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    Tectonic Plates

    Tectonic Plates

    Earth's rigid outer shell is broken into plates that drift a few centimeters a year. Textbooks usually name 7 major ones. The map uses the more detailed PB2002 model by geophysicist Peter Bird, which counts 52. It splits the Indo-Australian Plate in two, so 8 major plates cover 83% of the globe. The rest are medium plates and microplates squeezed between them.

    Plates in the PB2002 model
    52
    Major plates
    8 (83% of the surface)
    Medium plates
    12
    Microplates
    32
    Total length of boundaries
    260,800 km
    Fastest boundary
    263 mm a year (Tonga Plate and Pacific Plate)

    The 8 Major Plates

    Three Kinds of Plate Boundaries

    Divergent · 94,800 km
    Plates pull apart and magma rises between them, mostly along mid-ocean ridges on the seafloor.
    Convergent · 91,900 km
    Plates push together. One dives under the other (subduction) or both crumple into mountains. This is where the largest earthquakes and most explosive volcanoes come from.
    Transform · 74,100 km
    Plates slide past each other sideways, like the San Andreas Fault in California.

    All 52 Plates, Largest to Smallest

    Explore Further

    Sources: Bird, P. (2003), An updated digital model of plate boundaries, Geochemistry Geophysics Geosystems, PB2002 model · Live Atlas calculations