High volcanoes like those in the Cascades are typically found at convergent plate boundaries, where an oceanic plate subducts beneath a continental plate. This subduction process causes magma to form as the oceanic plate melts, leading to volcanic activity. The alignment of these volcanoes in a row parallel to the continental margin reflects the direction of the tectonic plates' movement and the specific areas where magma can escape to the surface. Thus, their location is a direct result of the geological processes associated with plate tectonics.
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