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2005 Kashmir earthquake

Earthquake in South Asia

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  • 5 chapters

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Through Pakistan, Tehsil and Lahore

At least 87,350 people were killed and 200,000 were injured in Pakistan, with an additional 1,360 deaths and 7,082 injuries in India and 4 deaths in eastern Afghanistan. Among the fatalities were 26,000 killed by landslides, 19,000 students and teachers killed by collapsing schools, and 317 Pakistani and Indian military personnel. Muzaffarabad, Balakot, Bagh and Battagram were the worst-affected areas in Pakistan; all 4,000 inhabitants in the destroyed village of Jabri Kailash died. Severe damage also occurred in Kupwara and Baramulla districts in India, with the tehsil of Karnah almost completely destroyed. More than 856,400 buildings and houses were severely damaged or destroyed in Pakistan and India, with buildings collapsing as far away as Lahore. More than 3.5 million people were displaced, resulting in a severe humanitarian crisis for the region.

Tectonic setting

Kashmir lies at the southern margin of the broad zone of continental collision between the Eurasian and Indian plates. The rate of convergence between these plates near this location is 38 mm per year. The main structures involved in accommodating this convergence are large thrust faults, such as the Main Central Thrust and the Main Frontal Thrust. Within the frontal thrust zone, there are many individual thrust faults.

The region where the 2005 earthquake occurred crosses the political borders of Pakistan, India and neighboring countries. The earliest recorded quake occurred in 1255 in Kathmandu, Nepal. The Kashmir valley is completely surrounded by mountains, with the valley floor being 1,850 m (6,070 ft) above sea level, but the encircling mountains reach heights of 3,000–4,000 m (9,800–13,100 ft). Its unique geography makes it particularly prone to natural disasters, including floods, windstorms, avalanches, landslides, fires and droughts. It is, however, particularly prone to earthquakes as it lies on top of active geological faults where two tectonic plates, the large Eurasian and small Indian tectonic plates collide. This collision forces the Indian plate under the Eurasian plate, causing movement of the earth's crust.

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