  | |
| UTC time | 2022-09-04 21:57:35 |
|---|---|
| ISC event | 624749335 |
| USGS-ANSS | ComCat |
| Local date | September 5, 2022 |
| Local time | 02:27 |
| Magnitude | 5.1 Mw |
| Depth | 10 km (6.2 mi) |
| Epicenter | 34°39′43″N70°42′04″E / 34.662°N 70.701°E |
| Fault | Reverse |
| Max. intensity | MMI VII (Very strong) |
| Casualties | 18 dead, 42 injured |
On September 5, 2022, a reverse faulting earthquake with a moderate magnitude of 5.1 struck Kunar Province, Afghanistan, close to the city of Jalalabad. [1]
Much of Afghanistan is situated in a broad zone of continental deformation within the Eurasian Plate. Seismic activity in Afghanistan is influenced by the subduction of the Arabian Plate to the west and the oblique subduction of the Indian Plate in the east. The subduction rate of the Indian Plate along the continental convergent boundary is estimated to be 39 mm/yr or higher. Transpression due to the plates interacting is associated with high seismicity within the shallow crust. Seismicity is detectable to a depth of 300 km (190 mi) beneath Afghanistan due to plate subduction. [2] These earthquakes beneath the Hindu Kush are the result of movement on faults accommodating detachment of the subducted crust. [3] Within the shallow crust, the Chaman Fault represents a major transform fault associated with large shallow earthquakes that forms the transpressional boundary between the Eurasian and Indian Plates. This zone consists of seismically active thrust and strike-slip faults that have accommodated crustal deformation since the beginning of the formation of the Himalayan orogeny. These earthquakes tend to display strike-slip faulting due to its abundance and high deformation rate. [4]
At least 18 people died and 42 others were injured. [5] [6] It was felt in Nangarhar, Kunar, Laghman, Kabul and other nearby provinces. The Ministry of Information and Culture said that at least nine fatalities were reported in the Mazar Dara and Shalat areas of Nurgal District in Kunar province. Three people from the district were also injured. Some of the injured were students of Nangarhar University who attempted to escape their dormitory by leaping out from windows. [6] Over a dozen homes are said to be destroyed, most of which were in the province's Nurgal District. [7] [8] [9] Some were previously damaged by flooding that killed over 600 people. In Laghman, 15 homes were totally or partially destroyed and two people were injured. [6]
A convergent boundary is an area on Earth where two or more lithospheric plates collide. One plate eventually slides beneath the other, a process known as subduction. The subduction zone can be defined by a plane where many earthquakes occur, called the Wadati–Benioff zone. These collisions happen on scales of millions to tens of millions of years and can lead to volcanism, earthquakes, orogenesis, destruction of lithosphere, and deformation. Convergent boundaries occur between oceanic-oceanic lithosphere, oceanic-continental lithosphere, and continental-continental lithosphere. The geologic features related to convergent boundaries vary depending on crust types.
At 20:55 PET on 25 September 2005, an earthquake measuring Mw 7.5 or ML 7.0 struck the Department of Loreto in Peru, resulting in 20 fatalities and 266 injuries, with 1,316 homes damaged or destroyed, mostly in the town of Lamas. It had a maximum perceived intensity of VI (Strong) on the Modified Mercalli Intensity Scale.
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Jalalabad Airport, also known as Nangarhar Airport, and referred to as Jalalabad Airfield (JAF) by the U.S. military during the War in Afghanistan, is located next to the Kabul–Jalalabad Road, about 3 miles (4.8 km) southeast of Jalalabad, which is the capital of Nangarhar Province in Afghanistan. It is a domestic airport under the country's Ministry of Transport and Civil Aviation (MoTCA), and serves the population of not only Nangarhar but also neighboring Kunar, Nuristan and Laghman provinces. It is also used by the Ministry of Defense for military purposes. Security in and around the airport is provided by the Afghan National Security Forces.
The 2002 Hindu Kush earthquakes struck in northern Afghanistan during the month of March. At least 166 people were killed with a very large and intermediate-depth mainshock on March 3. Three weeks later, at least 1,200 were killed during a moderate but shallow event that had a maximum Mercalli intensity of VII. The M7.4 and M6.1 reverse events were focused in the Hindu Kush mountain range area.
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A deep-focus earthquake in seismology is an earthquake with a hypocenter depth exceeding 300 km. They occur almost exclusively at convergent boundaries in association with subducted oceanic lithosphere. They occur along a dipping tabular zone beneath the subduction zone known as the Wadati–Benioff zone.
The 1990 Carlentini earthquake occurred off the Sicilian coast, 20 km east northeast from the town of Augusta, Sicily on 13 December at 01:24 local time. The moderately-sized earthquake measuring 5.6 on the moment magnitude scale (Mw ) resulted in the deaths of 19 people and caused at least 200 injuries. It also inflicted significant damage in the region, leaving 2,500 homeless.
The 1947 Satipo earthquake was the largest earthquake in the sub-Andean region of Peru. It occurred on November 1 at 09:58:57 local time with an epicenter in the Department of Junín. The earthquake had an estimated moment magnitude (Mw ) of 7.7 and focal depth of 20 km (12 mi). Damage was severe in the towns of Satipo and La Merced, and at least 233 people died.
The 2021 Luxian earthquake was a damaging seismic event occurring in the early hours of September 16 at 04:33 China Standard Time. The surface-wave magnitude (Ms ) 6.0 or moment magnitude (Mw ) 5.4 earthquake struck at a shallow depth of 7.5 km and severe shaking in an area of 4,000 square kilometers was assigned a maximum intensity of VIII on the China seismic intensity scale. Three people were killed and 146 injured when the earthquake struck Lu County, Luzhou, Sichuan Province. At least 36,800 buildings were affected, 7,800 of them seriously damaged or completely destroyed, causing about a quarter of a billion dollars worth of damage.
The 1983 Hindu Kush earthquake occurred south of Fayzabad, Badakhshan in northeast Afghanistan at 03:52 PST on December 31, 1983, near the border with Pakistan and the USSR. Striking 214.5 km beneath the Hindu Kush mountains, the moment magnitude 7.4 quake affected three countries, killing at least 26 people and injuring several hundred.
The Lenin Peak disaster occurred on 13 July 1990 when 43 climbers were killed during an avalanche on the 7,134-meter-high mountain peak in northeast Tajikistan and Kyrgyzstan. The deadly avalanche was triggered by a moment magnitude scale 6.4 earthquake which struck at a depth of 216.8 km beneath the Hindu Kush mountains in neighbouring Afghanistan. The incident is believed to be the deadliest mountaineering disaster in history.
The 1959 Coatzacoalcos earthquake occurred at 02:25 local time on August 26 near the Mexican state of Veracruz. The earthquake measured 6.4 Mw at a depth of 21 km (13 mi), and had a maximum Modified Mercalli intensity of VIII (Severe). It had an epicenter immediately off the coast of Coatzacoalcos. The shallow back-arc thrust faulting earthquake damaged the cities of Acayucan, Coatzacoalcos, Jáltipan and Minatitlán. A total of 25 people died, including 10 from Jáltipan while a further 200 were injured. The Middle America Trench, a subduction zone that borders the southwestern coast of Mexico and Central America, accounts for much of the seismicity in Mexico. The eastern side of the country near the Gulf of Mexico rarely experiences large earthquakes although they have been recorded around the Veracruz area, where seismicity is higher compared to other parts of the gulf. Seismicity in the gulf is attributed to back-arc compression due to subduction.
The 1706 Abruzzo earthquake, also known as the Maiella earthquake, occurred on November 3 at 13:00 CEST. The earthquake with a possible epicenter in the Central Apennine Mountains (Maiella), Abruzzo had an estimated moment magnitude of 6.6–6.84 Mw . It was assigned a maximum Mercalli intensity of XI (Extreme), causing tremendous destruction in Valle Peligna. At least 2,400 people were killed.
A 4.0-kilometre (2.5 mi) deep earthquake measuring magnitude (Mw ) 6.2 struck southeastern Afghanistan on 22 June 2022 at 01:24:36 AFT. The earthquake had a maximum Modified Mercalli intensity of IX (Violent). There were 1,052–1,163 deaths and 1,627–2,976 injured in Afghanistan and Pakistan. The worst affected provinces in Afghanistan were Paktika, Paktia, Khost and Nangarhar. Casualties and damage also occurred in Pakistan's Khyber Pakhtunkhwa. At least 10,000 homes collapsed or were severely damaged. The earthquake's shallow hypocenter, proximity to populated areas and low building quality contributed to its destructive effects. Shaking was felt over 500 km (310 mi) away by at least 119 million people, including Pakistan's Punjab and parts of India and Iran.
The 1977 Bob–Tangol earthquake struck Kerman province of Iran on December 20, 1977, at 03:04 Iran Standard Time. The earthquake measured Mw 5.9 and struck at a depth of 22.7 km (14.1 mi). A maximum Modified Mercalli intensity of VII was evaluated based on damage. It had a strike-slip focal mechanism, which was unusual as the source structure was a thrust fault. It was part of a sequence of strong earthquakes along the 400 km (250 mi) Kuh Banan Fault. Between 584 and 665 people perished while a further 500–1,000 were injured; thousands were also made homeless. Casualties from the earthquake was considered moderate due to the sparsely populated area it affected. Preceded by foreshocks the month before, many residents became wary of a larger earthquake and took refuge outside their homes, contributing to the moderate death toll. However, there were none immediately before the mainshock so many were still in their homes when it struck. Aftershocks were felt for several months, some causing additional damage.
The 1957 Alborz earthquake struck northern Iran's Mazandaran province at 04:12 local time on 2 July. It had a moment magnitude (Mw ) of 7.1 and occurred at a focal depth of 15 km (9.3 mi). The thrust-faulting shock was assigned a maximum Modified Mercalli intensity of IX (Violent). It devastated 120 villages in the Alborz Mountains and caused an estimated 1,500 fatalities. The earthquake also triggered landslides including one that dammed the Haraz River. Some damage was also reported in Tehran, Qaem Shahr and Sari.
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