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  Gujarat Earthquake Safety Initiative  
  A Case Study In Gujarat, India  
     
 

Identifying Earthquake-Unsafe Schools and Setting Priorities to Make Them Safe

 
     
 

After the January 26, 2001 Gujarat Earthquake, GeoHazards International (GHI) was concerned about the risk of school buildings in the largest Gujarat cities and asked the Volunteers for India Development and Empowerment (VIDE) and NGOs Kobe to help fund a study that would identify earthquake-unsafe school buildings in Ahmedabad, Baroda and Surat. VIDE and NGOs Kobe agreed to help. GHI worked with its Indian partner organization, SEEDS, to evaluate 153 schools: 42 in Ahmedabad, 58 in Baroda, and 53 in Surat. The schools included different structural types, served students from a variety of educational and economic levels, and were widely dispersed within each city.

GHI found that the earthquake risk of the schools in all three cities was and is significant, and recommended that the authorities responsible for these schools take steps to reduce the risk. GHI further recommended that these authorities initiate comprehensive school earthquake risk mitigation programs. GHI and SEEDS met with officials in these three cities to discuss these findings and follow-up actions.

Gujarat State is a highly earthquake-prone region in western India. Past earthquakes have devastated almost all parts of the state. There have been thirty-three significant earthquakes that struck the region since 893-894 A.D. 33 Significant Earthquakes The figure below shows the location of Ahmedabad, Baroda and Surat, and the location of selected historic earthquake epicenters, their date of occurrence and number of fatalities. Figure 2 in the full downloaded report (to the right) depicts the Seismic Zoning Map of India. The cities in this report lie in Zone 3 where, according to current Indian standards (IS: 1893-2002), peak ground accelerations of 0.16g and seismic intensities of VII MMI can reasonably be expected to occur once during the design life of a structure. The seismic zoning map is based on the intensity from likely earthquakes, and does not follow the current worldwide fashion of specifying zones in terms of ground acceleration (a measure of earthquake shaking intensity) with a certain probability of being exceeded in a given number of years.

 
     
     
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