Cape Mountain

Deposit with commodities tin

More information at and near this site: Sn-AK00035

About this location

Feature ID Sn-Mo00547
Geographic coordinates -167.956458, 65.583791
Point definition Mineral occurence represented as the same location as the mine feature
Reference Mulligan (1966); Page 24, Figure 7
Date: 1966; Scale: Large (>1:24,000)

Geologic information

Commodities tin
Valuable materials cassiterite
Associated materials wollastonite (1); green pyroxene (1); green tourmaline(1)
Mineralization style lenticular pods; veins; veinlets
Host rock age Upper Mississippian (2)
Host unit name Port Clarence Group (2)
Host lithologies granite; limestone
Alteration contact metamorphism (1)
Reference Mulligan, J.J., 1966, Tin-lode investigations, Cape Mountain Area, Seward Peninsula, Alaska, Bureau of Mines Report Investigations 6737, 43 p.
Additional references (1) Heide and others (1946); (2) Baggs and others (1988)

Descriptions from sources

Geology

?Tin, in the form of cassiterite, is known to occur as a constituent of quartz veins, as a replacement of limestone near the granite contact, and in granite near the limestone contact. The principal associates of the tin are tourmaline and pyrite. It is impossible to state whether any of these occurrences will yield tin in commercial quantities. In view of the excellent exposures on Cape Mountain, it would seem that if quartz veins of considerable magnitude were present they could easily be discovered, because such veins would form strong outcrops, and therefore, because of the scarcity of quartz-vein material on the surface it is improbable that large deposits of vein quartz occur on Cape Mountain.?

Steidtmann, E., and Cathcart, S.H., 1922, Geology of the York tin deposits, Alaska: U.S. Geological Survey Bulletin 733, 130 p.

Deposit models and geoenvironmental models

Type Model Reference
Deposit model 15b - Sn veins Reed, B.L., 1986, Descriptive Model of Alluvial Placer Sn, in Cox, D.P., and Singer, D.A., 1986, Mineral deposit models: U.S. Geological Survey Bulletin 1693, p. 275-275.
Geoenvironmental model Vein and Greissen Sn and W du Bray, E.A., 1995, ed., Preliminary compilation of descriptive geoenvironmental mineral deposit models: U.S. Geological Survey Open-File Report 95-831, 272 p.

Resource estimate summaries

Date Description Class Type Material Contained Units
1946 Reserve Indicated ore tin 47 metric tons
1946 Reserve Inferred ore tin 98 metric tons

Detailed resource estimates

1946: Reserve, Indicated
Year of estimate 1946
Resource description Reserve
Resource classification Indicated
Material tin
Material type ore
Material amount 650
Amount units metric tons
Grade 7.28
Grade units percent
Contained commodity 47
Contained commodity units metric tons
Material amount SI 650
Material amount SI units metric tons
Grade SI 7.28
Grade SI units percent
Contained commodity SI 47
Contained commodity SI units metric tons
Short reference Baggs and others (1988)Page 37
Reference Baggs, D.W., Northam, M.J., Meyer, M.P., and Maas, K.M., 1988, Selected Significant Mineral Deposits in Alaska A Minerals Availability System Overview, U.S. Bureau of Mines Information Circular 9177, p. 134.
1946: Reserve, Inferred
Year of estimate 1946
Resource description Reserve
Resource classification Inferred
Material tin
Material type ore
Material amount 1,350
Amount units metric tons
Grade 7.28
Grade units percent
Contained commodity 98
Contained commodity units metric tons
Material amount SI 1,350
Material amount SI units metric tons
Grade SI 7.28
Grade SI units percent
Contained commodity SI 98
Contained commodity SI units metric tons
Short reference Baggs and others (1988)Page 37
Reference Baggs, D.W., Northam, M.J., Meyer, M.P., and Maas, K.M., 1988, Selected Significant Mineral Deposits in Alaska A Minerals Availability System Overview, U.S. Bureau of Mines Information Circular 9177, p. 134.

History of the site

Dates Status Detail Reference
1902 to 1902 Discovery Lode tin was discovered Mulligan (1966)

Geographic context based on the point coordinates