The Oakland Creek (formerly known as Diomede Creek) is a tin 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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Oakland Creek (formerly known as Diomede Creek) MRDS details
Site Name
Primary: Oakland Creek (formerly known as Diomede Creek)
Commodity
Primary: Tin
Location
State: Alaska
District: Port Clarence
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
Model Name: Alluvial placer Sn
Orebody
Not available
Structure
Not available
Alterations
Not available
Rocks
Not available
Analytical Data
Not available
Materials
Ore: Cassiterite
Comments
Comment (Geology): Age = Quaternary
Comment (Reference): Primary Reference = Heide and Rutledge, 1949
Comment (Reserve-Resource): Reserves = Not defined
Comment (Workings): Workings / Exploration = The USBM completed 17 churn-drill holes to bedrock along 4 lines spread out over 5,600 feet of the drainage length (Heide and Rutledge, 1949).
Comment (Deposit): Model Name = Alluvial tin placer (Cox and Singer, 1986; model 39e)
Comment (Exploration): Status = Inactive
Comment (Geology): Geologic Description = Bedrock in the headwaters of Oakland Creek is thermally metamorposed thin-bedded metapelite, metasandstone, and minor impure metacarbonate rocks of unknown but probable Paleozoic age. These rocks makeup the relatively resistant upland of Potato Mountain that is interpreted to be underlain at depth by biotite granite (Hudson and Reed, 1997, p. 454). Three to ten feet of overburden are present on gravels that locally reach 37 feet of thickness. The USBM churn-drill results are for pay sections on bedrock that are generally 1 to 6 feet thick but in two holes the gravel and pay thickness were both much greater (27 and 35 feet of pay in gravel sections 34 and 37 feet thick respectively). Tin concentrations between 0.04 and 0.24 pounds of tin per cubic yard were returned from 12 of 17 USBM churn-drill holes (Heide and Rutledge, 1949, p. 20). The tin concentrations are higher in lower parts of the sampled drainage (elevations estimated to be between 150 to 200 feet). This is close to where a Pleistocene strandline has been inferred from the geomorphic character of the area (Hudson and Reed, 1997, p. 454).
References
Reference (Deposit): Cobb, E.H., and Sainsbury, C.L., 1972, Metallic mineral resource map of the Teller quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-426, 1 sheet, scale 1:250,000.
Reference (Deposit): Cobb, E.H., 1975, Summary of references to mineral occurrences (other than mineral fuels and construction materials) in the Teller quadrangle, Alaska: U.S. Geological Survey Open-File Report 75-587, 130 p.
Reference (Deposit): Heide, H.E. and Rutledge, F.A., 1949, Investigations of Potato Mountain tin placer deposits, Seward Peninsula, northwestern Alaska: U.S. Bureau of Mines Report of Investigations 4418, 21 p.
Reference (Deposit): Hudson, T.L., and Reed, B.L., 1997, Tin deposits of Alaska, in Goldfarb, R.J., and Miller, L.D., eds., Mineral Deposits of Alaska: Economic Geology Monograph 9, p. 450-465.
Reference (Deposit): Sainsbury, C.L., 1972, Geologic map of the Teller quadrangle, Seward Peninsula, Alaska: U.S. Geological Survey Map I-685, 4 p., 1 sheet, scale 1:250,000.
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