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K. Sameera
K.K.R.Gowtham Concept School
          Kakinada
Earthquakes




Any sudden movement of the earth’s surface
is called Earthquake.
Focus & Epicentre




• The point from which an earthquake originates
  is called the ‘focus’ and the point on the earths
  surface, directly above this is called the
  ‘Epicentre’.
Types of sysmic waves
Types of Seismic waves.
        (Earth waves)


1.P-Waves (Primary Wave)
2.S-Waves (Secondary
 Wave)
3.L-Waves (Long/Love Wave)
4.R-Waves (Rayleigh Wave)
P - WAVE




• Primary(P) waves cause the particles of rock
  to vibrate backwards and forwards in the
  wave direction.
S - WAVE




• Secondary(S) waves cause the particles to
  oscillate at right angles to the wave direction.
L - WAVE




•   When P and S waves reach the surface they are converted into long(L)
    waves.
•   They cause the particles to travel in transverse horizontal motion,
    perpendicular to the direction of propagation and generally parallel to the
    Earth’s surface.
•   It is the L waves that produce the most violent shocks and the resultant
    destruction.
RAYLEIGH WAVE




• Motion is both in the direction of propagation and
  perpendicular (in a vertical plane), and “phased” so
  that the motion is generally elliptical – either
  prograde or retrograde.
SEISMOGRAPH




• The instrument used to detect and record the seismic
  waves is called “Seismograph” and the record, which
  appears like a graph is called “Seismogram.”
Richter Scale




• Richter scale is used to measure the magnitude of
  the earthquakes. A magnitude of 2 is rarely felt,
  while a magnitude of 7 indicates the lower limit of an
  earthquake that has devastating effect over a large
  area.
THE END

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Earhquakes ppt by k.sameera kakinada

  • 2. Earthquakes Any sudden movement of the earth’s surface is called Earthquake.
  • 3.
  • 4. Focus & Epicentre • The point from which an earthquake originates is called the ‘focus’ and the point on the earths surface, directly above this is called the ‘Epicentre’.
  • 6. Types of Seismic waves. (Earth waves) 1.P-Waves (Primary Wave) 2.S-Waves (Secondary Wave) 3.L-Waves (Long/Love Wave) 4.R-Waves (Rayleigh Wave)
  • 7. P - WAVE • Primary(P) waves cause the particles of rock to vibrate backwards and forwards in the wave direction.
  • 8. S - WAVE • Secondary(S) waves cause the particles to oscillate at right angles to the wave direction.
  • 9. L - WAVE • When P and S waves reach the surface they are converted into long(L) waves. • They cause the particles to travel in transverse horizontal motion, perpendicular to the direction of propagation and generally parallel to the Earth’s surface. • It is the L waves that produce the most violent shocks and the resultant destruction.
  • 10. RAYLEIGH WAVE • Motion is both in the direction of propagation and perpendicular (in a vertical plane), and “phased” so that the motion is generally elliptical – either prograde or retrograde.
  • 11. SEISMOGRAPH • The instrument used to detect and record the seismic waves is called “Seismograph” and the record, which appears like a graph is called “Seismogram.”
  • 12.
  • 13. Richter Scale • Richter scale is used to measure the magnitude of the earthquakes. A magnitude of 2 is rarely felt, while a magnitude of 7 indicates the lower limit of an earthquake that has devastating effect over a large area.