A divergent boundary does not result in the subduction of one plate under the other.
When plates collide, one plate is typically forced beneath the other in a process known as subduction. This can create mountain ranges, volcanic arcs, and deep ocean trenches above the subduction zone as a result of the intense geological activity generated by the collision and subduction of the plates.
Convergent plate boundaries
Convergent plate boundaries where an oceanic plate collides with a continental plate or another oceanic plate are most likely to result in a subduction zone. In this scenario, the denser oceanic plate is forced beneath the less dense continental plate, creating a subduction zone.
A collision boundary is two plates colliding at each other creating a subduction zone. The heavier/slower plate dives 20-60 degrees down from the surface and the lighter/faster plate is crushed and forms folded mountains along the boundary.
Mount St. Helens is a result of subduction as the Juan de Fuca Plate is pushed under the North American Plate.
The density of the tectonic plates involved determines whether a subduction zone or collision zone is formed at a destructive plate margin. If one plate is denser than the other, it will subduct beneath the other plate, forming a subduction zone. If the plates have similar densities, they will collide and form a collision zone.
A subductive collision.
When plates collide, one plate is typically forced beneath the other in a process known as subduction. This can create mountain ranges, volcanic arcs, and deep ocean trenches above the subduction zone as a result of the intense geological activity generated by the collision and subduction of the plates.
Collision, Mountains, Ridges. I think that is what you are asking. :)
A subduction zone and a collision zone are the same place, a collision just happens earlier, when the crusts of the two plates are interacting. Later, when the crust of one plate is being forced under the crust of another plate into the mantle, it becomes a subduction zone.
Subduction occurs, as one plate collides with another, the harder plate may force the other plate downwards and into the mantle. For example, when the Indian Plate collided with the Asian Plate, the harder Asian Plate forced the Indian into subduction. This forced the Asian Plate to be raised and the Himalayas were the result.
At collision zones, tectonic plates converge and interact in different ways. This can result in the creation of mountain ranges, earthquakes, and the subduction of one plate beneath another. The intense pressure and friction at collision zones lead to the deformation and uplift of the Earth's crust.
The Himalayas are found at a convergent plate boundary also known as a subduction zone where one plate slips under the other driving the land mass up.
Convergent plate boundaries
Convergent plate boundaries where an oceanic plate collides with a continental plate or another oceanic plate are most likely to result in a subduction zone. In this scenario, the denser oceanic plate is forced beneath the less dense continental plate, creating a subduction zone.
A collision boundary is two plates colliding at each other creating a subduction zone. The heavier/slower plate dives 20-60 degrees down from the surface and the lighter/faster plate is crushed and forms folded mountains along the boundary.
Mount St. Helens is a result of subduction as the Juan de Fuca Plate is pushed under the North American Plate.