The Unnamed (north of Mt. Marchainville) is a titanium and iron 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
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Unnamed (north of Mt. Marchainville) MRDS details
Site Name
Primary: Unnamed (north of Mt. Marchainville)
Commodity
Primary: Titanium
Primary: Iron
Secondary: Nickel
Secondary: Copper
Location
State: Alaska
District: Yakutat
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: Conspicuous secondary iron-staining.
Rocks
Not available
Analytical Data
Not available
Materials
Ore: Pyrrhotite
Ore: Magnetite
Ore: Ilmenite
Ore: Chalcopyrite
Comments
Comment (Reference): Primary Reference = MacKevett and others, 1971
Comment (Workings): Workings / Exploration = Surface exposures only; knowledge is partly based on aircraft fly-by because of the extremely rough topography.
Comment (Geology): Age = Tertiary.
Comment (Geology): Geologic Description = Ilmenite and magnetite, accompanied by subordinate chalcopyrite and pyrrhotite, occur in heavily iron-stained masses near the south contact of the Crillon-LaPerouse layered mafic-ultramafic intrusion (Brew and others, 1978). The layered intrusive was emplaced in rocks of the Chugach terrane (Berg and others, 1972). The first reports of the occurrences were by Rossman (1963, B 1121-F); further reports were made by MacKevett and others (1971, p. 72-73) and Kimball and others (1978, p. C112).
Comment (Deposit): Other Comments = the occurrences are in extremely rugged country in the south part of the Crillon-LaPerouse intrusion in Glacier Bay National Park and Preserve.
Comment (Deposit): Model Name = Heavy-mineral segregations near basal contact of synorogenic layered mafic intrusive of Tertiary age (Foley and others, 1997).
References
Reference (Deposit): Foley, J.Y., Light, T.D., Nelson, S.W., and Harris, R.A., 1997, Mineral occurrences associated with mafic-ultramafic and related alkaline complexes in Alaska: Economic Geology, Monograph 9, p. 396-449.
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): 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): 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): 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): Berg, H.C., Jones, D. L., and Richter, D. H., 1972, Gravina-Nutzotin Belt-tectonic significance of an Upper Mesozoic sedimentary and volcanic sequence in southern and southeastern Alaska: U.S. Geological Survey Professional Paper 800-D, p. D1-D24.
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