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.

a. as the temperature increases, the kinetic energy of the gas molecules increases & the molecules move faster & further away from each other.

b. if you decrease the temperature of a fixed amount of gas at constant pressure, the combined gas law reduces to charles's law. in this case, volume will also decrease.