EARTHQUAKE HAZARDS Flashcards
(29 cards)
is a natural event feared by many, even by those who have not recalled any
experience of it or its effects.
Earthquake
and earthquake are usually used
synonymously because people perceive earthquake often when the ground below
shakes without warning.
Ground shaking
is a phenomenon caused by the sudden and rapid movement of large
volumes of rock along fractures on the surface of the earth called faults.
earthquake
rock along fractures on the surface of the earth called
faults
The outermost
shell of the earth, which includes the crust and the uppermost mantle, consists of
tectonic plates.
These are massive and irregularly shaped slabs of rock. Due to their
roughness, the edges of these plates get stuck while the plates continue moving.
tectonic plates.
energy stored in the rocks is released in the form of
seismic waves.
two types of seismic waves:
body waves and surface waves.
are seismic waves that travel through the interior of the earth.
Body waves
the first waves that reach the surface of the
earth and make the ground shake. They move the ground back and
forth along the direction they are traveling. The shaking from P
waves is light or sometimes not felt.
Primary (P) waves
are body waves that vibrate perpendicular to
their propagation direction, producing an up and down motion. They
move slower but shake the ground more strongly than P waves.
Secondary (S) waves
are waves that are trapped near the surface.
Surface waves
are
surface waves that have a horizontal motion perpendicular to the direction
they are traveling.
Love waves
shake the ground in a rotational manner
with no transverse motion.
Rayleigh waves
The severity of an earthquake is measured based on the energy it
releases, or its
magnitude,
its effects on people and man-made
structures, or what we call
intensity.
is the visible breaking and displacement of the Earth’s surface along the trace of a fault. It may
be a vertical movement, a lateral movement, or a combination of both, depending on the type of fault generating
Ground rupture
faults that are vertical or near-vertical faults that displace rock horizontally.
Strike-slip faults
If the block opposite you when
looking across a fault moves to the left, it is a
a sinistral (or left-lateral) fault.
fault. If the block moves to the right, it is a
dextral (or right-lateral) fault.
Reverse or thrust faults are faults which move the hanging wall up. These faults are
dip-slip
faults,
causes a vertical displacement of the ground.
dip-slip
faults,
cases wherein water rising from the ground as the ground shakes.
Sometimes, witnesses would describe the ground seemingly act like a liquid
during an earthquake.
liquefaction.