About Practices Directory
Home: Practices: Civil/Structural Engineering: Earthquake Engineering: Gujarat Earthquake Reconnaissance

 

This image shows the crown of a large lateral spread, which moved downhill to the left. The failure occurred in a cultivated field. The lateral spread acted like a carpet sliding on a slippery floor; the failure surface is only about 1 to 2 feet deep, and the slope only moved laterally a few feet. Nevertheless, a structure resting on shallow foundations could have been seriously damaged by this event.

     
  The abundant sand blows that affected the Rann of Kachchh area had a remarkable side effect – the instant creation of several rivers after several years of drought. This is one of four rivers that appeared after the earthquake; the others were spotted on remote sensing images. This shot was taken on a beach that bounded an arm of the Arabian Sea some 2,500 years ago.
     
 

The earthquake that struck on January 26 was of the “blind thrust” type, one of the largest such quakes ever recorded. It occurred on a fault plane that did not break the surface of the earth, like the Northridge earthquake that hit Los Angeles in 1994. However, some small faults were found along the edge of the epicentral area, which separated the area that lurched northward in the earthquake from areas to the east that did not move. These so-called “tear faults” showed a lateral offset of about 10-25 centimeters and could be traced over 2 kilometers across the desert.

   

prev | top | next