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Description: Island arc-type mountain building Steady subduction of oceanic lithosphere Joints Fractures along which no appreciable displacement has occurred Most are formed when rocks in the outer-most crust are deformed Orogenesis – processes that collectively produce a mountain belt Most mountain building occurs at convergent plate boundaries Compressional mountains Picture Stats: Views: 315 Filesize: 1.09MB Height: 695 Width: 952 Source: https://biology-forums.com/index.php?action=gallery;sa=view;id=39596 |