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Subduction
-Occurs when an oceanic plate collides with a continental plate.
-The oceanic plate is forced under the continental plate, creating subduction.
Divergent Boundaries
-Two oceanic plates are moving away from each other.
-Forms the Mid-Ocean Ridge.
-New crust is formed between the spreading of the plates by cooling magma that has erupted from the fault.
-This process is known as Sea Floor Spreading.
Continental Collision
-Two continental plates collide and force the crust to wrinkle upward and create mountains.
-The Himalayas are actually still growing because the Indian and Eurasian plates are colliding with each other.
Sliding/ Lateral/ Transform/ Conservative Boundaries
-Two or more plates slide past each other.
-Pressure will build up until a certain point where the two plates will finally shift possibly 10 feet, causing an earthquake.
-An example of this would be the San Andreas Fault in California.
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Subduction
-Occurs when an oceanic plate collides with a continental plate.
-The oceanic plate is forced under the continental plate, creating subduction.
Divergent Boundaries
-Two oceanic plates are moving away from each other.
-Forms the Mid-Ocean Ridge.
-New crust is formed between the spreading of the plates by cooling magma that has erupted from the fault.
-This process is known as Sea Floor Spreading.
Continental Collision
-Two continental plates collide and force the crust to wrinkle upward and create mountains.
-The Himalayas are actually still growing because the Indian and Eurasian plates are colliding with each other.
Sliding/ Lateral/ Transform/ Conservative Boundaries
-Two or more plates slide past each other.
-Pressure will build up until a certain point where the two plates will finally shift possibly 10 feet, causing an earthquake.
-An example of this would be the San Andreas Fault in California.