a covergent boundairy
A divergent boundary does not result in the subduction of one plate under the other.
Volcanic island arcs are likely to result from convergent boundaries where an oceanic plate subducts beneath another oceanic plate or a continental plate. The subducted plate can melt, causing magma to rise and form a series of volcanic islands above the subduction zone.
Mount St. Helens is a result of subduction as the Juan de Fuca Plate is pushed under the North American Plate.
The downward movement of a lithospheric plate into the asthenosphere is known as subduction. This process occurs at convergent plate boundaries where one plate is forced beneath another due to differences in density. Subduction can result in the formation of deep oceanic trenches and volcanic activity.
subduction boundary!!!
It is called subduction and only occurs in oceanic to oceanic or oceanic to continental plate collisions.
A divergent boundary does not result in the subduction of one plate under the other.
Volcanic island arcs are likely to result from convergent boundaries where an oceanic plate subducts beneath another oceanic plate or a continental plate. The subducted plate can melt, causing magma to rise and form a series of volcanic islands above the subduction zone.
The collision of tectonic plates with continental crust is most likely to result in the formation of extensive mountain ranges. This is because the thicker and less dense continental crust tends to crumple and fold when subjected to compression from plate movements, leading to the uplift of mountain ranges such as the Himalayas and the Alps.
Mount St. Helens is a result of subduction as the Juan de Fuca Plate is pushed under the North American Plate.
Mt. Fuji is a result of subduction at a convergent plate margin.
It is the result of the Cocos Plate subduction under the North American Plate.
The downward movement of a lithospheric plate into the asthenosphere is known as subduction. This process occurs at convergent plate boundaries where one plate is forced beneath another due to differences in density. Subduction can result in the formation of deep oceanic trenches and volcanic activity.
A subductive collision.
Subduction zone.
At plate boundaries, tectonic plates collide with each other, leading to geological processes such as subduction, mountain formation, and seismic activity. The collisions can result in the formation of new landforms, earthquakes, and volcanic eruptions, shaping the Earth's surface over time.
subduction boundary!!!