That depends! Continental-Continental convergent boundaries result in the formation of fold mountains. Crust here is neither created or destroyed.
Continental-Oceanic and Oceanic-Oceanic collision bounsdaries generally lead to the formation of a subduction zone, where the denser plate (usually the older and therefore cooler oceanic plate) sinks back into the mantle and melts so is destroyed (or more accurately recycled).
A transform plate boundary does not create or destroy crust. Instead, adjacent plates slide horizontally past each other. This movement can cause earthquakes along the boundary without significantly changing the amount of crust.
Divergent boundaries occur when tectonic plates move away from each other, creating new crust, while convergent boundaries happen when plates collide, leading to the destruction or subduction of crust.
Mountains are typically formed at convergent plate boundaries where two tectonic plates collide and one is forced over the other, leading to uplift and deformation of the crust. This collision can create major mountain ranges like the Himalayas or the Andes.
Yes, convergent boundaries and sea-floor spreading are related in the sense that sea-floor spreading can occur at divergent boundaries (where tectonic plates move apart), leading to the creation of new oceanic crust. This new oceanic crust can then be consumed at convergent boundaries (where tectonic plates collide), as one plate is subducted beneath the other.
No, new crust is not created at a convergent boundary. Instead, at convergent boundaries, two tectonic plates come together and one plate is usually forced beneath the other in a process called subduction. This process can lead to the destruction of crust rather than the creation of new crust.
Yes, volcanism is found at both convergent and divergent boundaries of tectonic plates. At convergent boundaries, subduction zones can result in the formation of volcanoes due to the melting of subducted crust. At divergent boundaries, magma rises to the surface to create new crust, leading to volcanic activity as seen in mid-ocean ridges.
At convergent boundaries are boundaries the crust is destroyed by subduction of oceanic crust underneath continental crust or other oceanic crust.
At convergent boundaries are boundaries the crust is destroyed by subduction of oceanic crust underneath continental crust or other oceanic crust.
A transform plate boundary does not create or destroy crust. Instead, adjacent plates slide horizontally past each other. This movement can cause earthquakes along the boundary without significantly changing the amount of crust.
Convergent plate boundaries.
They make a mountain.
At convergent boundaries some mantle material can melt and rise through the crust, forming volcanoes.
Continental and Oceanic plates.
A divergent boundary does not occur at a convergent boundary. At convergent boundaries, tectonic plates move towards each other and usually result in the formation of mountains, ocean trenches, or volcanic activity. In contrast, divergent boundaries occur when plates move away from each other and create new oceanic crust.
Divergent boundaries occur when tectonic plates move away from each other, creating new crust, while convergent boundaries happen when plates collide, leading to the destruction or subduction of crust.
Mountains are typically formed at convergent plate boundaries where two tectonic plates collide and one is forced over the other, leading to uplift and deformation of the crust. This collision can create major mountain ranges like the Himalayas or the Andes.
At subduction zones along convergent plate boundaries.