UTC time | 2004-02-14 10:30:22 |
---|---|
ISC event | 7251179 |
USGS-ANSS | ComCat |
Local date | 14 February 2004 |
Local time | 15:30 |
Magnitude | 5.5 Mw |
Depth | 11.0 km (6.8 mi) |
Epicenter | 34°46′26″N73°12′58″E / 34.774°N 73.216°E |
Areas affected | Pakistan |
Max. intensity | MMI VIII (Severe) [1] |
Landslides | Yes |
Casualties | 24 dead, 63 injured |
An earthquake struck Khyber Pakhtunkhwa Province, Pakistan on February 14, 2004. Extensive damage occurred and 24 people lost their lives.
Northern Pakistan 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. [2] 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. Many damaging earthquakes have resulted from movement on such thrust faults, such as the 2005 Kashmir earthquake which caused the deaths of around 87,000 people.
Eleven people were killed and 63 were injured by collapsing houses. Thirteen others were also killed and one was left missing when a landslide hit a minibus and fell into a deep ravine in Battagram. [3] [4] 564 houses were destroyed and 2,262 were damaged in the earthquake. [4] [5]
The Pakistani government supported affected families by giving 100,000 rupees for a deceased family member and 20,000 rupees for every injured person. [4]
The 2001 Gujarat earthquake, also known as the Bhuj earthquake, occurred on 26 January at 08:46 am IST. The epicentre was about 9 km south-southwest of the village of Chobari in Bhachau Taluka of Kutch (Kachchh) District of Gujarat, India.
The Great Sumatran fault, also known as Semangko fault, is a large strike-slip fault running the entire length of the island of Sumatra. This Indonesian island is located in a highly seismic area of the world, including a subduction zone off the west coast of the island.
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The 2008 Ziarat earthquakes hit the Pakistani province of Balochistan on October 29 with a moment magnitude of 6.4. The US Geological Survey reported that the first earthquake occurred 60 km (37 mi) north of Quetta and 185 km (115 mi) southeast of the Afghanistan city of Kandahar at 04:09 local time at a depth of 15 km (9.3 mi), at 30.653°N, 67.323°E. It was followed by another shallower magnitude 6.4 earthquake at a depth of 14 km (8.7 mi) approximately 12 hours after the initial shock, at 30.546°N, 67.447°E. 215 people were confirmed dead. More than 200 were injured, and 120,000 were rendered homeless. Qamar Zaman Chaudhry, director general of Pakistan Meteorological Department, stated the quake epicenter was 70 miles (110 km) north of Quetta, and about 600 km (370 mi) southwest of Islamabad.
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The 2019 Kashmir earthquake struck regions of Pakistan with an epicentre in Azad Kashmir on 24 September at 16:02 local time. It had a magnitude of 5.4 Mww and a maximum felt intensity of VII on the Modified Mercalli intensity scale or VIII on the European macroseismic scale. There was severe damage in Mirpur District, causing the deaths of 40 people and injuring a further 850. The epicentre of the shallow quake was near the city of Mirpur, Pakistan. The tremors were felt in the Kashmir region, Punjab (Pakistan), Punjab (India), Uttarakhand and northern parts of India including New Delhi.
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An earthquake struck Pakistan's province of Balochistan near the city of Harnai on 7 October 2021. The moment magnitude 5.9 Mww quake struck in the early morning at 03:01 local time, killing at least 42 people and injuring 300 others. The earthquake occurred just one day before the anniversary of the 2005 Kashmir earthquake.
The 1654 Tianshui earthquake occurred on July 21 in Tianshui, Gansu Province, Ming dynasty sometime between 21:00 and 23:00 local time. The event had an estimated moment magnitude of 7.0 and was assigned a maximum intensity of XI on the China seismic intensity scale. Resulting in extreme damage and affecting at least four provinces, the quake killed approximately 30,000 people.
The 1885 Kashmir earthquake, also known as the Baramulla earthquake occurred on 30 May in Srinagar. It had an estimated moment magnitude of Mw 6.3–6.8 and maximum Medvedev–Sponheuer–Karnik scale intensity of VIII (Damaging). At least 3,081 people died and severe damage resulted.
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The 1957 Farsinaj earthquake struck Hamadan province, Iran on 13 December at 05:15 local time. The moment magnitude 6.5 earthquake struck at a depth of 15 km (9.3 mi). The epicenter of the earthquake was located in the seismically active Zagros Mountains. The mountain range was also the location for several historic earthquakes. The earthquake occurred near two segments of the active strike-slip Main Recent Fault. At least 1,130 people died, including over 700 in the village of Farsinaj. Additional deaths also occurred in Dehasiyab, Sarab, and other villages. The earthquake left an estimated 15,000 homeless; poor weather conditions including a winter storm on 21 December killed another 20 people. Several deadly and damaging aftershocks in that month killed a total of 38 people.