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Earthquakes constitute one of the worst natural hazards
which often turn into disaster causing widespread
destruction and loss to human life.
The effects of earthquake vary upon the magnitude and
intensity. Earthquakes occur every now and then all
round the world, except in some places where
earthquakes occur rarely. The devastation of cities and
towns is one of the effects of earthquake.
What is Earthquake?
An Earthquake is the result
of a sudden release of energy
in the earth’s crust that creates
seismic waves.
The seismic activity of an
area refers to the
frequency,type and size of
earthquakes experienced over
a period of time
For example:
If you throw stone in a
pond of still water,series of
waves are produced on the
surface of water,these waves
spread out in all directions from
the point where the stone strikes
the water.
similarly, any sudden
disurbances in the earth’s crust
may produce vibration in the
crust which travel in all direction
from point of disturbances.
Focus(Hypocenter):
Focus is the point on the fault
where rupture occurs and the
location from which seismic
waves are released.
Epicenter:
Epicenter is the point on the
earth’s surface that is directly
above the focus ,the point where
an earthquake or underground
explosion originates.
Cont…
Fault Line:
A Fault line is the surface trace of
a fault, the line of intersection
between the earth’s surface.
Fault plane:
Fault plane are the crackes or
sudden slips of the land .
Fault Scrap:
A Fault scrap is the topographic
expression of faulting attributed
to the displacement of the land
surface by movement along
faults.
The primary cause of an earthquake is faults on the crust of
the earth.
“A Fault is a break or fracture b/w two blocks of rocks in
response to stress.”
This movement may occur rapidly, in the form of an
earthquake or may occur slowly, in the form of creep.
Earth scientists use the angle of the fault with respect to the
surface (known as the dip) and the direction of slip along the
fault to classify faults.
Normal fault:
a dip-slip fault in which the
block above the fault has
moved downward relative to
the block below.
1.Thrust (reverse)fault:
Thrust (reverse)fault:
a dip-slip fault in which the
upper block, above the fault
plane, moves up and over the
lower block.
Strike-slip fault:
A left-lateral strike-slip
fault :
It is one on which the
displacement of the far block is
to the left when viewed from
either side.
A right-lateral strike-slip
fault:
It is one on which the
displacement of the far block is
to the right when viewed from
either side.
Some major causes of earthquakes on basic of its causes are:
Surface causes
Volcanic causes
Tectonic causes
Surface cause:
Great explosions, landslides, slips on steep coasts, dashing
of sea waves , avalanches , railway trains, heavy trucks, some
large engineering projects cause minor tremors. some of them are
man made, other are natural.
Volcanic cause:
Volcanic eruptions produce earthquakes. Earthquakes may
precede, accompany and frequently follow volcanic eruptions.
They are caused by sudden displacements of lava within
or beneath the earth crust.
There are two general
categories of earthquakes
that can occur at a volcano:
volcano-tectonic
earthquakes
long period earthquakes.
Tectonic cause:
Structural disturbances resulting in the parts of the
lithosphere is the main cause of this type of earthquake.
Most of the disastrous earthquakes belong to this
category and occur in areas of great faults and fractures.
Sudden yielding to strain produced on the rocks of
accumulating stress causes displacements especially along
old fault zones known as great transform faults.
Plate Boundary Overview.flv
Seismic waves produced due to
earthquake are basically divided
into two major types:
Body waves
Surface waves
Body waves:
Body waves travels through the interior(body) of earth as they leave
the focus. Body waves are further divided into following types:
Primary (P) waves
Secondary(S) waves
Primary Waves (P-waves) Secondary Waves(S-wave)
High frequency High frequency
Short Wavelength Short Wavelength
Longitudinal waves Transverse waves
Pass trough both solids and
liquids
Can not move through liquids
Move forwards and
backwards as it compressed
and decompressed
Move in all direction from
their source
P-wave is faster S-wave is more slower than P-
wave
First P-wave arrive After P-wave,S-wave is arrive
Surface Wave:
Surface waves travels parallel to the earth’s surface and these
waves are slowest and most damaging. Surface wave are divided
into following types:
Love waves
Rayleigh waves
Love Waves Rayleigh wave
Guided waves Guided waves
Displacement is parallel to the
free surface
Displacement is perpendicular
to love-wave displacement
Love wave is faster Rayleigh wave is slower
Causes horizontal shifting of
the earth surface.
Ground move in circular
motion.
Earthquake

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Earthquake

  • 1.
  • 2. Earthquakes constitute one of the worst natural hazards which often turn into disaster causing widespread destruction and loss to human life. The effects of earthquake vary upon the magnitude and intensity. Earthquakes occur every now and then all round the world, except in some places where earthquakes occur rarely. The devastation of cities and towns is one of the effects of earthquake.
  • 3. What is Earthquake? An Earthquake is the result of a sudden release of energy in the earth’s crust that creates seismic waves. The seismic activity of an area refers to the frequency,type and size of earthquakes experienced over a period of time
  • 4. For example: If you throw stone in a pond of still water,series of waves are produced on the surface of water,these waves spread out in all directions from the point where the stone strikes the water. similarly, any sudden disurbances in the earth’s crust may produce vibration in the crust which travel in all direction from point of disturbances.
  • 5. Focus(Hypocenter): Focus is the point on the fault where rupture occurs and the location from which seismic waves are released. Epicenter: Epicenter is the point on the earth’s surface that is directly above the focus ,the point where an earthquake or underground explosion originates.
  • 6. Cont… Fault Line: A Fault line is the surface trace of a fault, the line of intersection between the earth’s surface. Fault plane: Fault plane are the crackes or sudden slips of the land . Fault Scrap: A Fault scrap is the topographic expression of faulting attributed to the displacement of the land surface by movement along faults.
  • 7. The primary cause of an earthquake is faults on the crust of the earth. “A Fault is a break or fracture b/w two blocks of rocks in response to stress.” This movement may occur rapidly, in the form of an earthquake or may occur slowly, in the form of creep. Earth scientists use the angle of the fault with respect to the surface (known as the dip) and the direction of slip along the fault to classify faults.
  • 8. Normal fault: a dip-slip fault in which the block above the fault has moved downward relative to the block below. 1.Thrust (reverse)fault: Thrust (reverse)fault: a dip-slip fault in which the upper block, above the fault plane, moves up and over the lower block.
  • 9. Strike-slip fault: A left-lateral strike-slip fault : It is one on which the displacement of the far block is to the left when viewed from either side. A right-lateral strike-slip fault: It is one on which the displacement of the far block is to the right when viewed from either side.
  • 10. Some major causes of earthquakes on basic of its causes are: Surface causes Volcanic causes Tectonic causes Surface cause: Great explosions, landslides, slips on steep coasts, dashing of sea waves , avalanches , railway trains, heavy trucks, some large engineering projects cause minor tremors. some of them are man made, other are natural.
  • 11. Volcanic cause: Volcanic eruptions produce earthquakes. Earthquakes may precede, accompany and frequently follow volcanic eruptions. They are caused by sudden displacements of lava within or beneath the earth crust. There are two general categories of earthquakes that can occur at a volcano: volcano-tectonic earthquakes long period earthquakes.
  • 12. Tectonic cause: Structural disturbances resulting in the parts of the lithosphere is the main cause of this type of earthquake. Most of the disastrous earthquakes belong to this category and occur in areas of great faults and fractures. Sudden yielding to strain produced on the rocks of accumulating stress causes displacements especially along old fault zones known as great transform faults. Plate Boundary Overview.flv
  • 13. Seismic waves produced due to earthquake are basically divided into two major types: Body waves Surface waves
  • 14. Body waves: Body waves travels through the interior(body) of earth as they leave the focus. Body waves are further divided into following types: Primary (P) waves Secondary(S) waves
  • 15. Primary Waves (P-waves) Secondary Waves(S-wave) High frequency High frequency Short Wavelength Short Wavelength Longitudinal waves Transverse waves Pass trough both solids and liquids Can not move through liquids Move forwards and backwards as it compressed and decompressed Move in all direction from their source P-wave is faster S-wave is more slower than P- wave First P-wave arrive After P-wave,S-wave is arrive
  • 16. Surface Wave: Surface waves travels parallel to the earth’s surface and these waves are slowest and most damaging. Surface wave are divided into following types: Love waves Rayleigh waves
  • 17. Love Waves Rayleigh wave Guided waves Guided waves Displacement is parallel to the free surface Displacement is perpendicular to love-wave displacement Love wave is faster Rayleigh wave is slower Causes horizontal shifting of the earth surface. Ground move in circular motion.