It's called a divergent plate boundary.
If you click on 'related links' below you can see some pictures of different plate boundaries
Two tectonic plates that are being pulled away from each other are referred to as divergent plates. This movement typically occurs at mid-ocean ridges, where new oceanic crust is formed as magma rises to the surface. As the plates separate, they can create features such as rift valleys on land or ocean basins underwater.
No, subduction zones are where tectonic plates collide and one plate is forced beneath the other. New crust is formed at divergent plate boundaries, where plates move apart and magma rises to create new crust.
A convergent boundary is formed when two tectonic plates collide. This collision can result in one plate being forced beneath the other in a process called subduction, where the denser plate sinks into the mantle. This can lead to the formation of mountain ranges, deep ocean trenches, and volcanic activity.
Divergent Boundary, (Constructive Boundary).
At a divergent boundary, tectonic plates move away from each other due to tensional forces. As the plates separate, magma from the mantle rises to the surface and solidifies, creating new crust. This process is responsible for the formation of mid-ocean ridges and rift valleys on land.
Two tectonic plates that are being pulled away from each other are referred to as divergent plates. This movement typically occurs at mid-ocean ridges, where new oceanic crust is formed as magma rises to the surface. As the plates separate, they can create features such as rift valleys on land or ocean basins underwater.
No, subduction zones are where tectonic plates collide and one plate is forced beneath the other. New crust is formed at divergent plate boundaries, where plates move apart and magma rises to create new crust.
A convergent boundary is formed when two tectonic plates collide. This collision can result in one plate being forced beneath the other in a process called subduction, where the denser plate sinks into the mantle. This can lead to the formation of mountain ranges, deep ocean trenches, and volcanic activity.
Divergent Boundary, (Constructive Boundary).
At a divergent boundary, tectonic plates move away from each other due to tensional forces. As the plates separate, magma from the mantle rises to the surface and solidifies, creating new crust. This process is responsible for the formation of mid-ocean ridges and rift valleys on land.
A landform that can be formed at a convergent plate boundary is a mountain range. This occurs when two continental plates collide, pushing up rock layers and creating uplifted peaks. Examples include the Himalayas formed by the collision of the Indian Plate with the Eurasian Plate.
At a divergent plate boundary new crust is created as two or more plates pull away from each other. An example of a rift where land between two continents are being pulled apart is the Great Rift Valley.
A convergent boundary with no subduction is a continental-continental boundary. Because oceanic crust is denser than continental crust, it is always the subducting plate in a oceanic-continental boundary. In an oceanic-oceanic boundary, one of the plates will subduct, depending on several factors. Continental plates are thicker and less dense than oceanic plates, and when they converge, they push up the area where the plates meet, forming mountain ranges (note that this is not the only, or even the predominant, method of mountain formation). The Himalayas are being formed as a result of a continental-continental boundary.
Japan is at the meeting place of four tectonic plates: The Pacific Plate, The Eurasian Plates, The Philippine Plate, and the Okhotsk Plate (sometimes considered part of the North American Plate).
The boundary between the Caribbean and Cocos plates is a convergent boundary. The Cocos plate is being subducted beneath the Caribbean plate, resulting in volcanic activity and earthquakes along the boundary.
convergence plate boundary, where tectonic plates move towards each other and collide, leading to subduction zones which are highly constructive regions of volcanoes. Volcanoes also form at divergent plate boundaries. A good example being the numerous Icelandic volcanoes which have formed over he Mid Atlantic Ridge.
Tectonic plates that are convergent are "crashing into" each other at this collision boundary, and a subduction zone there is possible. One of the plates will "dive under" the other one. This creates uplift, "hot spots" or volcanic "risers" and instability along the boundary. The west coast of the United States is a good example. A link is provided below.