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divergent plate boundaries are associated with normal faulting. Thus there is a horizontal least compressive stress, vertical most compressive stress and a intermediate horizontal stress. All stresses are orthoganal to each other.

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What are three types of plate bounderys?

the three types of plate boundaries are : -convergent plate boundaries -divergent plate boundaries -transformed plate boundaries


What are three types of bounderies?

the three types of plate boundaries are : -convergent plate boundaries -divergent plate boundaries -transformed plate boundaries


What plate boundary creates?

Divergent Plate Boundaries


Is subduction common at divergent plate boundaries?

No, subduction is not common at divergent plate boundaries. Divergent plate boundaries are characterized by plates moving away from each other, which creates new oceanic crust. Subduction occurs at convergent plate boundaries where plates collide and one descends beneath the other.


What causes rocks to pull apart?

The type of stress that causes rocks to pull apart is a tension stress. It is the major type of stress found in divergent plate boundaries.


What types of boundaries are there?

There are divergent, convergent, and transform plate boundaries.


Divergent plate boundaries are characterized by what?

Rifts.


What can occur at divergent plate boundaries?

plant boundaries move together


What are the four plate boundaries?

The four types of plate boundaries are divergent boundaries (plates moving apart), convergent boundaries (plates moving together), transform boundaries (plates sliding past each other), and subduction zones (one plate sinking beneath another).


What are plate boundaries that move away form each other?

divergent


What boundary creates a crust?

The Divergent Boundaries.


Which of the plate boundaries can produce earthquakes?

Earthquakes are produced at all types of plate boundaries: convergent boundaries, where plates collide; divergent boundaries, where plates separate; and transform boundaries, where plates slide past each other. The release of stress along these boundaries can result in seismic activity.