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[๐Ÿ‡ง๐Ÿ‡ฉ] Earthquake in Myanmar----Lessons for Bangladesh

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[๐Ÿ‡ง๐Ÿ‡ฉ] Earthquake in Myanmar----Lessons for Bangladesh
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Dhaka jolted by early morning earthquake

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An earthquake shook Dhaka and surrounding areas at 6.15am this morning.

According to Indian Center for Seismology, the tremor had a 4.1 magnitude on Richter Scale. The epicenter of the quake was Narsingdi. USGS was yet to report on it.

Bangladesh faces a high risk of major earthquakes due to its location along three active tectonic plate faults, experts warned recently following major tremors, stressing that preparedness, public awareness and modern technology are crucial to reducing casualties and damage.​
 
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Bangladesh shaken again as 5.9 magnitude quake hits near Myanmar border

bdnews24.com
Published :
Feb 03, 2026 22:45
Updated :
Feb 03, 2026 22:45

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Bangladesh has experienced its second earthquake in a single day, this time originating near the Myanmar border.

According to GFZ Earthquake Explorer, the tremor struck at 9:34pm Bangladesh time with a magnitude of 5.9 on the Richter scale.

No immediate reports of casualties or damage have emerged.

This follows an earlier tremor in the day.​
 
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Magnitude 5.1 earthquake in Myanmar shakes Bangladesh

bdnews24.com
Published :
Feb 26, 2026 00:20
Updated :
Feb 26, 2026 00:20

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A magnitude 5.1 earthquake in Myanmar have shaken Dhaka and several other parts of Bangladesh.

The tremor struck at 10:51pm on Wednesday, according to the Bangladesh Meteorological Departmentโ€™s earthquake monitoring centre.

Assistant Meteorologist Farzana Sultana said the epicentre was in Myanmar, 462 kilometres from the Agargaon Met Office in Dhaka.

The US Geological Survey (USGS) also recorded the quake at magnitude 5.1, with its origin 129 kilometres below the surface.

No immediate reports of damage or casualties were available.​
 
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Earthquake: Satkhira resident says building โ€˜swayed like a tree branchโ€™

Staff Correspondent
Dhaka
Published: 27 Feb 2026, 16: 43

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Bangladesh Meteorological Department (BMD) reported Asshashuni Upazila of Satkhira to be the epicentre. USGS

Mrityunjoy Roy, a resident of Satkhira Sadar upazila, has described his frightening experience during the earthquake that was felt in different parts of the country including Dhaka at 1:52:29 pm today, Friday.

According to the Bangladesh Meteorological Department (BMD), the epicentre of the earthquake was in Ashashuni Upazila of Satkhira. The earthquake measured 5.4 on the Richter scale and was of moderate intensity.

Speaking to Prothom Alo over the phone, Mrityunjoy Roy, who is a journalist by profession, said he was lying on his bed when the quake struck. Suddenly, he felt the entire bed shaking.

โ€œI wondered what was happening. Then I rushed outside shouting,โ€ he said.

Mrityunjoy added that it felt as though the five-storey building was swaying from side to side. The strong tremor made it seem as if the building was moving the way tree branches sway back and forth during a storm.

According to a report by media outlet Anandabazar Online, tremors were also felt in Kolkata and other districts of West Bengal in India, where the magnitude was recorded at 5 on the Richter scale.​
 
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Earthquake contingency plans must be foolproof

RECURRING earthquakes of varying magnitudes require the government to revisit its preparedness and mitigation plans. A 5.4-magnitude earthquake, originating in Satkhira, was felt on February 27. With the latest event, there were nine earthquakes in February, two of which had the epicentre in Satkhira. The Department of Meteorology says that 32 earthquakes have occurred in the country and in neighbouring areas since mid-February 2025. In November 2025, at least 10 people, including two children, died and several hundred became injured after a 5.7-magnitude earthquake struck Dhaka and surrounding districts. The worrying issue is that the frequency of earthquakes has recently increased. Earthquakes have, in particular, risen in Bangladeshโ€™s south-west, traditionally considered a low-risk area. Experts have differing views on the cause of the earthquake. While some believe that the earthquake in Satkhira was an aftershock of the Narsingdi earthquake, others think that it resulted from the south-west, being subjected to opposing tensile forces between the two tectonic plates at the eastern and western edges of Bangladesh. At this time of heightened risk, the government should urgently focus on strengthening earthquake resilience.

Bangladesh, with major seismic activities in the region, is considered an earthquake-prone region because of its location at the junction of the Indian, Eurasian and Burmese plates. An earlier survey of Rajdhani Unnayan Kartripakkha estimated that around 865,000 buildings could collapse in an earthquake of a magnitude of 6.9 originating in the fault line in Tangail. In March 2025, the Fire Service and Civil Defence issued an official alert identifying Dhaka, Chattogram, Mymensingh and Sylhet as high-risk regions and urged all concerned to take a nine-point measure that included constructing earthquake-resistant buildings, strengthening vulnerable buildings, ensuring proper maintenance of gas, water and electric lines and improving public awareness and skills in earthquake prevention and response. Bangladesh has an earthquake contingency plan, but its implementation is uncertain. The awareness programmes are irregular. Efforts to reduce long-term risks through measures such as strengthening building codes and improving land-use planning barely exist. The governmentโ€™s plan also appears ineffective given the way it has responded to recent injuries and fatalities from the earthquake, especially the one in Narsingdi.

It is almost impossible to predict when a major earthquake will occur. This means that the government must have a system that is ready to respond any time. The primary emphasis should be given to extensive awareness and practical training. This includes regular drills in all public and private establishments, retrofitting risky buildings, enforcing earthquake safety technologies in new buildings and implementing the governmentโ€™s guidelines on how to deal with the aftermath of an earthquake. The government must build capacity for prompt response, rescue and evacuation operations and treatment facilities in hospitals.​
 
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32 earthquakes in 13 months in country, origins in low-risk regions too

Partha Shankar Saha & Mostafa Yusuf
Dhaka
Published: 28 Feb 2026, 08: 11

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Roof tiles of a mud house collapse at Uttarpara village in Tala upazila of Satkhira after an earthquake jolted the country on 27 February 2026. Prothom Alo

Bangladesh is located at the junction of three earthquake-prone tectonic plates. So experts consider it natural that earthquakes will occur from time to time in the country. However, the worrying matter is that recently the tendency of earthquakes originating within the country has increased. In particular, earthquakes have increased in the countryโ€™s south-western region, which is known as a low-risk zone for earthquakes.

Experts think that this south-western region has come under tensional forces (opposing pulls) between two plates located on the countryโ€™s eastern and western edges. As a result, earthquake proneness in this region may have increased. They also think that a new fault may have formed in the south-western region, or an old fault may have become active again.

Experts believe that these earthquakes in the south-western region are not frightening. However, in their opinion, the increase in the number of earthquakes inside the country and in surrounding areas indicates a large earthquake. And proper preparation is needed to face such an earthquake. According to them the country lacks this considerably.

Yesterday, Friday afternoon, an earthquake shook various regions of the country including Dhaka. After that, the fear of earthquakes and ways to deal with them came up again for discussion. Yesterdayโ€™s earthquake originated in Ashashuni upazila of Satkhira. Its magnitude at the epicentre was 5.4 on the Richter scale, which is called a moderate earthquake.

Earthquake felt across Bangladesh, magnitude 5.4, epicentre in Satkhira

Although tremors were felt in different parts of the country including the capital, naturally they were felt much more strongly at the epicentre in Satkhira. There, people came out on the streets leaving their houses and shops in panic. Many of them said they felt a strong jolt. The earthquake, which lasted a few seconds at 1:52 pm, spread panic in the district.

Abdul Ali, a resident of Ashashuni Sadar, told Prothom Alo, โ€œSuddenly my two-storey house started shaking. Everyone in the family quickly came down.โ€ Purbopod Mallik, a resident of Harinagar village adjacent to the Sundarbans, said that suddenly around noon his two-storey house shook in the earthquake.

Why are earthquakes increasing in the southwest

Considering earthquake risk, the country has been divided into highly risky, moderately risky, and low-risk areas. Among these, the area from Lalmonirhat district in the north to Khagrachhari in the south-east is highly risky; the north-central region including Dhaka is moderately risky; and the southern and south-western regions of Barishal and Khulna divisions are considered low-risk areas.

In this low-risk area, a moderate earthquake originated yesterday in Satkhira. But not only yesterdayโ€”on Thursday a 3.2-magnitude earthquake originated in Kaliganj of Jhenaidah in the southwest. Also, on 3 February early morning, an earthquake originated in Kalaroa of Satkhira with a magnitude of 4.1. On 27 September last year, an earthquake of magnitude 3.5 occurred in Monirampur of Jashore.

The three earthquake-prone regions among which Bangladesh is located are the subduction zone in the east, the Dauki Fault in the north, and the Himalayan Frontal Thrust zone at the foothills of the Himalayas (stretching from Nepal to Arunachal).

Small earthquakes donโ€™t reduce risk of a major earthquake

Earthquake expert and former professor of the Geology Department at University of Dhaka, Humayun Akhter, told Prothom Alo that the Indian Plate is going under the Burma Plate to the east, which is called subduction. At the eastern edge the plate is sinking downward. But to the west, a large part of the same plate is relatively stable and resisting the pull toward the east.

Humayun Akhter compared this situation to stretching a rubber band. He said, when pulled from two sides, pressure and tension are created in the middle. If the tension exceeds the limit of elasticity, the rubber band snaps. Similarly, tension accumulating in the middle of a plate can reactivate an old fault at a weak point or create a new fracture. Then the accumulated energy is suddenly releasedโ€”that is an earthquake.

He thinks that in this Satkhira incident an old fault may have been reactivated or a new fault may have formed. He believes that if focal mechanism analysis (which indicates the type of displacement of rocks along a fault or fracture of a plate) is obtained in the future, it will be understood whether it is a normal fault or a newly activated one.

However, Humayun Akhter reassured that there is no major active tectonic plate boundary in that area. So moderate earthquakes may occur there, but the risk of a very large earthquake is low.

Akhtarul Ahsan, deputy director of the Geological Survey Department who is doing a PhD on earthquakes at Auburn University in the United States, thinks the Satkhira earthquake was an aftershock of the 5.7-magnitude earthquake on 21 November last year.

Earthquake: Another active fault line discovered in Bangladesh
Akhtarul Ahsan told Prothom Alo that the origin of the Satkhira earthquake was from a newly discovered 400-kilometre-long fault line extending from Kolkata to Jamalpur to Mymensingh. The Satkhira and Narsingdi regions fall within the hinge line (30-kilometre areas on both sides of the fault line) of this fault.

In Akhtarul Ahsanโ€™s research, a new 400-kilometre-long fault line has recently been found from Kolkata through Jamalpur in Bangladesh to Mymensingh.

Earthquake origins increasing inside the country

Data on earthquakes from 2016 to now have been obtained from the earthquake observation centre of the Bangladesh Meteorological Department (BMD). It shows that from mid-February 2025 to yesterday, 32 earthquakes originated inside the country and in border-adjacent areas. Among these, the highest numberโ€”10 earthquakesโ€”originated in the greater Sylhet area. These earthquakes originated near the Dauki Fault.

Rubaiyat Kabir, officer-in-charge of the earthquake observation centre of the BMD, told Prothom Alo yesterday that since 2016 there has been no record of 32 earthquakes originating inside the country in just 13 months. The increase of earthquakes inside the country and in border areas is the manifestation of the huge amount of energy accumulated beneath the earth. It indicates a large earthquake, which has been said for a long time.

Although agreeing about the possibility of a big earthquake, professor Humayun Akhter has a different explanation regarding the increase of earthquakes in and around the country.

He said, โ€œCompared to before, the effort to collect earthquake data in our country and neighbouring areas has increased. Earlier those were not there. Technology has also improved. So perhaps now we are getting more and more accurate earthquake-related information.โ€​
 
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Preparedness reduces earthquake losses

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WHEN the earth shakes, it does not ask whether a city is ready. It exposes the truth in seconds. Prime minister Tarique Rahmanโ€™s recent directive to prepare one hundred thousand volunteers in Dhaka for post-earthquake response is, at first glance, an administrative instruction. Look closer and it is something more serious: an acknowledgment that Bangladeshโ€™s seismic risk is no longer theoretical. It is immediate, measurable and unforgiving.

The decision follows a series of tremors felt across the country. These were not catastrophic, but they were clarifying. They reminded us of a scientific reality long articulated by geologists and engineers โ€” Bangladesh sits perilously close to active fault lines. Dhaka, Chattogram and Sylhet lie in zones where tectonic pressures accumulate quietly over decades before releasing energy violently within seconds.

The difference between tragedy and resilience will not be decided in those seconds. It will be decided in the years before them.

Geography we cannot change

BANGLADESH occupies one of the most seismically sensitive regions in the world. It lies at the junction of the Indian, Eurasian and Burmese tectonic plates. This geological reality is not political, not negotiable, and not partisan. It is physics.

Research conducted by engineers at the Bangladesh University of Engineering and Technology has repeatedly warned that a major earthquake โ€” magnitude 7 or above โ€” could cause widespread structural collapse in Dhaka. Thousands of buildings were constructed before modern building codes were introduced. Many more were erected without strict adherence to design standards. In a densely populated metropolis of more than 20 million people, vulnerability scales quickly.

Urbanisation in Dhaka has been rapid, vertical and often poorly regulated. Narrow roads would complicate rescue operations. Informal settlements lack structural reinforcement. Hospitals are already operating near capacity. These are not criticisms; they are facts.

The Comprehensive Disaster Management Programme has previously identified urban infrastructure fragility and limited rescue capability as systemic risks. In other words, the threat is documented. The question is whether preparation will be institutionalised.

The first 72 hours

DISASTER experts around the world emphasise a sobering truth: the first 72 hours after a major earthquake are decisive. Survival rates drop sharply after that window. Countries that have reduced earthquake fatalities did not do so through luck. They did so through planning.

Consider Japan. After the 1995 Kobe earthquake killed over 6,000 people, Japan reformed its building codes, strengthened urban search-and-rescue units and institutionalised public drills. When the 2011 Tลhoku earthquake struck โ€” magnitude 9.0, far stronger โ€” the death toll, while tragic, was dramatically mitigated by structural resilience and public preparedness.

Chile offers another example. Following devastating quakes in the 20th century, it implemented some of the strictest seismic construction standards in the world. When an 8.8 magnitude earthquake hit in 2010, building collapses were far fewer than in comparable disasters elsewhere.

Contrast this with Haiti in 2010. A magnitude 7.0 earthquake โ€” moderate by global standards โ€” killed over 200,000 people. The difference was not geology. It was infrastructure and preparedness.

Bangladeshโ€™s challenge is closer to Haitiโ€™s vulnerability than Japanโ€™s readiness. That is precisely why awareness and enforcement matter.

Volunteers: necessary but not sufficient

THE plan to mobilise one hundred thousand volunteers in Dhaka mirrors the successful cyclone preparedness programmes in coastal regions. Bangladeshโ€™s achievements in cyclone management are globally recognised. In 1970, Cyclone Bhola killed hundreds of thousands. By the time Cyclone Amphan struck in 2020, early warning systems, community volunteers and evacuation shelters dramatically reduced fatalities.

That transformation did not occur overnight. It was built on sustained awareness campaigns, local engagement and institutional discipline.

An earthquake response network in Dhaka could replicate that success โ€” but only if it extends beyond symbolic numbers. Volunteers must be trained in light search and rescue, basic first aid, evacuation coordination and communication protocols. They must know which schools and open fields are designated safe assembly areas. They must understand chain-of-command structures to prevent chaos. Preparedness is not a slogan. It is muscle memory.

Enforcement is prevention

YET response planning addresses only half the problem. The more difficult half is prevention. Strict enforcement of the Bangladesh National Building Code is indispensable. Risky structures must be identified. Retrofitting programmes, though costly, are far cheaper than post-collapse reconstruction and mass casualties. Public disclosure of high-risk buildings would create accountability. Insurance frameworks could incentivise compliance.

Data-driven governance is essential. Structural audits of bridges, flyovers and critical installations should be routine. Utility providers must ensure that gas lines and electrical systems have automatic shutoff mechanisms to prevent post-quake fires โ€” often deadlier than the tremors themselves.

Hospitals require surge-capacity planning. Trauma care units, blood banks, temporary field hospitals and mobile medical teams must be integrated into a unified emergency plan. Earthquakes do not respect administrative boundaries; inter-agency coordination must be rehearsed before disaster strikes.

Culture of awareness

HERE lies the most underestimated variable: public behaviour. In many earthquake-prone countries, schoolchildren practice โ€˜Drop, Cover and Hold Onโ€™ drills from an early age. Families maintain emergency kits. Media outlets broadcast preparedness guidelines regularly, not only after tremors but year-round.

In Bangladesh, awareness often spikes after an earthquake and fades as memory does. That cycle must end. During an earthquake, it is essential to prioritise personal safety by knowing what to do during the shaking, such as dropping, covering and holding on. Once the shaking stops, safely turning off gas and electricity can prevent fires and other hazards. Families and communities should establish a designated assembly point for after evacuation to ensure everyone is accounted for. It is also important to assist neighbours when possible, without putting oneself in danger. Finally, staying informed through reliable sources helps avoid misinformation and panic, allowing for a calm and coordinated response.

The mediaโ€™s role is critical. Sensationalism must give way to sober instruction. Social media platforms should coordinate with authorities to counter rumours. Panic can be as destructive as structural collapse. Preparedness is civic culture. It must become habitual.

From reaction to resilience

BANGLADESH has proven that it can transform disaster response. Cyclone management once symbolised helplessness; today it symbolises competence. That success was built on early warning systems, community engagement and strict institutional coordination.

Earthquake preparedness requires the same philosophy โ€” but with greater urgency. Cyclones offer hours of warning. Earthquakes do not.

This makes preventive measures more decisive than reactive ones. The cost of retrofitting, procurement of rescue equipment and training of urban search-and-rescue units may seem high in annual budgets. But the cost of inaction is measured in lives, not currency.

The prime ministerโ€™s directive signals recognition. A high-level review meeting to finalise post-disaster frameworks indicates seriousness. Fire Service and Civil Defence capacity enhancements are steps in the right direction. Yet leadership at the top must be matched by responsibility at every level โ€” local governments, hospitals, utility agencies, educational institutions and individual households.

A choice before the quake

HISTORY teaches a consistent lesson: disasters expose pre-existing weaknesses. When the ground eventually moves with force โ€” and in a tectonic region, it will โ€” the narrative that follows will not ask whether Bangladesh knew the risk. It will ask whether Bangladesh acted on what it knew.

Preparedness is not alarmism. It is prudence. We cannot relocate fault lines. We cannot prevent tectonic pressure from building. But we can reduce vulnerability. We can enforce standards. We can train volunteers. We can educate citizens. We can coordinate institutions.

Preparedness leads to protection. Neglect invites catastrophe. The tremors felt recently were warnings delivered without mass tragedy. Warnings are a gift history rarely gives twice.

Bangladesh stands at a moment of decision โ€” not during the shaking, but before it. Public awareness, institutional discipline and preventive governance will determine whether the next major earthquake becomes a national trauma or a testament to resilience. The earth will move when it chooses. The question is whether we will have moved first.

MA Hossain is a political and defence analyst based in Bangladesh.​
 
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