U.S. Geological Survey
Fact Sheet 068-03

MONITORING THE ONSET OF STRUCTURAL DAMAGE

office building in Southern California badly damaged  in 1970 by a magnitude 6.4 earthquake
 
Recordings of earthquake shaking within a heavily damaged building are rare—even today. The first set of such records was obtained in 1979 from southern California when a magnitude 6.4 earthquake seriously damaged this modern office building in the Imperial Valley. The estimated cost to repair the reinforced-concrete frame and shear-wall building was so large that the building was razed. The photo at far right shows the evolving failure of columns at one end of the building. The California Geological Survey (formerly the California Division of Mines and Geology) had installed 13 motion sensors at various points throughout the structure to document its swaying and twisting in an earthquake. Shown above the building is the roof-level record of horizontal acceleration parallel to the long axis of the structure. The sudden lengthening of vibrations at A (7 seconds after shaking begins) marks the onset of structural damage. About 4 seconds later (at B), faint high-frequency vibrations (rapid small pulses), superimposed on the slower vibrations, signal the collapse of columns. Such records from buildings that suffer earthquake damage enable engineers to document and investigate failure processes and to devise and improve methods for minimizing structural damage in future shocks.

 

| MAIN TEXT |
| MONITORING ONSET OF DAMAGE | EVALUATING EARTHQUAKE PROTECTION |
|SHAKING IN AN IRREGULAR STRUCTURE | ASSESSING SAFETY | CAPTURING BUILDING PERFORMANCE |