2002 Hindu Kush earthquakes

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2002 Hindu Kush earthquakes
HinduKushEQs.JPG
Afghanistan physical map.svg
Bullseye1.png
UTC  time2002-03-03 12:08:19
 2002-03-25 14:56:33
ISC  event 5267309
  2947182
USGS-ANSS  
  ComCat
  ComCat
Local date 
 March 3, 2002 (2002-03-03)
 March 25, 2002 (2002-03-25)
Local time16:38
 19:26
Magnitude7.4 Mw
 6.1 Mw
DepthMarch 3 – 226 km (140 mi)
8 km (5 mi)
Epicenter 36°30′N70°29′E / 36.5°N 70.48°E / 36.5; 70.48 Coordinates: 36°30′N70°29′E / 36.5°N 70.48°E / 36.5; 70.48
Type Dip-slip
Max. intensityMarch 3 - VI (Strong) [1]
March 25 - VII (Very strong) [2]
Casualties
  • 166 dead, some injured (March 3 event) [3]
  • 1,200 dead (March 25 event)

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 (Very strong). The M7.4 and M6.1 reverse events were focused in the Hindu Kush mountain range area. [1] [2]

Contents

Tectonic setting

Northern Afghanistan lies within the broad zone of continuing collision between the Indian Plate and the Eurasian Plate. The area is seismically active, particularly as a result of faulting at just over 200 km depth within the descending slab. Many large events of M ≥ 7 have been observed in the Hindu Kush, all with similar epicenters, with an approximate periodicity of about 10–15 years. These events have reverse fault focal mechanisms, which for the near-vertical slab indicates active extension. It has been proposed that these earthquakes are a result of "necking" of the downgoing slab, a process that may eventually lead to break-off. [4]

Smaller shallow focus earthquakes are also observed in the region, particularly associated with north–south trending zones of right lateral strike-slip, such as the Chaman Fault, with an increasing degree of shortening to the north, together accommodating the highly oblique convergence between the Indian Plate and the Eurasian Plate. [5]

Earthquakes

The earthquake on March 3 had a magnitude of 7.4 Mw, with a hypocentral depth of 225.6 km. The focal mechanism is consistent with reverse faulting within subducting oceanic crust. Comparison with similar earthquakes in 1993 and 2015, which have very similar depths and epicenters, suggests that the major component of the slip in all three events occurred on the same part of the fault. [4]

The earthquake on March 25 had a magnitude of 6.1 Mw, with a hypocentral depth of 8.0 km. It had a reverse fault mechanism that occurred on one of two possible moderately-dipping north–south trending faults.

Damage

March 3 event

At 12:08:19 UTC a 7.4 tremor hit an area 65 km (40 mi) S of Feyzabad, Afghanistan. At least 150 people were killed, several injured and 400 houses damaged or destroyed by a landslide that dammed and flooded Surkundara Valley, Samangan Province. At least 13 people were killed at Kabul and Rostaq and 3 people killed in Bajaur, Pakistan. At least 300 houses were destroyed in Badakhshan and Takhar Provinces. A 45 meter wide fissure opened in Xiker Reservoir in Xinjiang, China. This was a deep focus event and was felt in much of Afghanistan and Pakistan. Felt also in Tajikistan, Uzbekistan, Kyrgyzstan, Kazakhstan and India. [1]

March 25 event

At 14:56:33 UTC, a magnitude 6.1 tremor hit an area 160 km (99 mi) southwest of Feyzabad, Afghanistan. The United Nations estimated approximately 1,200 people dead and 20,000 families affected. This was a shallow focus event and was felt strongly in much of northern Afghanistan. Also felt in the Islamabad-Peshawar area, Pakistan and at Dushanbe, Tajikistan. [2] In Nahrin, many homes collapsed; the maximum Modified Mercalli intensity was assigned VII (Very strong). The high death toll and heavy damage was attributed to poor construction—most homes were constructed of mud brick. [6]

See also

Related Research Articles

Megathrust earthquakes occur at convergent plate boundaries, where one tectonic plate is forced underneath another. The earthquakes are caused by slip along the thrust fault that forms the contact between the two plates. These interplate earthquakes are the planet's most powerful, with moment magnitudes (Mw) that can exceed 9.0. Since 1900, all earthquakes of magnitude 9.0 or greater have been megathrust earthquakes.

The 2003 Colima earthquake occurred on 21 January with a moment magnitude of 7.6 and a maximum Mercalli intensity of VIII (Severe). The epicenter was located on the Pacific coast in the Mexican state of Colima. The earthquake was felt as far away as Mexico City and in southern parts of the United States.

The February 1998 Afghanistan earthquake occurred at 19:03 local time near the Afghanistan-Tajikistan border. The strike-slip shock had a moment magnitude of 5.9 and a maximum Mercalli intensity of VII. With several thousand dead and hundreds injured, the event's effects were considered extreme by the National Geophysical Data Center. It was felt at Tashkent and Dushanbe, and aftershocks continued for the next seven days.

The 1989 Malawi earthquake occurred on 10 March in central Malawi, with a moment magnitude of 6.3 and a maximum Mercalli intensity of VIII (Severe). It was preceded by a number of foreshocks, the largest being a 5.7 Mw shock on the previous day. The earthquake was felt strongly throughout central Malawi, and also felt in parts of Mozambique and Zambia. Nine people were killed, with many others injured or left homeless.

The 2005 Tarapacá earthquake occurred on June 13 at 22:44:33 UTC. Its epicenter was located near Mamiña, in northern Chile about 125 km east-northeast of Iquique, affecting the Tarapacá Region and adjacent parts of Bolivia. It had a magnitude of Mw 7.8 and a maximum felt intensity of VII on the Mercalli intensity scale.

<span class="mw-page-title-main">Lists of 21st-century earthquakes</span>

The following is a summary of significant earthquakes during the 21st century. In terms of fatalities, the 2004 Indian Ocean earthquake was the most destructive event with around 227,898 fatalities, followed by the 2010 Haiti earthquake with about 160,000 fatalities, the 2008 Sichuan earthquake with 87,587 fatalities, the 2005 Kashmir earthquake with 87,351 fatalities, and the 2023 Turkey–Syria earthquake with at least 55,190 fatalities.

A 6.2 magnitude earthquake occurred in Afghanistan on October 22, 2009 at 19:51:27 UTC. The maximum Mercalli intensity was V (Moderate) at Fayzabad, Badakhshan.

The 1881 Nicobar Islands earthquake occurred at about 07:49 local time on 31 December, with an epicentre beneath Car Nicobar. It occurred as two separate ruptures, the largest of which had an estimated magnitude of 7.9 on the moment magnitude scale and triggered a tsunami that was observed around the Bay of Bengal. It is probably the earliest earthquake for which rupture parameters have been estimated instrumentally.

The 1931 Oaxaca earthquake affected portions of southern Mexico on January 14 at 18:50 MST. It registered a magnitude of 8.0 on the surface wave magnitude scale and had a maximum perceived intensity of X (Extreme) on the Mercalli intensity scale.

<span class="mw-page-title-main">1819 Rann of Kutch earthquake</span> Earthquake and tsunami in Gujarat, India

The 1819 Rann of Kutch earthquake occurred at about 18:45 to 18:50 local time on 16 June. It had an estimated magnitude ranging from 7.7 to 8.2 on the moment magnitude scale and a maximum perceived intensity of XI (Extreme) on the Mercalli intensity scale. It triggered a tsunami and caused at least 1,543 deaths. The earthquake caused an area of subsidence that formed the Sindri Lake and a local zone of uplift to the north about 80 km long, 6 km wide and 6 m high that dammed the Koree / Kori / Puran / Nara river. This natural dam was known as the Allah Bund.

<span class="mw-page-title-main">2012 Afghanistan earthquakes</span> Earthquakes in Afghanistan in 2012

On 11 June 2012, two moderate earthquakes struck northern Afghanistan, causing a large landslide. The landslide buried the town of Sayi Hazara, trapping 71 people. After four days of digging, only five bodies were recovered and the search was called off. Overall, 75 people were killed and 13 others were injured.

<span class="mw-page-title-main">October 2015 Hindu Kush earthquake</span> Earthquake in Pakistan, Afghanistan and India

The October 2015 Hindu Kush earthquake was a magnitude 7.5 earthquake that struck South Asia on 26 October 2015, at 13:39 AFT with the epicenter 45 km north of Kuran wa Munjan, Afghanistan, at a depth of 212.5 km.

The 1946 Ancash earthquake in the Andes Mountains of central Peru occurred on November 10 at 17:43 UTC. The earthquake had a surface-wave magnitude of 7.0, and achieved a maximum Mercalli intensity scale rating of XI (Extreme). About 1,400 Peruvians are thought to have died from the event.

On January 30, 1973, at 15:01 (UTC–6), a magnitude 7.6 earthquake struck 35.3 km (21.9 mi) beneath the Sierra Madre del Sur range in the Mexican states of Colima, Jalisco and Michoacán. On the Mercalli intensity scale, the earthquake reached a maximum intensity of X (Extreme), causing serious damage in the region. At least 56 people were killed and about 390 were injured. The event is commonly referred to as the Colima earthquake.

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.

<span class="mw-page-title-main">Lenin Peak disaster</span> 1990 earthquake and subsequent avalanche in Tajikistan

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 1909 Benavente earthquake occurred on April 23 at 17:39:36 local in the Santarém District of the Central Region, Portugal. The earthquake had an estimated moment magnitude of 6.0 and a maximum intensity assigned at X (Extreme) on the Mercalli scale. It nearly destroyed the town of Benavente, killing 60 and injuring 75 people as a result.

The 1991 Hindu Kush earthquake occurred northeast of Kabul, Afghanistan on February 1, 1991. It was an intermediate-depth earthquake with a hypocenter 142.4 km beneath the Hindu Kush mountains. It measured 6.9 on the moment magnitude scale, and affected neighbouring Pakistan and the USSR. At least 848 people were killed in both countries and damage was estimated at $26 million USD.

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.

On 21 March 2023, a magnitude 6.5 earthquake struck Badakhshan Province, Afghanistan, with an intermediate depth of approximately 187 km (116 mi). The epicenter of the earthquake was 40 km (25 mi) south-southeast of Jurm.

References

  1. 1 2 3 USGS. "M7.4 - Hindu Kush region, Afghanistan". United States Geological Survey.
  2. 1 2 3 USGS. "M6.1 - Hindu Kush region, Afghanistan". United States Geological Survey.
  3. National Geophysical Data Center / World Data Service (NGDC/WDS) (1972), Significant Earthquake Database (Data Set), National Geophysical Data Center, NOAA, doi:10.7289/V5TD9V7K
  4. 1 2 Zhan, Z.; Kanamori, H. (2016). "Recurring large deep earthquakes in Hindu Kush driven by a sinking slab". Geophysical Research Letters. 43 (14): 7433–7441. Bibcode:2016GeoRL..43.7433Z. doi:10.1002/2016GL069603. S2CID   31948667.
  5. Ambraseys, N.N.; Bilham, R. (2003). "Earthquakes in Afghanistan". Seismological Research Letters. 74 (2): 107–123. doi:10.1785/gssrl.74.2.107. S2CID   130945532.
  6. Yeats, Robert S.; Madden, Christopher (2003). "Damage from the Nahrin, Afghanistan, Earthquake of 25 March 2002". Seismological Research Letters. 74 (3): 305–311. doi:10.1785/gssrl.74.3.305.

Sources