Such deep earthquakes usually don't cause enough shaking on the surface to be hazardous, but scientifically they are of great interest.
Not exact matches
The brief magnetic pulses observed prior to some moderate - sized
earthquakes might be triggered by chemical bonds breaking in rocks under stress (
such as those
deep beneath the San Andreas fault, shown).
Because
such shifts in olivine change the structure of earth's subducted lithosphere, the new phase transition mechanism could help explain the origins of some
deep earthquakes.
More broadly, the Pisagua event has seismologists rethinking some basic ideas about the risk of
earthquakes in similar geological settings elsewhere — places with
deep - diving crustal plates,
such as Japan and Indonesia.
Because we can not sample the
deep Earth, we must deduce its composition either by looking at the clues hidden in igneous and metamorphic rocks, or by examining proxies for composition and structure
such as the three - dimensional variation of the velocity of seismic waves produced by
earthquakes and sampled by networks of seismometers on the surface.
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