Tensional stress.
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.
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.
The Divergent Boundaries.
There are two plate boundaries that cause volcanoes. They are the divergent and convergent plate boundaries.
Tensional stress.
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.
the three types of plate boundaries are : -convergent plate boundaries -divergent plate boundaries -transformed plate boundaries
the three types of plate boundaries are : -convergent plate boundaries -divergent plate boundaries -transformed plate boundaries
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.
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.
There are divergent, convergent, and transform plate boundaries.
Rifts.
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).
plant boundaries move together
divergent