Destructive margin - Dense oceanic crust is subducted beneath the less dense continental lithosphere. As the oceanic crust descends it is partially melted, destroyed. The magma then rises into chambers and may result in explosive volcanoes. ocean trenches and island arcs and fold mountains. volcanoes and earthquakes.
Subduction zone - Challenger Deep, Mariana Trench - 36,000 ft deep (pacific and eurasion plate)
If Continental/continental it creates fold mountains. lower density and therefore not much subduction. no volcanoes.
Young fold mountain - Annapurna Range, Himalayas - central nepal, south asia. (Indo-Australian Plate and the Eurasian Plate)
If oceanic/oceanic it is the same process as first stated.ocean trenches and island arcs volcanoes and earthquakes.
Island arc - Mariana islands, NW Pacific (pacific and eurasion plate)
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