seismic wave that causes
rock particles to move at right angles to the direc-
tion of the wave, known as an S-wave.
permanent deformation
caused by strain when stress exceeds a certain
value.
seismic wave that squeezes and
pushes rocks in the same direction that the wave
travels, known as a P-wave.
place along an active fault that
has not experienced an earthquake for a long time.
the vibrations of the ground
during an earthquake.
measures earthquake
intensity on a scale from I to XII; the higher the
number, the greater the damage the earthquake has
caused.
large, powerful
ocean wave generated by the vertical motions of the
seafloor during an earthquake; in shallow water,
can form huge, fast-moving breakers exceeding
30 m in height that can damage coastal areas.
fracture or system of fractures in Earth’s
crust that occurs when stress is applied too quickly
or stress is too great; can form as a result of hori-
zontal compression (reverse fault) , horizontal shear
(strike-slip fault) , or horizontal tension (normal
fault) .
the size of the seismic waves; an
increase of 1 in the scale represents an increase in
amplitude of a factor of 10.
forces per unit area that act on a material—compression, tension, and shear.
Verticales
causes materials to bend
and stretch; proportional to stress, so if the stress is
reduced or returns to zero the strain or deforma-
tion is reduced or disappears.
point on Earth’s
surface directly above the focus of an earthquake.
seis-
mic vibrations in areas of fluid saturated sand can
cause the ground to behave like a liquid.
instru-
ment used to measure horizontal or vertical motion
during an earthquake.
deformation of materials in response
to stress.
numerical rating system used to
measure the amount of energy released during an
earthquake.
record pro-
duced by a seismometer that can provide individual
tracking of each type of seismic wave.
measure of the energy released
during an earthquake, which can be described
using the Richter scale.
point of the initial fault rupture where
an earthquake originates that usually lies at least
several kilometers beneath Earth’s surface.
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