Unnamed (west-northwest of Mt. Dagelet)

The Unnamed (west-northwest of Mt. Dagelet) is a titanium 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 (west-northwest of Mt. Dagelet)

State:  Alaska

County:  na

Elevation:

Commodity: Titanium

Lat, Long: 58.605, -137.26694

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 (west-northwest of Mt. Dagelet)

Unnamed (west-northwest of Mt. Dagelet) MRDS details

Site Name

Primary: Unnamed (west-northwest of Mt. Dagelet)


Commodity

Primary: Titanium


Location

State: Alaska
District: Glacier Bay


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: Bushveld Fe-Ti-V


Orebody

Not available


Structure

Not available


Alterations

Not available


Rocks

Not available


Analytical Data

Not available


Materials

Ore: Ilmenite


Comments

Comment (Deposit): Other Comments = the site is in Glacier Bay National Park and Preserve.

Comment (Deposit): Model Name = Possibly Bushveld Fe-Ti-V (Cox and Singer, 1986; model 3). Magmatic segregation; ilmenite deposit in layered mafic-ultramafic intrusive.

Comment (Reference): Primary Reference = Rossman, 1963 (B 1121-F)

Comment (Workings): Workings / Exploration = There are no workings. Sample 53ARm a37 contained 25 percent ilmenite (Rossman, 1963, p. F43).

Comment (Geology): Geologic Description = This occurrence consists of ilmenite segregations in the Crillon-La Perouse layered mafic-ultramafic intrusion, along its southwestern contact zone (Brew and others, 1978). The adjacent metamorphic rocks are hornblende and biotite schist probably derived from a Mesozoic protolith. The intrusion is of Tertiary age.? An ilmenite magmatic segregation deposit exists at the site. It continues along strike of the layered intrusion for several hundred feet but could not be traced farther because of extremely steep topography. At the site, the intrusion is estimated to contain from 10 to 25 percent ilmenite (Rossman, 1963, 1121-F). A sample that contained 25 percent ilmenite contained 2 percent graphite by weight.

Comment (Reserve-Resource): Reserves = An inferred resource could be calculated based on data given by Rossman.

Comment (Exploration): Status = Inactive

Comment (Geology): Age = Tertiary.


References

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): Rossman, Darwin, 1963, Geology and petrology of two stocks of layered gabbro in the Fairweather Range, Alaska: U.S. Geological Survey Bulletin 1121-F, p. F1-F50.

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.


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