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Seismological Research Letters; November/December 2007; v. 78; no. 6; p. 601-613; DOI: 10.1785/gssrl.78.6.601
© 2007 Seismological Society of America
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Seismic Hazard in Karachi, Pakistan: Uncertain Past, Uncertain Future

Roger Bilham1, Sarosh Lodi2, Susan Hough3, Saria Bukhary2, Abid Murtaza Khan2, and S. F. A. Rafeeqi2

The first 20% of the full text of this article appears below.

The city of Karachi, Pakistan (population 14 million), sits close to a plate boundary and within reach of earthquakes on numerous tectonically active structures surrounding the city. One can draw parallels—geologic as well as demographic—with another megacity for which seismic hazard is known to be high: Los Angeles, California (figure 1). Yet with a short historical record, limited instrumental seismic data, and little geological or geodetic constraint on slip rates, seismic hazard in Karachi is poorly characterized. In this report we present a critical review of the historical record as well as an overview of potential earthquake sources in and around Karachi.

Prior to 1800, the history of Karachi, the current capital of Sindh (one of Pakistan's four provinces), is indistinguishable from that of many fishing villages on the northern shores of the Arabian Sea. It was known to Arab and Portuguese traders who sometimes stopped at the village on the way to the Malabar coast. Colonial trade with Sindh was limited in the 18th century. Exploratory surveys starting in 1808 led to the annexation of Sindh to British rule in 1843. By 1901 Karachi had grown from a village to a town with a population of fewer than 140,000 people. The population grew to 500,000 by the time Pakistan became an independent nation in 1947, at which time the city grew dramatically with the influx of a million refugees from India. By 1960 its population exceeded 2 million, a figure that had doubled by 1980 and more than doubled again to 10 million by 2000. With an estimated annual growth rate of 3.75%, its population will exceed 30 million within two decades.

Karachi lies approximately 150 km east of the triple junction between the Arabian, Indian, and Asian plates (figure 2). The western and north-trending . . . [Full Text of this Article]

Cooperative Institute for Research in Environmental Sciences and the Department of Geological Sciences
University of Colorado at Boulder
Boulder, Colorado 80309-0399 USA
roger.bilham@colorado.edu
(R.B.)







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