How do the Aleutian volcanoes differ from the Cascades volcanoes?

Type of Convergence - Ocean to continent for Cascade/ Ocean to Ocean for Aleutian

Explanation:

Type of Convergence - Ocean to continent for Cascade/ Ocean to Ocean for Aleutian

Explanation:

If the two plates that meet at a convergent plate boundary both are of oceanic crust, the older, denser plate will subduct beneath the less dense plate.

The features of an ocean-ocean subduction zone are the same as those of an ocean-continent subduction zone, except that the volcanic arc will be a set of islands known as an island arc.

The older plate subducts into a trench, resulting in earthquakes. Melting of mantle material creates volcanoes at the subduction zone.

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rising temperatures because when water vapor in the air is cooled, it condenses. it turns back into a liquid and attaches to dust particles in the air. these very small water droplets group together to form clouds