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Earth’s Internal Structure
EURASIAN
PLATE
FIGURE 2
2900 km
JUAN DE FUCA
PLATE
NORTH
AMERICA
2000 km
PLATE
PACIFIC
PLATE
CARIBBEAN
PLATE
1370 km
PACIFIC
PLATE
Inner core,
solid nickleiron
EQUA
COCOS
PLATE
TOR
Outer core,
liquid nickle-iron
NAZCA
PLATE
Mantle, peridolite,
dense igneous rock
Crust (6-35 km) granitic under continents
and basaltic under oceans
LEGEND
subduction zone
spreading ridge
transform fault
Internal structure of the earth and the three types of plate boundaries. Convection cells of hot, molten
rock deep beneath the crust provide the energy which causes plate motion on the earth's surface.
Plate motion, particularly one plate moving against another, is a common cause of earthquakes.
SOUTH
AMERICAN
PLATE
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