continetal and oceanic
The three main types of plate boundaries are convergent boundaries, where plates move toward each other, divergent boundaries, where plates move away from each other, and transform boundaries, where plates slide past each other horizontally.
The three main types of plate boundaries are divergent boundaries (plates move apart), convergent boundaries (plates move toward each other), and transform boundaries (plates slide past each other horizontally). At divergent boundaries, new crust is formed as magma rises to the surface, while at convergent boundaries, crust is destroyed as one plate is subducted beneath another. Transform boundaries are characterized by earthquakes as the plates grind past each other.
The main types of plate movements are divergent (moving apart), convergent (moving towards each other), and transform (sliding past each other). Divergent boundaries result in new crust formation, convergent boundaries create subduction zones or mountain building, and transform boundaries lead to lateral sliding and earthquakes.
The three types of convergence are convergent boundary, divergent boundary, and transform boundary. Convergent boundaries occur when tectonic plates collide, divergent boundaries occur when tectonic plates move away from each other, and transform boundaries occur when tectonic plates slide past each other horizontally.
The difference between transform and divergent boundaries is that transform boundaries occur when tectonic plates slide past each other, whereas at divergent boundaries they move away from each other. However in both cases the plates move horizontally (unlike at convergent boundaries where one plate may be pushed underneath another).
The main types of tectonic plate boundaries are divergent boundaries, where plates move apart; convergent boundaries, where plates move toward each other; and transform boundaries, where plates slide past each other horizontally.
The three main types of plate boundaries are convergent boundaries, where plates move toward each other, divergent boundaries, where plates move away from each other, and transform boundaries, where plates slide past each other horizontally.
There are divergent, convergent, and transform plate boundaries.
convergent boundaries collide but divergent boundaries move away from each other.
the three types of plate boundaries are : -convergent plate boundaries -divergent plate boundaries -transformed plate boundaries
The three types of plate boundaries are divergent boundaries, where plates move away from each other; convergent boundaries, where plates move towards each other; and transform boundaries, where plates slide past each other horizontally.
The three main types of plate boundaries are divergent boundaries (plates move apart), convergent boundaries (plates move toward each other), and transform boundaries (plates slide past each other horizontally). At divergent boundaries, new crust is formed as magma rises to the surface, while at convergent boundaries, crust is destroyed as one plate is subducted beneath another. Transform boundaries are characterized by earthquakes as the plates grind past each other.
The three types of plate margins are convergent boundaries, where plates move toward each other; divergent boundaries, where plates move apart from each other; and transform boundaries, where plates slide past each other horizontally.
The three types of boundaries in science are convergent boundaries (where two plates move towards each other), divergent boundaries (where two plates move away from each other), and transform boundaries (where two plates slide past each other horizontally). These boundaries are important in understanding processes like plate tectonics.
divergent plate boundary- a boundary where two plates move apart from each other. convergent plate boundary- a boundary where two plates move towards each other so that one plate can sink beneath the other. transform plate boundary- a boundary where one plate slips along side another plate.
The main types of plate movements are divergent (moving apart), convergent (moving towards each other), and transform (sliding past each other). Divergent boundaries result in new crust formation, convergent boundaries create subduction zones or mountain building, and transform boundaries lead to lateral sliding and earthquakes.
At divergent boundaries, two plates move apart from each other and the space that this creates is filled with new crustal material sourced from molten magma that forms below.