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Sea-Floor Spreading
and Subduction Zones
The
Andes Mountain Range spans the entire length of South
America, along the western coast. This close-up shows
that coast, which represents the western terrestrial
edge of the South American Plate. The leading edge
of the Nazca Plate is subducting below the South American
Plate at a plate boundary known as a subduction zone.
During this subduction some Nazca crust is scraped
off along base of the Andes, adding height to the
entire range.
The East Pacific Rise [the ridge to
the left] is part of the global network of mid-ocean
ridges that girdle the planet. As the sea-floor spreads
on either side of this ridge, the Nazca Plate moves
easterly while the Pacific Plate moves westerly. The
Galapagos Islands, off the northwestern coast of South
America, are the result of a "Hot Spot"
that exists over a mid-ocean ridge.
Thanks to Bruce Heezen and Marie Tharpe.