Divergent.
Convergent.
Transform.
Tectonic movement.
The place where tectonic plates touch is known as a plate boundary. At plate boundaries, tectonic activity such as earthquakes and volcanic eruptions occur due to the movement and interaction of the plates. There are three types of plate boundaries: divergent, convergent, and transform.
the three types of plate boundaries are : -convergent plate boundaries -divergent plate boundaries -transformed plate boundaries
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Plate boundaries are places where two tectonic plates meet. There are three major types of plate boundaries. These are divergent, convergent, and transform plate boundaries.
The zone where tectonic plates meet is called a plate boundary. At plate boundaries, tectonic activity such as earthquakes, volcanic eruptions, and mountain building can occur due to the movement and interactions of these plates. There are three main types of plate boundaries: divergent, convergent, and transform.
There are three basic plate movement types, first there is convergent movement. Secondly, there is divergent movement and lastly there is transform movements.
There are three main types of plate tectonic boundaries: divergent boundaries, where plates move apart; convergent boundaries, where plates collide; and transform boundaries, where plates slide past each other horizontally. Each type of boundary has its own characteristic geologic features and tectonic activity.
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 types of stresses found at plate boundaries are compression (pushing together), tension (pulling apart), and shear (sliding past each other). These stresses occur due to the movement of tectonic plates and can result in various geologic phenomena such as earthquakes and mountain formation.
All of the tectonic plates have different types of plate boundaries, most having all three types of plate boundaries. Convergent, where the plate is subducting under another plate, divergent, where the plate is pulling away from another plate, and transform boundaries where the plates are sliding past each other.
The effect of subduction at the boundary of two plates is the movement of one tectonic plate under another tectonic plate. This creates a subduction zone, which often occurs in convergent boundaries.