ANATOMY OF AN EARTHQUAKE
POWERFUL VIBRATIONS ARE RELEASED DUE TO
THE MOVEMENT OF THE EARTHS PLATES.
THESE VIBRATIONS TRAVEL IN THREE TYPES OF
WAVES:
P-WAVES OR PRIMARY WAVES
S-WAVES OR SECONDARY WAVES OR SHEAR
WAVES
L-WAVES OR LONG WAVES OR SURFACE WAVES
PRIMARY WAVES
 PARTICLES VIBRATE IN
THE DIRECTION OF
WAVES
 CAN PASS THROUGH
SOLID LIGUID AND
GASES
 FIRST TO BE
RECORDED ON
SEISMOGRAPH
SECONDARY OR SHEAR WAVES
 PARTICLES VIBRATE AT
RIGHT ANGLES TO
THE DIRECTION OF
MOVEMENT OF THE
WAVE
 CANNOT PASS
THROUGH LIQUIDS
 RECORDED AFTER P
WAVES ON
SEISMOGRAPH
LONG OR SURFACE WAVES
 TRAVEL ALONG THE
SURFACE OF THE
EARTH
 RECORDED AFTER
PRIMARY AND
SECONDARY WAVES
 TWO TYPES OF L
WAVES ARE:LOVE
WAVES AND RAYLEIGH
WAVES
MEASUREMENTS
SEISMOGRAPH
RICHTER SCALE
MERICALLI SCALE
SEISMOGRAPH
 TO MEASURE DIRECTION
OF MOVEMENT OF WAVES
 IT HAS A PEN ATTACHED
TO IT THAT RECORDS THE
MOVEMENTS OF THE
WAVES ON A STRIP OF
PAPER.
 ALSO CALCULATES THE
DIFFERENCE BETWEEN
THE RECORDING STATION
AND EPICENTRE BY
CALCULATING THE
DIFFERENCE IN ARRIVAL
OF P AND S WAVES.
RICHTER SCALE
 TO MEASURE
INTENSITY (THE
AMOUNT OF ENERGY
RELEASED DURING AN
EARTHQUAKE)
 MEASURES THE
POWER OF AN
EARTHQUAKE ON A
SCALE OF ONE TO
NINE
MERICALLI SCALE
 TO MEASURE
INTENSITY (THE
AMOUNT OF ENERGY
RELEASED DURING AN
EARTHQUAKE)
 GRADES THE
EARTHQUAKES ON
THE BASIS OF
OBSERVED EFFECTS
ON A -12 POINT SCALE
SHANSHI (CHINA -1556),830000
KILLED
KOLKATA -1737,300000 KILLED
CONSTRUCTIVE EFFECTS OF
EARTHQUAKES
ENERGY RELEASE:
i. EARTH RELEASES ITS
STORED UP ENERGY
ii. ENERGY RELEASE
HELPS IN KEEPING
THE EARTH IN A
PROPER SHAPE
LANDFORMS
IN THE OCEAN BELTS
THE EARTHS CRUST
MAY BE EITHER
RAISED OR LOWERED
DUE TO VERTICAL OR
LATERAL
DISPLACEMENT.
EARTHQUAKE
EARTHQUAKE

EARTHQUAKE

  • 3.
    ANATOMY OF ANEARTHQUAKE POWERFUL VIBRATIONS ARE RELEASED DUE TO THE MOVEMENT OF THE EARTHS PLATES. THESE VIBRATIONS TRAVEL IN THREE TYPES OF WAVES: P-WAVES OR PRIMARY WAVES S-WAVES OR SECONDARY WAVES OR SHEAR WAVES L-WAVES OR LONG WAVES OR SURFACE WAVES
  • 4.
    PRIMARY WAVES  PARTICLESVIBRATE IN THE DIRECTION OF WAVES  CAN PASS THROUGH SOLID LIGUID AND GASES  FIRST TO BE RECORDED ON SEISMOGRAPH
  • 5.
    SECONDARY OR SHEARWAVES  PARTICLES VIBRATE AT RIGHT ANGLES TO THE DIRECTION OF MOVEMENT OF THE WAVE  CANNOT PASS THROUGH LIQUIDS  RECORDED AFTER P WAVES ON SEISMOGRAPH
  • 6.
    LONG OR SURFACEWAVES  TRAVEL ALONG THE SURFACE OF THE EARTH  RECORDED AFTER PRIMARY AND SECONDARY WAVES  TWO TYPES OF L WAVES ARE:LOVE WAVES AND RAYLEIGH WAVES
  • 8.
  • 9.
    SEISMOGRAPH  TO MEASUREDIRECTION OF MOVEMENT OF WAVES  IT HAS A PEN ATTACHED TO IT THAT RECORDS THE MOVEMENTS OF THE WAVES ON A STRIP OF PAPER.  ALSO CALCULATES THE DIFFERENCE BETWEEN THE RECORDING STATION AND EPICENTRE BY CALCULATING THE DIFFERENCE IN ARRIVAL OF P AND S WAVES.
  • 10.
    RICHTER SCALE  TOMEASURE INTENSITY (THE AMOUNT OF ENERGY RELEASED DURING AN EARTHQUAKE)  MEASURES THE POWER OF AN EARTHQUAKE ON A SCALE OF ONE TO NINE
  • 11.
    MERICALLI SCALE  TOMEASURE INTENSITY (THE AMOUNT OF ENERGY RELEASED DURING AN EARTHQUAKE)  GRADES THE EARTHQUAKES ON THE BASIS OF OBSERVED EFFECTS ON A -12 POINT SCALE
  • 12.
  • 13.
  • 14.
    CONSTRUCTIVE EFFECTS OF EARTHQUAKES ENERGYRELEASE: i. EARTH RELEASES ITS STORED UP ENERGY ii. ENERGY RELEASE HELPS IN KEEPING THE EARTH IN A PROPER SHAPE
  • 15.
    LANDFORMS IN THE OCEANBELTS THE EARTHS CRUST MAY BE EITHER RAISED OR LOWERED DUE TO VERTICAL OR LATERAL DISPLACEMENT.