Site hosted by Angelfire.com: Build your free website today!

Plate Tectonics

The earth crust is broken into large pieces call plates. These plates have been shown to move relative to each other.  There are 3 major types of plate boundaries that are a function of the movement that occurs at each of these boundaries. When two plates move together or "converge" a convergent plate boundary forms. Usually a Subduction Zone is formed where one plate is forced under the other. When a plate splits and moves apart, this is called a divergent plate boundary. The mid Ocean Ridge and the red sea are examples of divergent plate boundaries. If two plates slide past each other transform faults are formed, this is what is occurring at the San Andreas Fault in California.
 
 
 

Back to Plate Main Page