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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 kilometres (93 mi) to the west via the Jamuna River.
|Local date||2 April 1762|
|Max. intensity||XI (Extreme)|
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. The presence of active subduction along the eastern margin of the Bay of Bengal is disputed.
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. 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.
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. The Saint Martin’s Island has been uplifted by 2- 2.5 m during that earthquake. A repeat period of about 500 – 700 years has been suggested for earthquakes similar to that in 1762.
A tsunami was reported along the northeastern coast of the Bay of Bengal and at Dhaka and Kolkata. This is regarded as a local tsunami, as no effects were recorded on the western side of the bay.
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. 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.
- ^ a b c Mondal, Dhiman R.; McHugh, Cecilia M.; Mortlock, Richard A.; Steckler, Michael S.; Mustaque, Sharif; Akhter, Syed Humayun (October 2018). “Microatolls document the 1762 and prior earthquakes along the southeast coast of Bangladesh”. Tectonophysics. 745: 196–213. Bibcode:2018Tectp.745..196M. doi:10.1016/j.tecto.2018.07.020.
- ^ “Flooding concerns return to northeastern India”. Al Jazeera.
- ^ 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. 266 (1–4): 143–155. Bibcode:2009MGeol.266..143M. doi:10.1016/j.margeo.2009.07.015.
- ^ a b c Kundu, B.; Gahalaut V.K. (2012). “Earthquake occurrence processes in the Indo-Burmese wedge and Sagaing fault region”. Tectonophysics. 524–525: 135–146. Bibcode:2012Tectp.524..135K. doi:10.1016/j.tecto.2011.12.031.
- ^ 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.
- ^ National Geophysical Data Center / World Data Service: NCEI/WDS Global Historical Tsunami Database. NOAA National Centers for Environmental Information. “Tsunami Event Information”. doi:10.7289/V5PN93H7. Retrieved 15 April 2022.
- ^ 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.
- ^ National Geophysical Data Center / World Data Service (NGDC/WDS): NCEI/WDS Global Significant Earthquake Database. NOAA National Centers for Environmental Information. “Significant Earthquake Information”. doi:10.7289/V5TD9V7K. Retrieved 15 April 2022.
End Notes and External links
- source: “1762 Arakan earthquake” | Wikipedia
- Last updated on 20th April 2022
ပုံ၇။ ၁၇၆၂ခုနှစ် စစ်တကောင်းဗဟိုပြုမြေငလျင်ဖြစ်ပေါ်နေပုံ (Epocenter=အနီရောင်အဝိုင်း) (ဘယ်) နှင့် ၁၇၆၂ခုနှစ် ငလျင်ကြောင့်ဘင်္ဂလားပင်လယ်နှင့် ရခိုင်ကမ်းခြေတွင်စူနားမီဖြစ်နေပုံ (အနီရောင်) (ကျမ်းကိုး Cummins, P.R 2007 The Potential for giant Tsunamigenic Earthquakes in the northern Bay of Bengal: Nature v.449) (ညာ)။
source: “ရခိုင်ကမ်းရိုးတန်းကိုလေ့လာခြင်း Study of Arakan Coast | အပိုင်း (၈)“
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