Magnitude 6.4 - PAKISTAN

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2008 October 28 23:09:58 UTC

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Earthquake Details

  • This event has been reviewed by a seismologist.
Magnitude6.4
Date-Time
Location30.656°N, 67.361°E
Depth15 km (9.3 miles) set by location program
RegionPAKISTAN
Distances60 km (35 miles) NE of Quetta, Pakistan
190 km (120 miles) SE of Kandahar, Afghanistan
195 km (120 miles) NNE of Kalat, Pakistan
640 km (400 miles) WSW of ISLAMABAD, Pakistan
Location Uncertaintyhorizontal +/- 4.8 km (3.0 miles); depth fixed by location program
ParametersNST=166, Nph=166, Dmin=459.3 km, Rmss=1.11 sec, Gp= 25°,
M-type=regional moment magnitude (Mw), Version=A
Source
  • USGS NEIC (WDCS-D)
Event IDus2008yscs
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Earthquake Summary

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Felt Reports

One hundred sixty-six people killed, 370 injured and several villages destroyed in Balochistan. Several villages destroyed by landslides in the Ziarat area. A total of 3,487 homes destroyed and an additional 4,125 homes damaged in the Harnai area, Pishin and Ziarat. Felt (VI) at Quetta. Felt strongly in Bolan, Kalat and Qila Saifullah; and at Loralai, Mach, Mastung, Muslimbagh, and Surab. Felt (III) at Kandahar, Afghanistan.

Tectonic Summary


Earthquakes and active faults in western and northern Pakistan and adjacent parts of Afghanistan are the result of the India plate moving northward at a rate of about 40 mm/yr (1.6 inches/yr) and colliding with the Eurasia plate. Along the northern edge of the Indian subcontinent, the India plate is subducting beneath the Eurasia plate, causing uplift that produces the highest mountain peaks in the world, including the Himalayan, the Karakoram, the Pamir and the Hindu Kush ranges. West and south of the Himalayan front, the relative motion between the two plates is oblique, which results in strike-slip, reverse-slip, and oblique-slip earthquakes. The pattern of elastic waves that were radiated by the October 28 and 29, 2008, earthquakes implies that each earthquake was the result of predominantly strike-slip faulting. Seismographically recorded waveforms imply that the shocks were caused by either left-lateral slip on a northeast-striking fault or right-lateral slip on a northwest-striking fault.

The October 28 and 29 earthquakes occurred in the Sulaiman fold-and-thrust belt, a region where geologically young (Tertiary) sedimentary rocks have been folded and squeezed by forces associated with the India-Eurasia collision. The earthquakes are located approximately 80 km east of the 650-km-long Chaman fault, which is a major left-lateral strike-slip fault that accommodates a significant amount of the slip across the plate boundary. The occurrence of the earthquakes suggests that other strike-slip faults are present beneath the fold-and-thrust belt and that they accommodate some of the relative motion of the India and Eurasia plates.

The earthquakes of October 28 and 29, 2008, are located approximately 50 km northeast of the region of most intense damage from the Pakistan earthquake of May 30, 1935 (M 7.6), which is estimated to have killed 30,000 people. The 1935 earthquake probably occurred as the result of left-lateral strike-slip motion on a northeast-striking fault.

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