The zones of seismic activity longwhich plates are in contact. These may coincide with continental margins, but usually do not. Movement between plates is predominately horizontal,and may be divergent, or convergent, or side-by-side.
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The zones of seismic activity longwhich plates are in contact. These may coincide with continental margins, but usually do not. Movement between plates is predominately horizontal,and may be divergent, or convergent, or side-by-side.