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Sea-Floor Spreading And the Mid Ocean Ridge
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Magma erupts along the mid-ocean ridge. This happens slowly.
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New crust (sea floor) is formed as magma cools and slowly pulls away from the ridge.
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Older rock becomes more dense and sinks down into the mantle at deep ocean trenches in a process called subduction.
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Sea-Floor Spreading Animation
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Earth’s polarity changes at irregular intervals
Earth’s polarity changes at irregular intervals. Evidence of this is found in the magnetized “stripes” of the ocean floor rock.
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Evidence of Sea-Floor Spreading
Molten material- rocks show evidence of molten material erupting again and again along mid-ocean ridges Magnetic stripes- iron bits in rock on both sides of the mid-ocean ridge lineup to point either north or south. The pattern is the same on each side of the ridge. Rock samples- younger rock found near ridge and older rock found away from ridge
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