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Tectonic formation
Earthquake
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Earthquake Definition
Shaking
of the
earth’s ground
due to
sudden release
of
energy
in the
earth’s lithosphere
Earthquake occurrence
Generally occur along
plate boundaries
, which contain systems of deep fractures called
faults
Earthquake occur when
Rock masses
on either side of a fault are pushed by
tectonic forces
Friction
causes them to get
locked
, and
stress build up
When the
stress exceeds
the
strength
of the fault (rock), the rocks
snap
or
suddenly move
to a
new position
The sudden movement causes
seismic waves
to be released resulting in
ground shaking
Earthquake concepts
The point in the earth’s crust where waves are released is known as
focus
-> origin of earthquake
The point on the earth’s surface directly above the focus is called the
epicentre
-> shaking is generally felt strongest
How are earthquake measured?
Measured using:
seismometers
->
sensitive instruments
that detect
ground vibrations
& determine the
magnitude
of an
earthquake
->
greater
the
seismic energy
released during an earthquake =
greater
the
magnitude
Richter Scale
(
ML)
Calculates
earthquake magnitude
using the
height
of the
largest
wave recorded on
seismometers
—> Measured based on the maximum seismic intensity reached
—> Scale numbered from 1 to 10
—> Scale is logarithmic ( magnitude 6 earthquake is 32 times more energy than magnitude 5 )
Richter Scale limitation
Rate
an earthquake with a single
drastic
spike in wave energy as having a
higher
magnitude than a
long
earthquake with many
large
,
intense
wave
underestimates longer
earthquakes ->
released
more
overall
energy -> could deal more
damage
no longer
commonly
used (expect for
small
,
local
earthquake)
Moment
Magnitude Scale (
Mw
)
Rate earthquake magnitude based on the
total energy
released during the earthquake
estimates
total energy
instead of
largest
wave
more accurate (especially in magnitude
8
earthquake & above)
scale is
logarithmic
(magnitude
6
earthquake is 32 times more energy than magnitude
5
)