A plate boundary is a three-dimensional surface or zone where the velocity (speed or direction) of one lithospheric plate in relation to the next lithospheric plate changes significantly.
Types of plate boundaries include convergent, divergent and transform boundaries.
When tectonic plates move, The highly hot, molten material known as lava can escape from the mantle when the plates move because they collide or split apart.
When two plates collide, they either push one plate under the other and back into the mantle, where it melts, or they crumple up and create mountains.
Convergence barriers create strong earthquakes as well as volcanic mountains or islands when the oceanic plate that is sinking melts.
One or both of the colliding plate boundaries may bow upward into mountain ranges or downward into a deep undersea trench as a result of the collision.
Strong earthquakes and a chain of volcanoes frequently form around the edges of converging plate boundaries. These borders are converging when two plates are interacting.
Subduction zones form when one or both of the tectonic plates are composed of oceanic crust.
Borders that diverge allude to the division of two plates. The transformative borders points are the where plates pass one
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