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Geology Presentation
by :
Faraz Haider
(+92 336 8666897)
Stresses Due To
Seismic Waves
Seismic waves are waves of energy that travel
through the Earth's layers, and are a result of
an earthquake, explosion, or a volcano that
imparts low-frequency acoustic energy.
Types Of Seismic Waves
 Body Waves :
Primary Waves and Secondary Waves.
 Surface Waves :
Love Waves and Rayleigh Waves.
Body Waves
Body Waves travel through the Interior of earth.
They follow the ray paths refracted by the
varying density and modulus (Stiffness) of the
earth interior.
This effect is similar to the refraction of light
waves.
Types of Body Waves
These are the fastest moving waves. There are
two types of Body Waves.
 P (primary) Waves or Compressional Waves.
 S (secondary) waves or Shear Waves.
P (primary) Waves
A longitudinal earthquake wave that travels
through the interior of the earth and is usually
the first conspicuous wave to be recorded by a
seismograph.
S (secondary) waves
A transverse earthquake wave that travels
through the interior of the earth and is
usually the second conspicuous wave to
reach a seismograph.
Surface Waves
Surface waves are analogous to water waves and
travel along the earth’s surface.
They Travel Slower then Body Waves because of
there low frequency, long duration, and large
amplitude.
They can be the most destructive type of
Seismic Waves.
Types of Surface waves
There are two main types of surface waves
Rayleigh Waves
Love Waves
Impact Of Seismic Waves
Seismic
waves result from
slip and rupture
(breakage) of
rocks and plates of
earth along faults.
Disasters of
Seismic Waves
These waves
causes problems
for buildings and
weakened their
strength.
 Earthquakes occur with the passage of large
seismic waves.
 In other words we can say that there is a
sequence of seismic waves following each other.
There is a Question raised that,
How can we reduce the effect
and destructions of Seismic waves…..?
Resistant Techniques
Earthquake may not be able to damage entire
building but it damage members of it.
So special techniques are adopted :
Base Isolation Devices
and
Seismic Dampers
Base Isolation Devices
Seismic Dampers
Resistant Structure
Rectangles are
such structure of
building on which
the Seismic waves
are less effective.
Rectangular Buildings
Arches and Triangles
Arches and triangles are also such
structures of building on which the
Seismic waves are less effective or not
effect just like other buildings.
Arch Structures
Triangular Structures
Precautionary
Measurements
We need different levels of resistance for
different classes of structures.
Critical structures such as hospitals, power
plants, water-treatment, and chemical plants,
dams, etc.
 These buildings must not only survive the
shaking, but must remain in operation.
These structure require the largest
investment of resources to insure that
they can provide services following an
earthquake.
Thankyou…

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Stresses due to seismic waves

  • 1. Geology Presentation by : Faraz Haider (+92 336 8666897)
  • 2. Stresses Due To Seismic Waves Seismic waves are waves of energy that travel through the Earth's layers, and are a result of an earthquake, explosion, or a volcano that imparts low-frequency acoustic energy.
  • 3. Types Of Seismic Waves  Body Waves : Primary Waves and Secondary Waves.  Surface Waves : Love Waves and Rayleigh Waves.
  • 4. Body Waves Body Waves travel through the Interior of earth. They follow the ray paths refracted by the varying density and modulus (Stiffness) of the earth interior. This effect is similar to the refraction of light waves.
  • 5. Types of Body Waves These are the fastest moving waves. There are two types of Body Waves.  P (primary) Waves or Compressional Waves.  S (secondary) waves or Shear Waves.
  • 6. P (primary) Waves A longitudinal earthquake wave that travels through the interior of the earth and is usually the first conspicuous wave to be recorded by a seismograph.
  • 7.
  • 8. S (secondary) waves A transverse earthquake wave that travels through the interior of the earth and is usually the second conspicuous wave to reach a seismograph.
  • 9.
  • 10. Surface Waves Surface waves are analogous to water waves and travel along the earth’s surface. They Travel Slower then Body Waves because of there low frequency, long duration, and large amplitude. They can be the most destructive type of Seismic Waves.
  • 11. Types of Surface waves There are two main types of surface waves Rayleigh Waves Love Waves
  • 12. Impact Of Seismic Waves Seismic waves result from slip and rupture (breakage) of rocks and plates of earth along faults.
  • 13.
  • 14. Disasters of Seismic Waves These waves causes problems for buildings and weakened their strength.
  • 15.  Earthquakes occur with the passage of large seismic waves.  In other words we can say that there is a sequence of seismic waves following each other.
  • 16.
  • 17. There is a Question raised that, How can we reduce the effect and destructions of Seismic waves…..?
  • 18. Resistant Techniques Earthquake may not be able to damage entire building but it damage members of it. So special techniques are adopted : Base Isolation Devices and Seismic Dampers
  • 21. Resistant Structure Rectangles are such structure of building on which the Seismic waves are less effective.
  • 23. Arches and Triangles Arches and triangles are also such structures of building on which the Seismic waves are less effective or not effect just like other buildings.
  • 26. Precautionary Measurements We need different levels of resistance for different classes of structures. Critical structures such as hospitals, power plants, water-treatment, and chemical plants, dams, etc.
  • 27.  These buildings must not only survive the shaking, but must remain in operation. These structure require the largest investment of resources to insure that they can provide services following an earthquake.