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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).
Aleutian Trench. The Aleutian Trench forms the border between the North American Plate to the north and the Pacific Plate on the south side of the Aleutian Islands. It formed as the heavier Pacific Plate converged with the North American Plate forcing the Pacific's oceanic plate into the mantle. The Aleutian Islands have formed on the continental side of the trench. NOAA. Size of the trench The trench between the Pacific Plate and the North American Plate is 2,200 miles long. It is between 50 and 100 miles wide and reaches depths of 25,000 feet in some places. The Aleutian Islands have formed on the continental side of the fault zone.