The plate boundry for subduction can be convergent plate boundries.
Divergent borders, where fresh crust is produced as the plates separate. As one plate slides under another, the crust is destroyed at convergent borders. Plates glide past each other horizontally at transform borders, where crust is neither created nor destroyed.
Subduction occur in convergent plate boundries, Divergent boundries creates a new crust by magma pushing up from the mantle, convergent plate boundries formed mountain in which two plates are moving one another, Volcanoes form are produced by two boundries Divergent and convergent plate boundries and divergent boundries where river changes its path.
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