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The 1762 Arakan earthquake occurred at about 17:00 local time on 2 April, with an epicentre somewhere on the coast from Chittagong (modern Bangladesh) to Arakan in modern Burma. It had an estimated magnitude of as high as 8.8 on the moment magnitude scale and a maximum estimated intensity of XI (Extreme) on the Mercalli intensity scale. It triggered a local tsunami in the Bay of Bengal and caused at least 200 deaths. The earthquake was associated with major areas of both uplift and subsidence. It is also associated with a change in course of the Brahmaputra River to from east of Dhaka (Old Brahmaputra River) to 150 km to the west via the Jamuna River.[1]

1762 Arakan earthquake
1762 Arakan earthquake is located in Bangladesh
1762 Arakan earthquake
Date 2 April 1762 (1762-04-02)
Magnitude ≤8.8 Mw
Epicenter 22°00′N 92°00′E / 22.0°N 92.0°E / 22.0; 92.0Coordinates: 22°00′N 92°00′E / 22.0°N 92.0°E / 22.0; 92.0
Areas affected Bangladesh
Max. intensity XI (Extreme)
Tsunami Yes
Casualties 200+

Contents

Tectonic settingEdit

The eastern part of Bangladesh and the southwestern part of Burma lie along the highly oblique convergent boundary between the Indian Plate and the Eurasian Plate. The degree to which this deformation is partitioned into zones of thrust tectonics (accommodating that part of the motion perpendicular to the boundary) and strike-slip tectonics (accommodating the northward movement of the Indian Plate) varies along the boundary. A pure strike-slip boundary that strike parallel to the plate vector runs along the Western Burma Scarp, that is replaced to the north by the Indo-Burmese Wedge fold and thrust belt, at the western edge of the boundary zone, and a series of major dextral (right lateral) strike-slip faults, particularly the Kabaw Fault and Sagaing Fault further to the east.[2] The presence of active subduction along the eastern margin of the Bay of Bengal is disputed.[2][3]

EarthquakeEdit

The earthquake lasted for about four minutes at Chittagong. The epicentre is not well-constrained and likely locations have varied from near Chittagong to along the Arakan coast. The extent of the rupture is uncertain but may have been as much as 700 km along the plate interface. This is based both on the extent of uplift, which was recorded along the coast of Burma from Foul Island to Ramree Island, and the area of subsidence around Chittagong, further north. The 700 km extent combined with an estimated displacement of ten metres gives a maximum estimated magnitude of 8.8 on the moment magnitude scale.[4] Other workers have pointed out that neither the subsidence, which could be due to lateral spreading, nor the uplift, which is not unequivocally linked to the 1762 earthquake, necessarily provide a reasonable estimate for the size of this event and prefer to regard this as a magnitude 7–8 earthquake.[3]

Studies of uplifted marine terraces along the Burmese coast have found evidence for three uplifts, the most recent of which is interpreted to be from the 1762 earthquake. A repeat period of about 900 years has been suggested for earthquakes similar to that in 1762.

TsunamiEdit

A tsunami was reported along the northeastern coast of the Bay of Bengal and at Dhaka and Kolkata.[5] This is regarded as a local tsunami, as no effects were recorded on the western side of the bay.[3]

DamageEdit

In Chittagong it was reported that no buildings or walls built of brick had escaped either destruction or serious damage. The East India Company's factory inside the fort was so badly damaged that it could no longer be safely used.[6] An area of about 60 square miles (160 km2) permanently subsided beneath the sea along the coast near Chittagong. At Bar Chara, just north of Cox's Bazar, the land sank and 200 people were killed. Chittagong was said to have "suffered severely" with soil liquefaction effects such as sand volcanoes and ground fissures.[7]

See alsoEdit

ReferencesEdit

  1. ^ "Flooding concerns return to northeastern India". www.aljazeera.com. 
  2. ^ a b Maurin, T.; Rangin C. (2009). "Impact of the 90°E ridge at the Indo-Burmese subduction zone imaged from deep seismic reflection data". Marine Geology. Elsevier. 266 (1–4): 143–155. Bibcode:2009MGeol.266..143M. doi:10.1016/j.margeo.2009.07.015. Retrieved 22 March 2012. 
  3. ^ a b c Kundu, B.; Gahalaut V.K. (2012). "Earthquake occurrence processes in the Indo-Burmese wedge and Sagaing fault region". Tectonophysics. Elsevier. 524–525: 135–146. Bibcode:2012Tectp.524..135K. doi:10.1016/j.tecto.2011.12.031. Retrieved 22 March 2012. 
  4. ^ Cummins, P.R. (2007). "The potential for giant tsunamigenic earthquakes in the northern Bay of Bengal". Nature. 449 (7158): 75–78. Bibcode:2007Natur.449...75C. doi:10.1038/nature06088. PMID 17805292. 
  5. ^ NGDC. "Comments for the Tsunami Event". Retrieved 22 March 2012. 
  6. ^ Verelst (1764). "An Account of the Earthquakes that have been felt in the Province of Islamabad, with the Damages attending them, from the 2d to the 19th of April, 1762". Philosophical Transactions of the Royal Society. 53: 265–269. doi:10.1098/rstl.1763.0043. Retrieved 27 March 2012. 
  7. ^ NGDC. "Comments for the significant earthquake". Retrieved 22 March 2012.