Divergent Boundary
Check out this short animation to see a divergent boundary.
Convergent Boundary
Another type of boundary is when plates come together or collide with each other. One plate is forced down and melted while the other is forced upward and folded into mountains. A trench is formed where the two plates meet. This is called a "Convergent Boundary".
This is a real-world example of a Convergent Boundary. See how the land in the middle of the picture is pushing up where the two sides meet? Pretty amazing!
Transform Boundary
The last type of boundary we'll look at is called "Transform" or "Sliding" boundary. The reason it is called this is because instead of the plates moving away from each other, or crashing into each other, the plates are sliding by each other, kind of like when you pass someone in the hallway. These plates slide along beside of each other. Since plate boundaries are not smooth, plates do not slide smoothly. The plates can suddenly break free of each other and cause powerful earthquakes. One of the most well known Transform Boundaries in the world is called "The San Andreas Fault", which is located in the state of California. California experiences many earthquakes each year because of this boundary, or fault zone. Notice the red arrows in this map of the San Andreas fault, which show the two land masses sliding beside each other.
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