At a convergent plate boundary, where two tectonic plates collide, one plate is forced beneath the other in a process called subduction. The descending plate sinks into the mantle, causing it to melt and create magma. This magma can then rise to the surface, leading to volcanic activity. The interaction between the plates and the mantle at a convergent boundary is dynamic and can result in the formation of mountain ranges, earthquakes, and volcanic arcs.
Yes, the mantle can be seen at a plate boundary where tectonic plates interact, such as at divergent or convergent boundaries.
At a convergent boundary, plates move towards each other.
Convergent boundary.
At a convergent boundary, tectonic plates are typically pushed together by the force of subduction where one plate is forced beneath the other, or by collision where the plates directly collide with each other. This movement can be driven by the force of mantle convection, where heat from the Earth's core causes the mantle to flow in a circular motion.
A convergent boundary is where two plates collide. This can lead to the formation of mountains, earthquakes, and volcanic activity.
Yes, the mantle can be seen at a plate boundary where tectonic plates interact, such as at divergent or convergent boundaries.
The mantle is below the plates.
Density plays a key role in convergent boundaries. When two plates collide at a convergent plate boundary, it is the denser plate that will subduct.
At a convergent boundary, plates move towards each other.
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.
Convergent boundary.
Convergent means where plates are moving together. Divergent means where plates are moving apart.
When plates collide it is called a convergent boundary.newtest3
At a convergent boundary two plates move toward each other. At a transform boundary plates slide past each other.
At a convergent boundary, tectonic plates are typically pushed together by the force of subduction where one plate is forced beneath the other, or by collision where the plates directly collide with each other. This movement can be driven by the force of mantle convection, where heat from the Earth's core causes the mantle to flow in a circular motion.
No, the Australian and Eurasian plates are not on a convergent boundary; they are primarily on a divergent boundary. The Australian Plate is moving away from the Eurasian Plate, which is part of the tectonic activity in the region of the Indian Ocean. However, there are areas where these plates interact, such as the boundary near Indonesia, which can involve complex tectonic interactions.
An area where two tectonic plates collide is called a boundary. There are three kinds of boundaries. They are convergent, divergent, and transform boundaries.