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Types of Plate Boundaries
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When 2 plates meet….. 1- They can crash together =
Convergent Boundary OR 2- They can move away from each other = Divergent Boundary OR 3- They can slide past each other = Sliding/Transform Boundary 2
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Convergent Boundaries
There are two types of Convergent Boundaries: A. Subduction: when one plate is more dense than another, the more dense plate goes underneath the less dense plate. Subduction The 2nd type is collision 3
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Convergent Boundaries: Subduction
One plate goes under the other Features that occur: Earthquakes, Volcanoes, Ocean Trench Remember: “The Ocean floor is going DOWN!!!!” 4
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Example Mt. St. Helens- Juan de Fuca plate goes under the North American Plate. What are some indicators that a volcano might erupt soon? 5
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Convergent Boundaries, Collision
B. Collision: when the 2 plates are the same material. When they hit, they both buckle up (this makes mountains) The two plates have the same density, they buckle up and move to a higher elevation Features: Earthquakes, Folded Mountains 6
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Example Mt. Everest, Himalayas
The plates are still colliding and gaining Elevation What are some forces of nature that keep Everest from getting much higher? 7
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Divergent Boundaries When two plates move apart. Features:
In continents: Rift Valley, Volcanoes, Earthquakes In oceans: Mid-Ocean Ridge, Volcanoes, Earthquakes 8
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Examples: Great Rift Valley, Africa Mid-Atlantic Ridge, Atlantic Ocean
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Example: Great Rift Valley, Africa
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Sliding/Transform Boundary
When two plates slide past each other. Features: Earthquakes 11
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Example: California- Pacific Plate slides past the North American Plate at the San Andreas Fault. 12
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Example: San Andreas Fault Where is it?
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