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TLW identify convergent, divergent, and transform plate boundaries
For the purpose of understanding the different landforms formed by these plate boundaries As measured by naming the three types of plate boundaries correctly
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Why do we have earthquakes?
Plate Tectonics Why do we have earthquakes?
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Is the earth’s crust solid?
No, the earth’s crust is broken into many plates.
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Do the plates move? At one time, there was only one continent called Pangaea. Yes, the plates move slowly over time.
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Why do they move? Heat from the inner earth creates convection currents that move the magma.
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Driving Forces of Plate Tectonics
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Two Tectonic Plates That Separate
Divergent Boundary Two Tectonic Plates That Separate
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Magma rises up and new crust is formed
Divergent Boundary Sea-floor spreading Magma rises up and new crust is formed
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Divergent Boundary Mid-Atlantic Ridge Indian Ridge
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Divergent Divergent Boundary Boundary
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Divergent Boundary Rift Valley Iceland
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Divergent Boundary Rift Valley in Africa
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(Land Subsidence = sinking land)
The East African Rift Valley is land that has sunken by divergent boundary (Land Subsidence = sinking land)
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Two tectonic plates slide past each other.
Transform Boundary Two tectonic plates slide past each other.
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Transform Boundary
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Transform Boundary
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Two tectonic plates collide.
Convergent Boundaries Two tectonic plates collide.
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Ocean-Continent Convergent Boundary
Rising magma forms new crust in the form of mountains and volcanoes Two plates converge Heavier plate squeezed down Sea Trench Subduction Melting of old crust
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Andes Mountains Visualizing Physical Geography Copyright © 2008 John Wiley and Sons Publishers Inc.
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Ocean-Ocean Convergent Boundary
Aleutian Trench Old crust is melted and recycled.
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Aleutian Islands
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Continent-Continent Convergent Boundary
No new crust is formed or created
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TLW identify convergent, divergent, and transform plate boundaries
For the purpose of understanding the different landforms formed by these plate boundaries As measured by naming the three types of plate boundaries correctly
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