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The only lodes known in the Aleutian Islands region are gold deposits (some of which may have been productive) and occurrences of metallic sulfide minerals on Unalaska and neighboring Amaknak and Sedanka Islands (Berg and Cobb, 1967, P. 7â8, fig. 2).
The western Aleutian Islands are defined herein to be those islands that are located west of the eastern edge of the Adak 1:250,000-scale quadrangle boundary. The map area, which includes Great Sitkin Island on the east and Attu Island on the west, is largely uninhabited. maximum age for early Aleutian-Arc volcanism is suggested by the ages of rocks included in the Meshik Arc on the Alaska Peninsula (Wilson, 1985), the rocks of which appear to directly correlate with those of the Lower Series in the Aleutian Islands.