-aligned boundary between Paleozoic strata intruded by granitic rocks of Cretaceous age on the east and rocks of Cretaceous and Tertiary age to the west (Brew and others, 1978). The Brady Glacier nickel-copper deposit (MF003) is in the western province and within the drainage basin of the glacier. Glacial erosion of the sulfide and oxide deposits of the Crillon-LaPerouse layered mafic intrusion, the host of the Brady Glacier deposit, would furnish titanium and PGEs to the glacial outflow. Gold deposits similar to the LeRoy mine (MF022) could exist in the Cretaceous rocks in the eastern terrane.? Gold, in extremely fine-grained form, ilmenite, PGEs, and zircon locally are concentrated in transient placers at the front of the glacier.? Placer samples collected from the outwash fan by the U.S. Bureau of Mines contained as much as 0.15 ppm gold (Kimball and others, 1978) and 6.15 percent titanium (Foley and others,1995).

Comment (Deposit): Model Name = Placer: Low-grade glacial outwash reworked on tidal flat.

Comment (Deposit): Other Comments = the placer sites are in Glacier Bay National Park and Preserve.

Comment (Reference): Primary Reference = Kimball and others, 1978

Comment (Geology): Age = Holocene.


References

Reference (Deposit): Foley, J.Y., La Berge, R.D., Grosz, A.E., Oliver, F.S., and Hirt, W.C., 1995, Onshore titanium and related heavy mineral investigations in the eastern Gulf of Alaska region, southern Alaska: U.S. Bureau of Mines Open-File Report 10-95, 125 p.

Reference (Deposit): Rossman, Darwin, 1963, Geology of the eastern part of the Mount Fairweather quadrangle, Glacier Bay, Alaska: U.S. Geological Survey Bulletin 1121-K, p. K1-K57.

Reference (Deposit): MacKevett, E.M., Jr., Brew, D.A., Hawley, C.C., Huff, L.C., and Smith, J.G., 1971, Mineral resources of Glacier Bay National Monument, Alaska: U.S. Geological Survey Professional Paper 632, 90 p., 12 plates, scale 1:250,000.

Reference (Deposit): Kimball, A.L., Still, J.C., and Rataj, J.L., 1978, Mineral resources, in Brew, D. A., and others, Mineral resources of the Glacier Bay National Monument wilderness study area, Alaska: U.S. Geological Survey Open-File Report 78-494, p. C1-C375.

Reference (Deposit): Brew, D.A., Johnson, B.R., Grybeck, D., Griscom, A., Barnes, D.F., Kimball, A.L., Still, J.C., and Rataj, J.L., 1978, Mineral resources of the Glacier Bay National Monument Wilderness Study Area, Alaska: U.S. Geological Survey Open-File Report 78-494, 670 p.

Reference (Deposit): Cobb, E.H., 1972, Metallic mineral resources map of the Mount Fairweather quadrangle, AK: U.S. Geological Survey Miscellaneous Field Study Map MF-436, 1 sheet, scale 1:250,000.


The Top Ten Gold Producing States

The Top Ten Gold Producing States

These ten states contributed the most to the gold production that built the West from 1848 through the 1930s. The Top Ten Gold Producing States.