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A divergent boundary, or constructive boundary, is where two sections of the eggshell - two tectonic plates - are moving away from each other. When this happens, they leave a gap in-between, and this gap can be filled by the magma from below. This creates a series of volcanoes all the way along the boundary.
Divergent Margins. boundaries where plates are moving toward each other, and. sometimes one plate sinks (is subducted) beneath another. The. location where the sinking of a plate occurs is called a subduction. zone. A transform boundary is where plates slide past each other. with no creation or destruction of lithosphere. Plate Margin Examples. There are three general types of plate boundaries: divergent, convergent, and transform. Each general type has multiple. âspeciesâ: divergent boundaries can be spreading ocean ridges or. continental rift zones; convergent boundaries can occur between. two continental plates.