Actually that whole region is a series of volcanic island arcs, so the dominant volcanic material is andesitic. Midway along the gas content, so you can have mild or violent eruptions. The flood basalt areas, like Boring, are the stitching that hold the region together.
Pinatubo and Krakatoa are both stratovolcanoes, Krakatoa just happens to have a bit more silica in it's melt which makes it more dangerous. That and it is right on the ocean. So the major explosions have been phreatomagmatic. Big big big booms with those.
Same thing happened with Mt. St. Helen's. Earthquake dislodged a large slab of material which brought the glacier in direct contact with the magma body, and BOOM.