When the oceanic and continental lithosphere collides, the dense oceanic ltihosphere subducts beneath the less dense continental lithosphere. Thus, deep oceanic trenches, volcanoes, island arcs, submarine mountain ranges and fault line can be formed.
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Answer:
When the oceanic and continental lithosphere collides, the dense oceanic ltihosphere subducts beneath the less dense continental lithosphere. Thus, deep oceanic trenches, volcanoes, island arcs, submarine mountain ranges and fault line can be formed.