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Partial melting occurs in the depth window of 100-150 km (Harry and Leeman, 1995).

Below are pictured certain volcanoes, represented by the volcano icon. They appear to mostly occur in areas where earthquake depths also fall between this range. These are not hotspot volcanoes (like the Hawaiian islands, which occur in the middle of a plate), for they are the result of the subduction zone to the south of the arc.

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Using seismic reflection, slopes of the plain were determined to be 50 m per km: Figure from Piper et al., 1973.

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It is seen on the google earth image that the Pacific plate is subducting under the North American plate. On the map earthquakes of the last 2 years are displayed. The deepest earthquakes are located in the middle of the trench with a maximum depth of ~250 km (The red arrow).

At the west end of the trench there is a zone of only shallow earthquakes. This represents the Bering-Kresta Shear zone that is a transform fault. There is also an inactive zone marked with the pink arrow.

There is a clear line between earthquakes that happened on the subducting plate before it subducts and the ones that happened as part of the subduction.

Two years of earthquakes (Google Earth)

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Topographic map of Aleutian Islands Region

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Topographic map of Aleutian Islands Region

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This map depicts the topography of the Aleutian Trench and the surrounding region. Note that the island arc does not occur immediately adjacent to the trenchContour Interval: 400 m. Figure from McCarthy and Scholl, 1985.

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A-B: 35 NW
C-D: 42 N

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-By 10 million years, approximately 750 km of plate will have subducted under the Aleutian Island Arc. Having formed ~55-50 Ma, the island arc will likely gain fairly insubstantial mass. However, with rising sea levels, the islands may become slightly submerged.

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Harry, D. and Leeman, W. (1995). Partial melting of melt metasomatized subcontinental mantle and the magma source potential of the lower lithosphere. Journal of Geophysical Research: Solid Earth, 100(B6), pp.10255-10269.
McCARTHY, J. and SCHOLL, D. (1985). Mechanisms of subduction accretion along the central Aleutian Trench. Geological Society of America Bulletin, 96(6), p.691.
Piper, D., von Huene, R. and Duncan, J. (1973). Late Quaternary Sedimentation in the Active Eastern Aleutian Trench. Geology, 1(1), p.19.

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Eva, Shannon, Kaeli, Sandra, Rob, Josh