The Cape 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
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.
Cape Creek MRDS details
Site Name
Primary: Cape Creek
Secondary: American Tinfields, Inc.
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: Past Producer
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 (Reference): Primary Reference = Mulligan and Thorne, 1959; Hudson, 1984; Hudson and Reed, 1997..
Comment (Reserve-Resource): Reserves = Unkown but extensive mining took place in the 1970's and 1980's. Most of the placer deposits, especially the higher grade portions, are probably mined out (Bundzten and others, 1990, p. 33).
Comment (Workings): Workings / Exploration = A churn-drill exploration program defined both upper and lower pay streaks before larger scale mining (Mulligan and Thorne, 1959). Early mining was by hand in the west headwater. Power shovels were used later and the recovered pay was hauled by truck to the beach for washing. The latest mining used a dragline to remove overburden, a dozer to consolidate pay in the pit, and a front-end loader to transport pay to a nearby washing plant. Cassiterite-bearing concentrate was placed in 55 gallon barrels and transferred by crane to barges on the beach for transfer to a coastal freighter anchored nearby.
Comment (Exploration): Status = Inactive
Comment (Deposit): Model Name = Alluvial tin placer (Cox and Singer, 1986; model 39e)
Comment (Geology): Age = Quaternary
Comment (Production): Production Notes = Most of the recorded 1,650 short tons of tin production from the Cape Mountain area (Hudson and Reed, 1997, p. 452) has come from Cape Creek ; over 60% of the total production (1,036 tons) took place between 1979 and 1989 (Bundzten and others, 1990, p. 33). Goodwin Gulch, with between 132 and 650 tons of tin production, has been the only other significant placer source in this area.
Comment (Geology): Geologic Description = Cape Creek, the principal drainage on the east side of the Cape Mountain upland, has headwaters in the contact zone of the Late Cretaceous Cape Mountain biotite granite (Hudson and Arth, 1983) with Mississippian marble (Sainsbury, 1972). Private company and USBM churn-drill holes defined upper and lower pay sections along most of Cape Creek including the lower part of the east fork. The upper pay streak was related to the active stream drainage, did not have extensive overburden, and contained a few to several ponds of tin per cubic yard. The lower pay streak, separated from the upper by up to 65 feet of silt and minor sand containing marine shells, was 7 feet or less in thickness, developed on and adjacent to bedrock, and high grade in most places. Grades to over 30 pounds of tin per cubic yard were reported by Mulligan and Thorne (1959, p. 40). Mining during the 1970's and 1980's by Lost River Mining Company verified grades of about 30 pounds of tin per cubic yard over large parts of this pay streak (R. Murray, personal communication in Hudson and Reed, 1997, p. 451). Development of these high grades has been attributed to reworking during the marine transgression that flooded the area and led to the thick silt-rich marine section in Cape Creek (Hudson and Reed, 1997, p. 451-452). . Some of the detrital cassiterite is very coarse grained. Washing plant operations in 1982 included a 1.5 inch grizzley and hand picking of the oversize conveyor belt was required to collect coarse aggregates of cassiterite crystals. The largest cassiterite aggregate found in this way weighed 142 pounds (R. Murray, personal communication in Hudson, 1984, p. 8). Some of the cassiterite aggregates are an assemblage of cassiterite, muscovite, quartz, and feldspar (Hudson, 1984, p. 16). The character of this material is consistent with its derivation from lode deposits on slopes above the west headwater of Cape Creek (Mulligan and Thorne, 1959; Mulligan, 1966)
References
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): Mulligan, J.J., and Thorne, R.L., 1959, Tin-placer sampling methods and results, Cape Mountain district, Seward Peninsula, Alaska: U.S. Bureau of Mines Information Circular 7878, 69 p.
Reference (Deposit): Bundtzen, T.K., Swainbank, R.C., Deagen, J.R., Moore, J.L., 1990 (1991), Alaska's Mineral Industry 1989: Alaska Division of Geological & Geophysical Surveys, Special Report 44, 100 p..
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): 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): Mulligan, J.J., 1966, Tin-lode investigations, Cape Mountain area, Seward Peninsula, Alaska; with a section on petrography by W. L. Gnagy: U.S. Bureau of Mines Report of Investigations 6737, 43 p.
Reference (Deposit): Hudson, T.L., 1984, Tin systems of Seward Peninsula, Alaska: Anchorage, Anaconda Minerals Company internal report, 51 p. (Report held by Cook Inlet Region Inc., Anchorage, Alaska)
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.
Reference (Deposit): Hudson, T.L., and Arth, J. G., 1983, Tin-granites of Seward Peninsula, Alaska: Geological Society of America Bulletin, v. 94, p. 768-790.
Reference (Deposit): Heide, H.E., and Sanford, R.S., 1948, Churn drilling at Cape Mountain tin placer deposits, Seward Peninsula, Alaska: U.S. Bureau of Mines Report of Investigations 4345. 14 p.
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.