Page 199 - Science Class 08
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Epicentre                                             of an earthquake at a par cular place. Intensity

              Epicentre of an earthquake is the point on the        is  determined  from  observa ons  of  an  earth-
              earth’s surface that is directly above the focus.     quake’s  effect  on  people,  structure  and  the
              Distance from epicentre to any point of interest      earth’s surface.
              is called epicentral distance.                        There  are  two  major  scales  in  which  earth-

              Magnitude                                             quakes  are  measured.  These  two  scales  are—
                                                                    the Mercalli Scale and the Richter Scale.
              Earthquake  magnitude  is  the  measure  of  the
              strength of an earthquake or the strain energy        Richter Scale
              released  by  it.  It  is  calculated  from  the      On a Richter Scale, only units from 1 to 10 are
              instrument  record  made  by  the  event  on  a       used. But, unlike many other scales in Science,
              calibrated seismic-graph.                             Richter Scale is not linear. This means, each one
                                                                    unit on this increase in the earthquake strength.
                                                                    Therefore, an increase of 2 in magnitude means

                                                                    1000  mes more destruc ve energy.
                                                                                SEISMIC ZONES IN INDIA
                                                                    You have studied that earthquakes are caused
                                                                    by  the  movement  of  plates,  the  boundaries

                                                                    of the plates are the weak zones where earth-
                                                                    quakes  are  more  likely  to  occur.  The
                                                                    weak zones are also known as seismic or fault
              Seismograph                                           zones.
              Seismograph  is  simply  a  vibra ng  rod  or  a                                                    ZONE 1
              pendulum  which  begins  to  vibrate  as  soon  as                                                  ZONE 2
                                                                                                                  ZONE 3
                                                                                                                  ZONE 4
              tremors  occurs.  A  pen  is  a ached  to  the                                                      ZONE 5
              vibra ng  system.  The  pen  records  the  seismic                                CHINA
              waves  on  a  paper  which  moves  under  it.  The       PAKISTAN                 TIBET

              scien sts  analyse  these  waves  to  construct  a                           NEPAL
                                                                                                     BHUTAN
              complete map of the earthquake. They can also
              es mate its power to cause destruc on.               Tropic of Caner
                                                                                                             MYANMAR
                                                  Frame                                            BANGLADESH
                   Wire
                                                  Weight              ARABIAN                       BAY
                                                                                                    OF
                                                                       SEA                         BENGAL
                                                  Rota ng Drum
               Vibra ons
                                                                                          ZONE 1  Intensity 5 or below
                                                                                              (moderate)
                                                                                          ZONE 2  Intensity 6 (strong)
                                                                                          ZONE 3  Intensity 7 (very strong)
                                                                                          ZONE 4  Intensity 8 (destructive)
                   Base                                                (INDIA)  LAKSHADWEEP   ZONE 5  Intensity 9 and above
                                                                                              (very disastrous)
                                  Seismograph
                                                                                      SRI
                                                                                      LANKA
              Intensity
                                                                               I  N  D  I  A    O  C  E  A  N
              Earthquake intensity is a measure of the effects                     Earthquake Prone Areas

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