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This type of boundadry occurs when two continental plates slide past each other. The movement is mostly horizontal. The plates slowly scrape against another, building up energy. This energy is later is released by a sudden shift. Rocks are broken or distort cause of the movements.

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When older oceanic plate is forced to go under another plate, it creates a volcano or islands.

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The denser plate, made out of oceanic plate, is subducted underneath the less dense plate, which is continental plate. This is what occurs when oceanic plate converges to a continental plate

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Plate Tectonics-- Geological features of Convergent Plate Boundaries

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When two continental plates converge/collide, one plate goes underneath the other plate. This is what you call subduction.

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This divergent boundary is can also occur if oceanic-oceanic plates diverge and create a mid ocean ridge.

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Divergent Plate Boundaries (or How do you make an ocean?)

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A divergent boundary is when continental-continental plates diverge/move away from each other. This will form a ridge