TSUNAMI
TSUNAMI IS CAUSED BY ///
• TSUNAMI as known as a seismic sea wave, is a
series of waves in a water body caused by the
displacement of a large volume of water,
generally in an ocean or a large
lake.[3] Earthquakes, volcanic eruptions and
other underwater explosions
TSUNAMI
VEDAVYAS
VEDAVYAS
BASIC CONCEPTS: RIGID PLATES
• Earth's outer shell made up of ~15 major rigid plates ~ 100 km
thick
• Plates move relative to each other at speeds of a few cm/ yr
(about the speed at which fingernails grow)
• Plates are rigid in the sense that little (ideally no) deformation
occurs within them,
• Most (ideally all) deformation occurs at their boundaries, giving
rise to earthquakes, mountain building, volcanism, and other
spectacular phenomena.
• Style of boundary and intraplate deformation depends on
direction & rate of motion, together with thermo-mechanical
structure
INDIAN PLATE MOVES NORTH
COLLIDING WITH EURASIA
MODELING
SEISMOGRAMS
shows how slip
varied on fault plane
Maximum slip area
~400 km long
Maximum slip ~ 20
m
• VEDAVYAS
VEDAVYAS
• NORMAL
MODES (ULTRA-
LONG PERIOD
WAVES) SHOW
SEISMIC
MOMENT 3
TIMES THAT
INFERRED FROM
SURFACE WAVES
• IMPLIES SLIP ON
AREA 3 TIMES
LARGER
• Entire 1200-km
long aftershock
zone likely
slipped
• V
E
D
A
V
Y
A
S
TSUNAMI - water wave generated by earthquake
TSUNAMI WARNING
• Deep ocean buoys can
measure wave heights, verify
tsunami and reduce false
Because seismic waves travel much faster
(km/s) than tsunamis, rapid analysis of
seismograms can identify earthquakes
likely to cause major tsunamis and
predict when waves will arrive
MADE
BY:
VEDAVYAS
8 ‘D’

Ppt on tsunami

  • 1.
  • 2.
    TSUNAMI IS CAUSEDBY /// • TSUNAMI as known as a seismic sea wave, is a series of waves in a water body caused by the displacement of a large volume of water, generally in an ocean or a large lake.[3] Earthquakes, volcanic eruptions and other underwater explosions
  • 3.
  • 4.
  • 5.
  • 6.
    BASIC CONCEPTS: RIGIDPLATES • Earth's outer shell made up of ~15 major rigid plates ~ 100 km thick • Plates move relative to each other at speeds of a few cm/ yr (about the speed at which fingernails grow) • Plates are rigid in the sense that little (ideally no) deformation occurs within them, • Most (ideally all) deformation occurs at their boundaries, giving rise to earthquakes, mountain building, volcanism, and other spectacular phenomena. • Style of boundary and intraplate deformation depends on direction & rate of motion, together with thermo-mechanical structure
  • 7.
    INDIAN PLATE MOVESNORTH COLLIDING WITH EURASIA
  • 8.
    MODELING SEISMOGRAMS shows how slip variedon fault plane Maximum slip area ~400 km long Maximum slip ~ 20 m • VEDAVYAS
  • 9.
    VEDAVYAS • NORMAL MODES (ULTRA- LONGPERIOD WAVES) SHOW SEISMIC MOMENT 3 TIMES THAT INFERRED FROM SURFACE WAVES • IMPLIES SLIP ON AREA 3 TIMES LARGER • Entire 1200-km long aftershock zone likely slipped
  • 10.
    • V E D A V Y A S TSUNAMI -water wave generated by earthquake
  • 11.
    TSUNAMI WARNING • Deepocean buoys can measure wave heights, verify tsunami and reduce false Because seismic waves travel much faster (km/s) than tsunamis, rapid analysis of seismograms can identify earthquakes likely to cause major tsunamis and predict when waves will arrive
  • 12.