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              A mild
              earthquake struck the 
              border areas of the states of Maharashtra, Madhya Pradesh and 
              Gujarat on 27 July 2003 
              at 10:05 AM local time. It caused some 
              minor damage in the region and had a magnitude of
              ML=3.8. 
               
              
               
              
              The earthquake 
              was centred 3.7 kms NE of Sindvani 
              (Maharashtra), India, 
              14.5 kms NE of Dhadgaon (Maharashtra), India, 
              37.9 kms NNE of Taloda (Maharashtra), India, 
              58 kms N of Nandurbar (Maharashtra), India, 
              60.3 kms WSW of Barwani (Madhya Pradesh), India, 
              86.5 kms E of Rajpipla (Gujarat), India, 
              118 kms NNW of Dhule (Maharashtra), India, 
              128 kms SE of Vadodara (Gujarat), India. 
            
            
              
              The tremor was felt strongly at Dhadgaon (Nandurbar), Maharashtra. 
              One wall collapse was reported from here and many other 
              buildings developed cracks. Roof tiles  fell off many 
              buildings and household articles were displaced or fell down. 
               
              The quake was felt at Dediapada, Rajpipla, Sagbara and Tilakwada talukas of 
              Narmada district and Kawant taluka in Vadodara district of 
              Gujarat. It was also felt at Kevadia Colony in the vicinity of the 
              Sardar Sarovar Dam in the Narmada district. It was also 
              felt in Akkalkuva, Molgi, Nandurbar, Shahada and Taloda talukas of 
              Nandurbar District in Maharashtra. In the town 
              of Taloda if was felt for several 
              seconds.  | 
          
          
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              References 
              01)
              India Meteorological Department (IMD), 
              Delhi. 
              02) 
              International Seismological Centre (ISC), Berkshire, UK. 
              
              03) 
              Macroseismic information has been compiled by 
              the ASC from reports by local media and local NGO personnel. 
             
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