Up, down, and sidewise.
At Divergent Plate Boundaries.
Tectonic plates interact at plate boundariesThey move apart at divergent boundaries
tectonic plates move apart allowing magma to move to the surface.
Tectonic plates move along, against, or away from eachother at their boundaries. These movements produce earthquakes
Constructive tectonic plates?
At tectonic plate boundaries, earthquake zones, and the edges of tectonic plates.
Tectonic plates move along, against, or away from eachother at their boundaries. These movements produce earthquakes
Tectonic plate interactions are of three different basic types: Divergent boundaries are areas where plates move away from each other, forming either mid-oceanic ridges or rift valleys. These are also known as constructive boundaries. Convergent boundaries are areas where plates move toward each other and collide.
When plates collide, plate boundaries are formed. There are three kinds. At divergent boundaries, two tectonic plates move away from each other and make earthquakes. At convergent boundaries, two plates come together and make mountain ranges. At transform boundaries, one plate slides under the other.
The place where two tectonic plates move away from each other horizontally are called divergent plate boundaries.
Plates move apart at these tectonic plate boundaries.
Earth's crust is broken up into segments called tectonic plates, which move very slowly. A plate boundary is where two of these plates meet. There are three basic types: convergent boundaries where plates collide, divergent boundaries where plates pull apart, and transform boundaries where plates slide past each other.