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                Earthquakes in 
                Madhya Pradesh, India  | 
               
             
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                   State 
              - Madhya Pradesh, India 
              
              Capital 
              - Bhopal 
              
              
              Population 
              - 
              60,385,118
              (2001) 
              
               
              
                  Million+ Cities 
              
                  
                  
              Indore 
              - pop. 
              1,639,044 
              
                  
                  
              Bhopal 
              - pop. 
              1,454,830 
              
                  
                  
              Jabalpur 
              - pop. 
              1,117,200 
               
              
                  Population per 
              district (Top 5) 
              
                  
                  
              Indore
              - pop. 2,465,827 
              Jabalpur 
              - pop. 2,151,203 
              Sagar - pop. 2,021,987 
              Rewa - pop. 1,973,306 
              Satna - pop. 1,870,104  
            
           
          
            
          
            
            Earthquake History 
            In peninsula 
          India the state of Madhya Pradesh, along with Gujarat and Maharashtra, 
          has suffered from frequent earthquakes, both deadly and damaging, 
          although not located on or near any plate boundaries. All the 
          earthquakes here, as in all of peninsula India, are intraplate events. 
          Most of the activity is confined to the 
          Narmada-Son fault zone which runs across the state. Several faults 
          have been identified in this region out of which many show 
          evidence of movement (1) 
          during the Holocene epoch. Among them and the most prominent is the 
          Narmada-Son South Fault (1) 
          zone that runs from near Khargaon in western Madhya Pradesh in an 
          east-northeasterly direction right upto the Rihand reservoir in 
          southern Jharkhand in the east. The Gavilgadh Fault (1) 
          extends from near Bhusawal in Maharashtra and extends up
          to Seoni district in Madhya Pradesh. In the north, the Great 
          Boundary Fault (1) runs along 
          the Chambal river which forms the state border with Rajasthan. This 
          fault has repeatedly reactivated in the past (1) 
          changing the course of the Chambal and Yamuna rivers. However, it must 
          be stated that proximity to faults does not necessarily translate into 
          a higher hazard as compared to areas located further away, as damage 
          from earthquakes depends on numerous factors such as subsurface 
          geology as well as adherence to the building codes. 
            
          
          
Seismic Hazard 
            
          
The seismic hazard map of India was 
updated in 2000 (5) by the Bureau of 
Indian Standards (BIS). Apart from the merging of Zones I and II into Zone II in 
the latest map, there are no major changes from the BIS 1984 map. Zone III 
stretches across the length of the state, and includes all the districts that 
lie in the Narmada and Son Valleys, where the maximum expected intensity is VII 
(MSK). The rest of the state, i.e. north and south of the Narmada-Son Valleys, 
including the capital, Bhopal, lie in Zone II, where the maximum expected 
intensity is VI (MSK).
Since the earthquake database in 
India is still incomplete, especially with regards to earthquakes prior to the 
historical period (before 1800 A.D.), these zones offer a rough guide of the earthquake hazard in any 
particular region and need to be regularly updated 
(See also:
GSHAP Hazard Map for Madhya Pradesh). 
  
          
Largest Instrumented 
Earthquake in 
Madhya Pradesh 
02 June 1927 - Umaria area, Madhya Pradesh, Mw 6.4 (9) 
23.500 N, 81.000E, 16:37:34 UTC (9) 
This earthquake was located in Madhya Pradesh's Umaria District.  It was a 
deep-seated event and was felt (12) at 
Allahabad in Uttar Pradesh and Dehri-on-Son in Bihar as well 
as in many parts of central and eastern India. 
  
          
          
Significant 
Earthquakes  in 
Madhya Pradesh 
          The following list briefly outlines known earthquakes in this region 
which either had observed intensities of 
VI 
or higher (historical 
events) or had known magnitudes of 
M5.0 or more 
(instrumented events). General locations are provided for historical events for 
which "generalized" epicentral co-ordinates are available.
Some events which were significant for other reasons are also included. 
This list will be updated whenever newer information is available. Please note 
that Magnitude and Intensity are NOT THE SAME. All events are within the state 
or union territory covered on this page unless stated otherwise.  
           
          Acronyms Used: 
D=Depth, 
OT=Origin 
Time, Mw=Moment 
Magnitude, Ms=Surface 
Wave magnitude, 
Mb=Body 
Wave Magnitude, ML=Local 
Magnitude, M?=Magnitude 
Type unknown 
                
                  
                  
                    
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                      This listing will be modified 
                      without notice. Please check back for the latest version 
                      when using it elsewhere. Additionally, please
                      reproduce using appropriate
                      
                      
                      CITATIONS/CREDITS.  | 
                     
                   
                  
             
            
             
            18 November 1863 - Nagalwadi-Julwania area, Madhya Pradesh. 
            21.800 N, 75.300 E (6) 
            Maximum observed intensity VI (6). 
            This region lies along the border of Maharashtra in the Khandwa area 
            of Madhya Pradesh. 
             
            17 May 1903 - Bargi-Jabalpur area, Madhya Pradesh, Ms 5.0 (1). 
            23.000 N, 80.000 E (1) 
            Maximum observed intensity VI (6).
             
             
            31 December 1926 - Badarwas-Digod area, Madhya Pradesh. 
            25.000 N, 77.500 E, OT=16:53:45 UTC (7) 
            Maximum observed intensity VII (7).  
             
            02 June 1927 - Umaria area, Madhya Pradesh, Mw 6.4 (9) 
            23.500 N, 81.000E, 16:37:34 UTC (9) 
            This earthquake was located in Madhya Pradesh's Umaria District.  It 
            was a deep-seated event and was felt (12) at 
            Allahabad in Uttar Pradesh and Dehri-on-Son in Bihar 
            as well as in many parts of central and eastern India. 
             
            11 April 1929 - Badarwas-Digod area, Madhya Pradesh. 
            25.000 N, 77.500 E, OT=23:53 UTC (7) 
            Maximum observed intensity VII (7).  
             
            25 June 1930 - Sirsod-Shivpuri area, Madhya Pradesh, Ms 5.6 (1) 
            25.500 N, 77.500 E (1), 
            OT=00:49 UTC (7) 
            Maximum observed intensity VII (7). This earthquake 
            is also referred to as the Lukwasa earthquake. 
             
            14 March 1938 - Bhusawal-Sawda area, Maharashtra, Mw 6.3 (9). 
            21.130 N, 75.830 E, D=040.0 kms, OT=00:48:38 UTC (1) 
            Maximum observed intensity VII (1). 
            This earthquake was felt over a wide region, including at Agra in 
            the north and Mumbai in the west. Deep-seated event (9), 
            with a focal depth (JSTN) of 40 kilometres. 
             
            25 August 1957 - Lalburra-Tikari area, Madhya Pradesh, Ms 5.5 (1). 
            22.000 N, 80.000 E, OT=21:04:50 UTC (1) 
            The district of Balaghat in Madhya Pradesh and Bhandara in 
            Maharashtra were affected. 25 fatalities are reported for this 
            event. The epicentre of this earthquake was north of the town of 
            Waraseoni in Madhya Pradesh and the town of Gondia in Maharashtra. 
             
            18 April 1987 - Paunar-Amarwara area, Madhya Pradesh, mb 4.9 (8). 
            22.346 N, 79.259 E, D=033.0 kms, OT=16:59:48 UTC (8) 
            Felt in the epicentral area. 
             
            31 August 1994 - Gwalior-Gohad (Bhind) 
            area, Madhya Pradesh, Ms 4.8 (3) 
            26.300 N, 78.400 E, D=008.0 kms, OT=23:30:00 UTC (3) 
            Maximum observed intensity MSK VI and VII (1) 
            in an area to the south of Bhind and east of Gwalior. Felt at MSK 
            IV-V (1) in many northern 
            districts of Madhya Pradesh and adjoining areas of Uttar Pradesh and 
            Rajasthan. This event is known as the Bhind earthquake. 
             
            22 May 1997 - Barela-Jabalpur area, Madhya Pradesh, Mw 5.8 (8) 
            23.083 N, 80.041 E, D=036.0 kms, OT=22:51:28 UTC (8) 
            38 people were killed, and more than a thousand were hurt in the 
            city of Jabalpur and the surrounding areas. This was the first major 
            earthquake to be centred near a densely populated urban area since 
            1947.  
             
            16 October 2000 - 
            
            Kundam area, Madhya Pradesh, Mb
            4.4 
            A 
              light earthquake struck Jabalpur and the 
            adjoining parts of eastern Madhya Pradesh, on 16 
            October 2000 at 18:11 PM local time and was felt in many parts of 
            the region resulting in minor damage. It 
              had a magnitude of Mb=4.4.  
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          References  
          
          
          01)
          Dasgupta, S., Pande, P., Ganguly, D., Iqbal, Z, Sanyal, K, 
          Venkatraman, N.V., Dasgupta, S., Sural, B., Harendranath, L., Mazumdar, 
          K., Sanyal, S., Roy, K., Das, L.K., Misra, P.S., Gupta, H.,  "Seismotectonic 
          Atlas of India and its Environs", Geological Survey of India, 2000. 
           
          02) Giardini, D., 
          Grünthal, G., Shedlock, K.M., 
          Zhang, P., "The GSHAP Global Seismic Hazard Map", Annali di Geofisica, 
          Vol. 42, No.6, p. 1225 - 1230, 1999. 
           
          03) India Meteorological Department, Lodhi Road, New 
          Delhi. 
           
          04) International Seismological Centre, On-line 
          Bulletin, http://www.isc.ac.uk/Bull, Internatl. Seis. Cent., Thatcham, 
          United Kingdom, 2001. 
           
          05) IS 1893 (Part 1): 2002 Indian Standard 
          Criteria for Earthquake Resistant Design of Structures Part 1 General 
          Provisions and Buildings (Fifth Revision). 
           
          06) Rao, B. Ramalingeswara and Rao, P. 
          Sitapathi, "Historical seismicity of 
          Peninsular India", Bulletin of the 
          Seismological Society of America, Vol. 74, No. 6, pp.2519-2533, 
          1984. 
           
          07) Tandon, A.N., and Srivastava, H.N.,
          "Earthquake occurrence in India: Earthquake 
          Engineering (Jai Krishna Vol.)", pp. 1 - 48, 
          Sarita Prakashan, Meerut, 1974. 
           
          08) U.S. Geological Survey, National Earthquake 
          Information Center, Golden, CO, USA. 
           
          09) Johnston, A.C., Report TR-102261, Electric 
          Power Research Institute, Chap.3, 1993. 
           
          10) Ambraseys, N. and Jackson, D., "A note on early 
          earthquakes in northern India and southern Tibet", Current Science, 
          Vol. 84, No. 4, 25 February 2003. 
           
          11) Iyengar, R.N, Sharma, 
          D, and Siddiqui, J.M, "Earthquake History of India in Medieval Times", 
          Indian Journal of history Science, 34 (3), 
          1999. 
           
          12) Chandra, U.,
          "Earthquakes of Peninsular India--A 
          seismotectonic study", Bulletin of the 
          Seismological Society of America, Vol. 67, No. 5, pp. 1387 - 1413, 
          1977. 
           
          13) Wessel, P., and Smith, 
          W.H.F., "Free software helps map and display data", EOS Trans., AGU, 
          1991, 72, 441, 445.
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