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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).
Magma produced from the melting Pacific plate rises to the surface and erupts to form the volcanic islands of the Aleutian island chain. Mount Cleveland: Plate Tectonic Setting The Aleutian Islands were formed by interactions between the North American and Pacific plates. They are located on the southern edge of the North American plate where it collides with the Pacific plate (see map above) to form a convergent plate boundary.