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Damage Patterns
This chapter provides an overview of the macroseismic effects of the Bhuj earthquake. Such
information is useful for several reasons. First, direct information about the vulnerability of
structures to strong ground motion is useful for assessing, and perhaps mitigating, the hazard posed
to similar structures by future large earthquakes. Secondly, given the paucity of instrumental
recordings of the Bhuj earthquake, macroseismic data can provide useful information about the
spatial variation of ground motions. Finally, detailed damage assessments for this earthquake can
be compared to available accounts of historic earthquakes in India and other similar tectonic
regimes around the world. These comparisons will provide additional insight into the magnitude
of important earthquakes for which there are few or no instrumental recordings.
The Bhuj earthquake is of particular interest because of the possibility that it represents an analog
for the principal New Madrid (central United States) earthquakes of 1811-1812. The Bhuj earthquake
occurred much closer to an active plate boundary than did the New Madrid events, and the Bhuj
earthquake might therefore be considered a plate boundary-related event. However, in both cases, the
regions primarily affected by the earthquake are stable continental interiors with low attenuation.
A quantification of damage patterns, such as that presented in this chapter, can provide useful
insight into the attenuation and frequency content of ground motions, which may in turn be useful
in resolving whether the Bhuj earthquake should be considered interplate or intraplate for the
purpose of data classification.
This chapter combines two different approaches to quantify macroseismic effects of the Bhuj
earthquake. First, a large-scale map of intensities was compiled based on media accounts. Second,
ground-level surveys of damage in towns and villages across the epicentral area by the India-U.S.
Geotechnical Earthquake Engineering Reconnaissance Team were synthesized. This approach
provides both coarse- and fine-scale overviews of damage, as well as an opportunity to compare
detailed ground-based intensity results to a "broad brush" intensity value determined from one or
a small handful of media accounts for any one location