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Plate Tectonics
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The Earth’s Crust is Made of Plates
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What Causes the Plates to Move?
Convection- hot magma rises, cool magma sinks (like a lava lamp
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Two Types of crust Continental Crust- made of granite (light)
Oceanic Crust- made of basalt (heavy)
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Plate Boundaries Cracks in the plates are called faults
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Types of Boundaries (Faults)
Convergent Boundary Divergent Boundary Transform Boundary
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Divergent Boundary Plates move away from each other Forms volcanoes,
new crust and rift valleys Ex) Iceland, mid-Atlantic ridge
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Divergent Boundary – Arabian and African Plates
Arabian Plate Red Sea African Plate
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Divergent Boundary – Iceland
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Rift Valleys A deep valley formed as plates move apart at a divergent boundary. Ex) The Great Rift Valley in eastern Africa
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Sea Floor Spreading Mid Ocean Ridges – underwater mountain chains that run through the Earth’s Basins Magma rises to the surface and solidifies and new crust forms Older Crust is pushed farther away from the ridge
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Transform Boundary Plates slide past each other Creates earthquakes
Ex) San Andreas Fault in California
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Convergent Boundary Plates move toward each other
Earthquakes, forms mountain ranges Ex) Himalayan Mountains
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Continental-Continental Boundary
Plates fold, creating mountains
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Convergent Boundaries - Continental
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Oceanic-Oceanic Boundary
Creates trenches (deep valleys) Forms volcanoes Forms Island Arcs Ex) Aleutian Islands (Alaska)
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Convergent Boundary – Oceanic & Oceanic
Note – plates are reversed Subduction occurs when the denser plate sinks below the other &
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Oceanic-Continental Boundary
Oceanic plate pushes down because it is more dense. Creates deep ocean trenches Creates coastal mountain ranges Ex) Andes mountains
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Convergent Boundary – Oceanic & Continental
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Hot Spots Hot material rises from deep within the mantle.
Heats the lithosphere, causing volcanoes at the surface. Ex) Hawaiian Islands, Yellowstone N.P.
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Evidence of Pangaea
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Vocab to Remember Fault Convection Divergent Boundary
Convergent Boundary
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Vocab ctd… Transform Boundary Rift Valley Hot Spot
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