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Explore 2.3 Dynamics at Subduction Zones: Back Arc Spreading at Convergent Margins with 16,357 views, 176 likes, and 6 comments. Experience the impact of this video content that has captured audience attention.

See our playlist of videos for Geology & Earth Science https://www.youtube.com/watch?v=owlPSr39Nn8&list=PL6taRb3I0WLhYc8g1cuBk5crqUtLs3oXZ 2.3 Dynamics at Subduction Zones: Back Arc Spreading at Convergent Margins Because subduction zones form where two plates are converging, it is natural to assume that large compressional forces are at work to deform the plate margins. Indeed, this is the case along many convergent plate boundaries. However, convergent margins are not always regions dominated by compressional forces. Extension and Back Arc spreading Along some convergent plate margins, the overlying plates are under tension, which causes stretching and thinning of the crust. But how do extensional processes operate where two plates are moving together? Snow Mountain Arts http://xue-lin.com/category/natural-sciences/earth-science .

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