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     Chapter 2                                                   Selsmologlcal Aspects
                           RANN OF KUTCH
                                                  ARAVALI
                                           CAMBAY
                                                                                      SINGHBHUM
                                                        NARMADA
                            GIRNAR
                                            PANVEL
                                                                               KAKINADA-MIDNAPORE
                                               BHADRACHALAM
                                 KOYNA
                                                                ONGOLE
                            BELLARY MALABAR
                                 KERALA  IAMILNADU
                    Figure 2-4. Seismotectonic zones of the Peninsular India (Chandra 1977).
                   Figure 2-5  depicts  the reported epicenters of the earthquakes octurred in the
                   region around Jabalpur from the period 1903 to 1997, in the grid bounded by Lat-
                   itude 21°N to 26°N and Longitude 78°E to 85°E, including the epicenter of the
                   Jabalpur earthquake (1997).  The magnitude of the recorded earthquakes in this
                   region falls  in the range of 38 to  6.5.  There are six  moderate size earthquakes
                   (5<M<7)  and eight small size earthquakes (M<5),  which have occurred in this
                   grid. Out of the 14 reported earthquakes there are two earthquakes having mag-
                   nitude greater than 6.  The above seismotectonic scenario demonstrates that the
                   Narmada seismic zone is characterized by the moderate earthquake activity in
                   the magnitude range of 5 to 6.5. The Jabalpur earthquake which have occurred in
                                     Jabalpur Earthquake of May 22,  1997                      22





