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Major Geological Events
Caused by Plate Tectonics
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Types of Boundaries Divergent Plates move apart Convergent
Plates come together Transform Plates slide horizontally past each other
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Divergent Structures New crust is formed as plates pull apart.
Land features include: Mid-Ocean Ridges Ex. - Mid-Atlantic Ridge Rift Valleys Ex. - African Rift Valley Earthquakes
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Mid–Ocean Ridge (Location of Sea Floor Spreading)
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Sea Floor Spreading (Mid-Ocean Ridge)
Younger Older Older Divergent Structure
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Rift Valley Divergent Structure
Divergent Structure
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Convergent Boundaries
Crust is destroyed and recycled back into the mantle Three types of convergent collisions Features include: Trenches – Mariana Trench Volcanic Arc (Volcanic Mountains) – Andes mountains Mountain Ranges – Himalayan Mountains Earthquakes
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Subduction Result of convergent boundary
A more dense plate slides under a less dense plate and sinks into the mantle. Features include: Oceanic-Oceanic = Trenches Oceanic-Continental = Mountain Ranges
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Subduction Examples
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Oceanic-Oceanic convergence
Convergent Boundary Oceanic-Oceanic Land Features – Trench and Island Arc Oceanic-Oceanic convergence
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Oceanic-Continental convergence
Convergent Boundary Oceanic-Continental Land Features – Trench and Volcanic Arc (Volcanic Mountains) Oceanic-Continental convergence
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Continental-Continental convergence
Convergent Boundary Continental-Continental Land Features – Folded Mountains Continental-Continental convergence
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Mountain Ranges
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Transform Fault Structures
Crust is neither destroyed nor created Can occur between two oceanic plates or oceanic-continental plates Features include: Earthquakes Fault line – San Andreas Fault
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Transform Boundary Oceanic-Oceanic Land Feature – Fault Line
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Transform Boundary San Andreas Fault Line
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Transform Boundary Continental-Continental Land Features – Fault Line
Aerial view of San Andreas Fault in the Carrizo Plain, self-made, Nov 16, 2007, I. Kluft,
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Earthquakes – All Boundaries
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Volcanoes
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Putting It All Together
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Plate Boundaries
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Plate Movement
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