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Published byDwight Jacobs Modified over 9 years ago
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Sea-Floor Spreading Copy the following map of the ocean floor between continents. Label the parts of your map as we go along.
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Convection currents in the asthenosphere push the crust apart.
Sea-Floor Spreading Mid-ocean ridge Oceanic crust Mantle Convection currents in the asthenosphere push the crust apart.
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Sea-Floor Spreading Mid-ocean ridge Oceanic crust Mantle Magma
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Sea-Floor Spreading Mid-ocean ridge Sea-floor spreading Oceanic crust
Mantle Sea-floor spreading: New magma is pushed up at the mid-ocean ridge, which pushes the older rock away. Magma
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Newly formed oceanic crust
Sea-Floor Spreading Newly formed oceanic crust Mid-ocean ridge Sea-floor spreading Oceanic crust Mantle Magma
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Newly formed oceanic crust
Sea-Floor Spreading Newly formed oceanic crust Old oceanic crust Mid-ocean ridge Sea-floor spreading Oceanic crust Mantle Magma
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Newly formed oceanic crust
Sea-Floor Spreading Newly formed oceanic crust Old oceanic crust Mid-ocean ridge Continental crust Sea-floor spreading Trench Oceanic crust Mantle Magma
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Newly formed oceanic crust
Sea-Floor Spreading Newly formed oceanic crust Old oceanic crust Mid-ocean ridge Continental crust Sea-floor spreading Trench Oceanic crust Mantle Subduction: Old oceanic crust is pushed under a continent causing the rock to melt back into magma in the mantle. Magma
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Sea-Floor Spreading Oceanic crust Mid-ocean ridge Deep-ocean trenches
forms subducted through Mid-ocean ridge Deep-ocean trenches Molten material forms erupts through
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Sea-Floor Spreading Oceanic crust Mid-ocean ridge Deep-ocean trenches
forms subducted through Mid-ocean ridge Deep-ocean trenches Molten material forms erupts through
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Sea-Floor Spreading Oceanic crust Mid-ocean ridge Deep-ocean trenches
forms subducted through Mid-ocean ridge Deep-ocean trenches Molten material forms erupts through
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Sea-Floor Spreading Oceanic crust Mid-ocean ridge Deep-ocean trenches
forms subducted through Mid-ocean ridge Deep-ocean trenches Molten material forms erupts through
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