VOLCANOE ALONG CONVE!GEN' #LA'E $O%N&A!' E Volcanoes are a (ibrant manifestation of plate tectonics processes. Vo lcanoes are common along con(ergent and di(ergent plate boundaries) but are also found *ithin lithospheric plates a*a+ from plate boundaries.,here(er mantle is able to melt) (olcanoes ma+ be the result.

Volcanoes erupt because mantle roc melts. 'he rst stage in creating a (olcano is *hen mantle roc begins to melt because of e/tremel+ high temperatures ) lithospheric pressure lo*ers) or *ater is added. Along subducting plate boundaries) the crust heats up as it sins into the mantle. Also) ocean *ater is mi/ed in *ith the sediments l+ing on top of the subducting plate.

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'his *ater lo*ers the melting point of the mantle material) *hich increases melting. Volcanoes at con(ergent plate boundaries are found all along the #acic Ocean basin) primaril+ at the edges of the #acic) Cocos) and Nazca plates.