mountais
When two oceanic plates collide, a deep ocean trench is formed due to one plate being pushed under the other in a process known as subduction. This subduction zone can create volcanic activity and earthquakes in the region.
mountain or volcanoe
When tectonic plates collide, they can form various geological features depending on the nature of the collision. If two continental plates converge, they can create mountain ranges, such as the Himalayas. When an oceanic plate collides with a continental plate, it can lead to subduction, forming deep ocean trenches and volcanic arcs. Additionally, the collision of two oceanic plates can result in island arcs.
These zones are known as subduction zones where tectonic plates collide, forcing one plate to be pushed beneath the other. This process leads to the formation of deep ocean trenches and can result in earthquakes, volcanic activity, and the creation of mountain ranges.
False. A strike-slip fault forms at a transform boundary where two tectonic plates slide past each other horizontally. A convergent boundary is formed when two plates collide and one plate is forced beneath the other in a subduction zone.
Usually either a mountain range, or a subduction zone.
convergent
When two oceanic plates collide, a deep ocean trench is formed due to one plate being pushed under the other in a process known as subduction. This subduction zone can create volcanic activity and earthquakes in the region.
earthquakes
When two oceanic plates collide, a process called subduction occurs, where one plate is forced beneath the other into the mantle. This often leads to the formation of volcanic arcs, deep-sea trenches, and earthquakes. Over time, the subducted plate melts and can contribute to the formation of new oceanic crust.
mountain or volcanoe
When tectonic plates collide, they can form various geological features depending on the nature of the collision. If two continental plates converge, they can create mountain ranges, such as the Himalayas. When an oceanic plate collides with a continental plate, it can lead to subduction, forming deep ocean trenches and volcanic arcs. Additionally, the collision of two oceanic plates can result in island arcs.
These zones are known as subduction zones where tectonic plates collide, forcing one plate to be pushed beneath the other. This process leads to the formation of deep ocean trenches and can result in earthquakes, volcanic activity, and the creation of mountain ranges.
collide into each other
A Convergence Boundary.
When two plates move together (at least one must be oceanic crust), one will sink beneath the other. The result is that a subduction zone forms between the two plates at the location where they meet.
Mountains and grass