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Volcanoes are a result of the magma bursting through the surface as rocks. Volcanoes are also caused by the plates hitting each other. The opposite of convergent plates is a divergent plate. This is where the plates move apart. Most divergent plates are in the oceans. The gap is filled by magma rising to the surface. This forms an oceanic ridge. East Africa’s Rift Valley is an example of a divergent boundary on land. Earthquakes are common at divergent boundaries.
A transform plate boundary is where two plates slide past each other. The crust is cracked and torn, causing earthquakes. The San Andreas Fault is an example of a transform boundary.
Movement at plate boundaries causes stress or pressure on the rocks. The types of stress are compression, tension, and shear. A break in the Earth’s crust due to rock movement is called a fault.
Compression stress is caused by the plates pushing together. One type of compression change is squeezing. Fold mountains, such as the Himalayas, are caused by two plates colliding. In this case, an oceanic plate subducts beneath the continental plate and an upper rock layer folds into mountains. Compression creates a reverse fault or thrust fault, where a block is pushed up.
Tension stress is caused by plates pulling apart and stretching the Earth’s crust, a divergent boundary. We see the results of tension stress in rift valleys, such as here in Iceland. Tension stress produces a normal fault, where a block drops down about the areas around it.
Shear stress is caused when rocks slip past each other, as found in transform boundaries. This is called a transform fault or a strike-slip fault. The blocks of rock slide past each other horizontally.
Geologists discovered rocks have many layers. These are sedimentary rocks, which form in horizontal layers. They also discovered some mountain areas have rocks that are not in horizontal layers but are folded and angled.
Fill in this table to review fault and boundary type: | Type of Boundary | Type of Fault | Type of Pressure on Rock | How it Moves | Surface Feature | |-----------------------|------------------------|--------------------------|-----------------------|---------------------------| | Divergent boundary | Normal Fault | Stretching apart | Basin and Range | | Convergent boundary | Reverse or Thrust Fault| Compression | Pushing Together | Himalayas and other mountains | | Transform boundary | Strike-slip or Slip Fault | Shear | Sideways horizontally | San Andreas Fault |
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