“…2) at an altitude of 200-300 ft (60-90 m), where a large area of marine planation and shore deposits was interpreted by W. H. Condon (in Berg, 1973, p. 34). Shore deposits of marine origin are recorded at similar and higher altitudes elsewhere in the southern part of southeastern Alaska and nearby British Columbia (Dolmage, 1923;Twenhofel, 1952;Clague, 1975 Stuckenrath andMielke, 1973, p. 395), and from the central part of the east coast of Prince of Wales Island, 50 mi (80 km) northwest of Metlakatla at an altitude of about 30 ft (9 m) (9,510±280 years B.P., 1-1621; Swanston, 1969a).…”