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Transcript
Seafloor spreading and recycling of oceanic crust
A scientist by the name of Harry Hess theorized that mid-ocean ridges mark structurally weak zones where the
ocean floor was being ripped in two lengthwise along the ridge crest. New magma from deep within the Earth
rises easily through these weak zones and eventually erupts along the crest of the ridges to create new oceanic
crust. This process is called seafloor spreading.
A profound consequence of seafloor spreading is that new crust was, and is now, being continually created along
the oceanic ridges. If the Earth's crust was expanding along the oceanic ridges, Hess reasoned, it must be
shrinking elsewhere. He suggested that new oceanic crust continuously spread away from the ridges in a conveyor
belt-like motion. Many millions of years later, the oceanic crust eventually descends into the oceanic trenches -very deep, narrow canyons along the rim of the Pacific Ocean basin.
According to Hess, the Atlantic Ocean was expanding while the Pacific Ocean was shrinking. As old oceanic
crust was consumed in the trenches, new magma rose and erupted along the spreading ridges to form new crust.
In effect, the ocean basins were perpetually being "recycled," with the creation of new crust and the destruction of
old oceanic lithosphere occurring simultaneously. Thus, Hess' ideas neatly explained why the Earth does not get
bigger with sea floor spreading, why there is so little sediment accumulation on the ocean floor, and why oceanic
rocks are much younger than continental rocks.
1. How is the ocean floor created during sea floor spreading? Use the term mid ocean
ridge in your answer.
2. How is the ocean floor destroyed during sea floor spreading? Use the term trench in
your answer.
3. How is sea floor spreading evidence for the Continental Drift Theory?
4. By observing the diagram, how are rift valleys formed?
5. Why doesn’t the earth get bigger with sea floor spreading?
Sea Floor Spreading
Oceanic crust
is recycled
within the
Earth’s
interior as it
subducts
underneath
the continental
crust.