The Yakutat Beach is a iron, titanium, and 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
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Yakutat Beach MRDS details
Site Name
Primary: Yakutat Beach
Commodity
Primary: Iron
Primary: Titanium
Primary: Gold
Secondary: Garnet
Secondary: Zirconium
Secondary: Tungsten
Secondary: PGE
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: Past Producer
Operation Type: Unknown
Years of Production:
Organization:
Significant:
Physiography
Not available
Mineral Deposit Model
Model Name: Placer Au-PGE
Orebody
Not available
Structure
Not available
Alterations
Not available
Rocks
Not available
Analytical Data
Not available
Materials
Ore: Ilmenite
Ore: Magnetite
Ore: Rutile
Ore: Scheelite
Ore: Zircon
Gangue: Sphene
Gangue: Pyroxene
Gangue: Pyrite
Gangue: Hornblende
Gangue: Garnet
Gangue: Topaz
Comments
Comment (Geology): Geologic Description = The Yakutat beach is developed on a wide band of unconsolidated sediments of Holocene age (MacKevett and Plafker, 1970; Foley and others, 1995; Wright, 1969; Wright, 1972). The deposit consists of transient modern beach concentrations and somewhat older and more stable layers and lenses of materials relatively rich in heavy minerals in the upland beach. Although less well known than some of the other Gulf of Alaska beaches (for example, Yakataga), the Yakutat beach is enriched in economic heavy minerals (ilmenite + zircon + rutile) relative to the Yakataga and Mt. Fairweather beaches studied by the U. S. Bureau of Mines (Foley and others, 1995). The Yakutat beach is the northwestward continuation of the Situk and Blacksand beach deposits. Potentially productive segments of the beach consist mainly of medium coarse sand in relatively continuous layers as much as several feet thick.Native gold, platinum minerals, rutile, and scheelite occur locally in concentrates. Foley and others (1995) estimate about 3.4 percent total economic heavy minerals (ilmenite + rutile + zircon) in a prism averaging about 5.5 meters thick that extends for several kilometers along the coast. These investigators found gold in more than 10 percent of their samples of heavy- mineral concentrates. Thomas and Berryhill (1962) reported about 35 pounds of iron per cubic yard of material in their samples from the Yakutat beach.
Comment (Geology): Age = Holocene
Comment (Deposit): Model Name = Beach placer: heavy-mineral ilmenite-rich. Characterized by small amounts of gold and PGEs. High energy beach processes.
Comment (Reserve-Resource): Reserves = also investigated recovery of gold and PGEs by flotation.
Comment (Reference): Primary Reference = Foley and others, 1995; Thomas and Berryhill, 1962.
Comment (Deposit): Other Comments = The Yakutat beach deposits are a significant resource of ilmenite-based titanium and associated other metals. Titanium mainly occurs in iron-rich minerals that probably were derived mostly from mafic-ultramafic rocks, not the metamorphic terranes that are the hosts of high-grade titanium (rutile) deposits. The placer deposits are essentially lag deposits produced in a young, high-energy environment (Foley and others, 1995, p. 56). The Yakutat area is within the Tongass National Forest and probably could be developed.
Comment (Reserve-Resource): Reserves = The beaches at Yakutat are broader than those in the Cape Yakataga area. Including a very small part of the Situk beach, Foley and others (1995, p. 56) assumed a wedge-shaped prism 0 to 11 meters deep, averaging 300 meters wide for a linear distance of 24 km down the coast. This prism contains 36 million cubic meters of beach sand, or approximately 57 million tonnes of sand. This mass contains from about 0.2 to 14.8 percent valuable heavy minerals (ilmenite + zircon + rutile) and averages about 3.4 percent valuable heavy metals.. Somewhat more than 10 percent of the samples collected by Foley and others contained gold, detected either in head samples or in spiral concentrates. The minimum limit of detection for gold in Foley's investigation was 0.028 grams/tonne (ppm).. Thomas and Berryhill (1962) reported about 35 pounds of iron, 20.5 pounds of titania and traces of gold and scheelite in the Yakutat and closely related beaches.. Foley and others (1995, table 3)
Comment (Production): Production Notes = Some gold has probably been recovered from the area.
Comment (Workings): Workings / Exploration = The Yakutat beach has been extensively explored by the U.S. Bureau of Mines (Thomas and Berryhill, 1962; Foley and others, 1995) using hand and powered augers and excavation. Foley and others collected 213 samples (nos. 164-258) from the Yakutat beach as defined here. (Samples nos. 242-245 were collected on Tawah creek, a tributary to Lost Creek.) The two studies by the Bureau complement each other. The report by Thomas and Berryhill (1962) contains some data on scheelite and other trace minerals not given by Foley. Foley and his coinvestigators worked especially on total economic heavy metal minerals--ilmenite + zircon + rutile. Data on gold and platinum group minerals were gathered as part of the broader investigation and are not quantitative. Both gold and platinum metals would be recovered in a large-scale placer mining operation for titanium and zircon at Yakutat. Reconnaissance-type samples were collected by MacKevett and Plafker (1970) and Reimnitz and Plafker (1976) of the U.S. Geological Survey.
References
Reference (Deposit): MacKevett, E.M., Jr., and Plafker, G., 1970, Geochemical and geophysical reconnaissance of parts of the Yakutat and Mount St. Elias quadrangles, Alaska: U.S. Geological Survey Bulletin 1312-L, 12 p.
Reference (Deposit): Cobb, E.H., 1972, Metallic mineral resources map of the Yakutat quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-408, 1 sheet, scale 1:250,000.
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): Cobb, E.H., 1979, Summary of references to mineral occurrences (other than mineral fuels and construction materials) in the Bering Glacier, Icy Bay, Middleton Island, and Yakutat quadrangles, Alaska: U.S. Geological Survey Open-File Report 79-1246, 41 p.
Reference (Deposit): Reimnitz, Erk, and Plafker, George, 1976, Marine gold placers along the Gulf of Alaska margin: U.S. Geological Survey Bulletin 1415, 16 p.
Reference (Deposit): Wright, F.F., 1969, Sedimentation and gold distribution, Yakutat Bay, Alaska: University of Alaska Marine Science Report R69-9, 12p.
Reference (Deposit): Wright, F.F., 1972, Marine geology of Yakutat Bay, Alaska: U.S. Geological Survey Professional Paper 800-B, p. B9-B15.
Reference (Deposit): Thomas, B.I., and Berryhill, R. V., 1962, Reconnaissance studies of Alaskan beach sands, eastern Gulf of Alaska: U.S. Bureau of Mines Report of Investigations 5986, 40 p.
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