It is neither, because plate is not being made or destroyed. Divergent is constructive. Convergent is destructive. Subduction is constructive.
divergent - creates new crustal rockconvergent - destroys old crustal rock
The Mid-Atlantic Ridge is another name for the divergent boundary in the Atlantic Ocean. It is a mountain range that formed by the seafloor spreading along this boundary.
The main types of divergent boundaries are mid-ocean ridges, where new oceanic crust is formed as tectonic plates move apart; continental rifts, where plates within continents separate, creating rift valleys; and back-arc basins, where oceanic plates are being subducted under continents, leading to extension and back-arc spreading.
At the western edge of the Nazca plate and the eastern edge of the Pacific plate lies the East Pacific Rise. The East Pacific Rice is known as a mid-ocean ridge, formed from a divergent boundary.
It is neither, because plate is not being made or destroyed. Divergent is constructive. Convergent is destructive. Subduction is constructive.
divergent - creates new crustal rockconvergent - destroys old crustal rock
divergent - creates new crustal rockconvergent - destroys old crustal rock
I can name u destructive boundaries. CONVERGENT, DIVERGENT, TRANSFORM. Well it depennds what kind of destructive forces ur talking about be more if you are i will be willing to tell you r email me
The Mid-Atlantic Ridge is another name for the divergent boundary in the Atlantic Ocean. It is a mountain range that formed by the seafloor spreading along this boundary.
I think there 1)Destructive (convergent) 2)collision(convergent) 3)constructive(divergent) 4)conservative(transform) the brackets are the same words
The main types of divergent boundaries are mid-ocean ridges, where new oceanic crust is formed as tectonic plates move apart; continental rifts, where plates within continents separate, creating rift valleys; and back-arc basins, where oceanic plates are being subducted under continents, leading to extension and back-arc spreading.
At the western edge of the Nazca plate and the eastern edge of the Pacific plate lies the East Pacific Rise. The East Pacific Rice is known as a mid-ocean ridge, formed from a divergent boundary.
a constructive (divergent) plate boundary, new crust is being created to infill the gaps caused by spreading plates. At a destructive (subduction-convergent) plate boundary, old, dense oceanic crust is diving into, and becoming part of the mantle.Read more: What_is_the_difference_between_a_constructive_plate_boundary_and_a_destructive_plate_boundary
Divergent boundaries are considered constructive because they involve the pulling apart of tectonic plates, creating new crust from the mantle through volcanic activity. This process leads to the formation of new land and ocean basins. In contrast, convergent boundaries are considered destructive because they involve the collision of tectonic plates, leading to subduction zones, earthquakes, volcanic eruptions, and the destruction or recycling of crust.
The three types of plate margins are convergent boundaries, where plates move toward each other; divergent boundaries, where plates move apart from each other; and transform boundaries, where plates slide past each other horizontally.
The three main types of tectonic plate boundaries are divergent boundaries (where plates move apart), convergent boundaries (where plates collide), and transform boundaries (where plates slide past each other horizontally).