The National Disaster Management Authority (NDMA) reports 155 deaths and more than 375 people injured, with media reporting more than 300 deaths. NASA image created by Jesse Allen, using data obtained from the The shape is repeated in the southeast by the wide belt of vegetation (dark green) along the banks of the Indus River. Geodyn Pak 285–294Kazmi AH (1979b) The Bibai and Gogai Nappes in the Kach-Ziarat area of Northeastern Baluchistan. Depths of events were 15Km and 12 km respectively. Geodyn Pak 341–350Guralp systems (2007) Scream software. There was another severe shock on 2nd June,Killed about 30000 to 60000 peopls. The quake and aftershocks caused building collapses and landslides northeast of the city of Quetta that killed at least 160 people and left at least 15,000 people homeless, according to reports from BBC news.Pakistan is prone to earthquakes because it lies in the collision zone of the India tectonic plate to the south and the Eurasian plate to the north. South of the city of Quetta, the folded rocks line up generally north-south, but to the east, the mountains have been bent into a “U†shape. Depths of events were 15 and 12 km, respectively. A magnitude 6.4 earthquake hit the rural, mountainous region of southwestern Pakistan on October 29, 2008, at 4:09 a.m. local time (October 28 at 23:09 UTC). The earthquake caused destruction in almost all the towns close to Quetta, including the city … Seismosoft (2011) Earthquake engineering software and solutions. As many as 3,000 people may have been displaced as nearly 2,000 houses were destroyed by the earthquake. The 2008 Ziarat earthquakes hit the Pakistani province of Balochistan on October 29 with a moment magnitude of 6.4. This color-coded map shows the topography, bathymetry, fault lines, and earthquake locations related to earthquakes in New Britain on July 18–19, 2010. In affected areas, night temperatures have This image originally appeared in the NASA Earth Observatory story Subscription will auto renew annually.Over 10 million scientific documents at your fingertips Pakistan is prone to earthquakes because it lies in the collision zone of the India tectonic plate to the south and the Eurasian plate to the north. A magnitude 6.4 earthquake hit the rural, mountainous region of southwestern Pakistan on October 29, 2008.
(In October 2005, an even The India plate is drifting generally northward and ramming into the Eurasia plate. Geol Soc Lond 9:363–370, Special publicationNiamatullah M, Durrani KH, Qureshi AR, Khan Z, Kakar DM, Jan MR, Ghaffar A (1989) Emplacement of Bibai and Gogai Nappes, NE of Quetta. doi:Abd El-Aal AK, Mohamed AA (2010) Near-surface seismic refraction applied to exploring subsurface clay layer at a new mining area in southeast Cairo, Egypt. A catalog of NASA images and animations of our home planet Immediate online access to all issues from 2019. The first tremor struck at 4:09 am local time (23:09 GMT) at a depth of 15 kilometer while the second one jolted area at 5:35pm.
Previous studies have come up with different models for these earthquake swarms. Jadoon AK, Khurshid A (1996) Gravity and tectonic model across the Sulaiman fold belt and the Chaman fault zone in western Pakistan and eastern Afghanistan. The epicentre of the quake was established to be 4-kilometres south-west of the town of Ali Jaan in Balochistan, some 153-kilometres away from Quetta in British India. Pak J Hydrocarb Res 4(1):9–31Lawrence RD, Khan SH, DeJong KA, Farah A, Yeats RS (1981) Thrust and strike slip fault in interaction along the Chaman transform zone, Pakistan.
2), followed by a doublet on the very next day, with the same magnitude of 6.4 (Table 1).Focal mechanism solutions for the earthquakes revealed strike-slip mechanisms, which was unexpected in light of the dominance of nearby thrust faults (Yadav et al. The area where the October 29 quake occurred seems to sit near a pivot point in different fold belts. The Pakistan meteorological department put the magnitude of today's quake at 6.5. On 31st May 1935 at 3.40 am in the early morning the city of Quetta and the countryside for 100 miles to the south-west including the town of Khelat were devastated by a severe earthquake which lasted three minutes. Earthquake in Quetta - 2008 Quetta (October 30, 2008): More than 150 people were killed around Quetta when a magnitude 6.4 earthquake struck before dawn and destroyed as many as 20 villages. An earthquake of magnitude 6.5 Mb occurred on 29 October 2008 near Chiltan hills, Balochistan Province, in Pakistan with a foreshock of magnitude 5.0 Mb.
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