Bangladesh
is a part of the Bengal basin which is one of the most seismically
active zones of the world. Lying as it does in the confluence of the
India, Burma and Eurasia plate, the land is extremely prone to
earthquake disasters and in the past have experiences some of the
worst earthquakes in the history. However, a relatively long period
of "rest" from any major hazards and high attention paid to other
disasters such as cyclones, floods, etc. have led to both neglect
and denial of earthquake as the most destructive of all natural
disasters.
Although the world experiences millions of earthquakes every year,
few are felt because of their low intensity and magnitude. In
general there is a severe earthquake every year (more than 8), 10
large quakes and 100 moderate quakes. The movement of the earth's
plates which forms the thin outer shell of the earth's crust causes
earthquake. Bangladesh is in such a location.
The point of origin for quakes within the earth
is called focus and the point immediately above the focus is called
the epicenter. Shallow earthquakes occur 70 km. below the surface
while deeper ones happen 600 km. below.
The two measures for earthquakes are intensity
and Magnitude. Magnitude measures the energy released which is
generally based on the Richter scale measurements. Intensity
measures the scale of damage. So an earthquake of the same magnitude
may have different intensities depending on the havoc caused.
Seismic Zones in Bangladesh and
their Earth quake Potential |
Zones |
Operational Basis Magnitude
(Richter) |
Max. Credible Magnitude (
Richter) |
Depth of Focus (km) |
Asam-Meghalaya fault zone |
8.0 |
8.7 |
0 - 70 |
Tripura fault zone |
7.0 |
8.0 |
0 - 70 |
Sub-Dauki fault zone |
7.3 |
7.5 |
0 - 70 |
Bogra fault zone |
7.0 |
7.5 |
0 - 70 |
Chronology of Major Earthquakes
1548 The first recorded earthquake was a terrible one. Sylhet and
Chittagong were violently shaken, the earth opened in many places
and threw up water and mud of a sulphurous smell.
1642 More severe damage occurred in Sylhet district. Buildings were
cracked but there was no loss of life.
1663 Severe earthquake in Assam, which continued for half an hour
and Sylhet district was not free from its shock.
1762 The great earthquake of April 2, which raised the coast of Foul
island by 2.74m and the northwest coast of Chedua island by 6.71m
above sea level and also caused a permanent submergence of 155.40 sq
km near Chittagong. The earthquake proved very violent in Dhaka and
along the eastern bank of the Meghna as far as Chittagong. In Dhaka
500 persons lost their lives, the rivers and jheels were agitated
and rose high above their usual levels and when they receded their
banks were strewn with dead fish. A large river dried up, a tract of
land sank and 200 people with all their cattle were lost. Two
volcanoes were said to have opened in the Sitakunda hills.
1775 Severe earthquake in Dhaka around April 10, but no loss of
life.
1812 Severe earthquake in many places of Bangladesh around May 11.
The earthquake proved violent in Sylhet
1865 Terrible shock was felt, during the second earthquake occurred
in the winter of 1865, although no serious damage occurred.
1869 Known as Cachar Earthquake. Severely felt in Sylhet but no loss
of life. The steeple of the church was shattered, the walls of the
courthouse and the circuit bungalow cracked and in the eastern part
of the district the banks of many rivers caved in.
1885 Known as the Bengal Earthquake. Occurred on 14 July with 7.0
magnitude and the epicentre was at Manikganj. This event was
generally associated with the deep-seated Jamuna Fault.
1889 Occurred on 10 January with 7.5 magnitude and the epicentre at
Jaintia Hills. It affected Sylhet town and surrounding areas.
1897 Known as the Great India Earthquake with a magnitude of 8.7 and
epicentre at Shillong Plateau. The great earthquake occurred on 12
June at 5.15 pm, caused serious damage to masonry buildings in
Sylhet town where the death toll rose to 545. This was due to the
collapse of the masonry buildings. The tremor was felt throughout
Bengal, from the south Lushai Hills on the east to Shahbad on the
west. In Mymensingh, many public buildings of the district town,
including the Justice House, were wrecked and very few of the
two-storied brick-built houses belonging to zamindars survived.
Heavy damage was done to the bridges on the Dhaka-Mymensingh railway
and traffic was suspended for about a fortnight. The river
communication of the district was seriously affected
(Brahmaputra). Loss of life was not great, but loss of property was
estimated at five million Rupees. Rajshahi suffered severe shocks,
especially on the eastern side, and 15 persons died. In Dhaka damage
to property was heavy. In Tippera masonry buildings and old temples
suffered a lot and the total damage was estimated at Rs 9,000.
1918 Known as the Srimangal Earthquake. Occurred on 18 July with a
magnitude of 7.6 and epicentre at Srimangal, Maulvi Bazar. Intense
damage occurred in Srimangal, but in Dhaka only minor effects were
observed.
1930 Known as the Dhubri Earthquake. Occurred on 3 July with a
magnitude of 7.1 and the epicentre at Dhubri, Assam. The earthquake
caused major damage in the eastern parts of Rangpur district.
1934 Known as the Bihar-Nepal Earthquake. Occurred on 15 January
with a magnitude of 8.3 and the epicentre at Darbhanga of Bihar,
India. The earthquake caused great damage in Bihar, Nepal and Uttar
Pradesh but did not affect any part of Bangladesh. Another earhquake
occured on 3 July with a magnitude of 7.1 and the epicentre at
Dhubri of Assam, India. The earthquake caused considerable damages
in greater Rangpur district of Bangladesh.
1950 Known as the Assam Earthquake. Occurred on 15 August with a
magnitude of 8.4 with the epicentre in Assam, India. The tremor was
felt throughout Bangladesh but no damage was reported.
1997 Occurred on 22 November in Chittagong with a magnitude of 6.0.
It caused minor damage around Chittagong town.
1999 Occurred on 22 July at Maheshkhali Island with the epicentre in
the same place, a magnitude of 5.2. Severely felt around Maheshkhali
island and the adjoining sea. Houses cracked and in some cases
collapsed.
2003 Occurred on 27 July at Kolabunia union of Barkal upazila,
Rangamati district with
magnitude 5.1. The time was at 05:17:26.8 hours.
Major Earthquake Affecting
Bangladesh |
Date |
Name |
Magnitude |
Epicentre distance From Dhaka (km) |
10 Jan, 1869 |
Kachar earthquake |
7.5 |
250 |
14 Jul, 1885 |
Bengal earthquake |
7.0 |
170 |
12 Jun, 1897 |
Great Indian earthquake |
8.7 |
230 |
8 Jul, 1918 |
Srimangal earth quake |
7.6 |
150 |
2 Jul, 1930 |
Dhubri earthquake |
7.1 |
250 |
15 Jan, 1934 |
Bihar-Nepal earthquake |
8.3 |
510 |
15 Aug, 1950 |
Assam earthquake |
8.5 |
780 |
Zones of Vulnerability: In Bangladesh,
concern regarding the destructive capacity of earthquakes was linked
to the protection of major industrial and infrastructural
constructions especially those with foreign funding. This led to
preparation of vulnerability zoning maps. At present, Bangladeshis
divided into three zones with north and northeast-Sylhet, Mymensingh
and Rangpur, etc. in Zone 1 which is the most vulnerable. Zone 2
which runs across the middle of the country from northwest to
southeast includes Dhaka, Chittagong, Dinajpur, Bogra, Tangail, etc.
and zone 3 which is considered less risky, but as parts of an active
zone no part is fully safe. Zoning also changes according to the
movement of the plates and energies generated by the same.
Although there is an observatory in Chittagong, the situation of
that institution is dismal. It is practically not functioning. In
fact, few scientific activities regarding earthquakes are underway
in Bangladesh. However, the capacity of global level observatories
are very high and it is possible for these to communicate with
Bangladesh via Internet and satellites until something more
sustainable is established here. It should also be noted that
despite efforts, the capacity to predict earthquakes has yielded
poor results so the main work is monitoring the activities of the
plate and preparing the people.
Some Bangladeshi scientists studying the problem believe that
seismic pressure since the last major quake has built up quite high
and it is possible that an earthquake of 7 to 8 magnitude on the
Richter scale may hit Bangladesh anytime between 1998 to 2005.
Vulnerabilities: Vulnerabilities are
caused by many factories and some experts think that cities are more
susceptible to damage than rural areas which do not have high
structures. Falling structures in the urban areas, buildings made by
poor masonry, or construction of houses in areas which are subject
to soil liquefaction constitute immediate dangers as a results of
tremors. Liquefaction means the settling of loose soil which has a
high water content. Urbanization has forced development of housing
in many areas where the soil is not ready for construction
especially multistoried ones or where adequate piling has not been
carried out to prepare the ground.
The Government of Bangladesh set up a committee in 1992 to prepare a
Building Code, setting the minimum standards which had to be met to
construct a house. However, this has not been turned into a law as
yet. After the Guzrat earthquake the government has setup committee
to recommend action but the preparation level is still extremely
low.
In case an earthquake strikes, the utilities such as electricity,
water, gas, etc. will be badly affected and some may become threats
to life and resources as well. Gas and electricity originated fires
have generally killed hundreds of people, sometimes more than the
victims of collapsed buildings or masonry. Burst water pipes also
create extreme health hazards as unclean water spreads diseases
rapidly. The capacity of the response mechanism, if low, makes such
vulnerability into mega hazards. A general breakdown of the
socio-economic structure will accelerate the economic deprivation.
That will again create another set of vulnerabilities. It is now
accepted that pre-disaster planning is much more useful than
post-disaster mitigation. Many recommended actions are found in plan
books of earthquake sensitive countries. However, in Bangladesh,
this isn't the case.
The most critical part of any disaster prevention is public
awareness which is basically absent in Bangladesh. In order to
create a situation which may reduce vulnerability, an organized
plan, based on already existing recommendations taking into account
the various stages of preparation, should be made. There are many
manuals and informative documents available for earthquake
management but few are used or accessed and the threat of earthquake
is not recognized in Bangladesh. This is, despite the fact as many
fear that the next and inevitable earthquake may hurt millions of
people.
Source: Bangladesh National
Report
Progress of implementation of the Habitat Agenda (1996-2001)
Unlocking the Potential, National Strategy for Accelerated Poverty
Reduction (PRSP)
Government of the People’s Republic of Bangladesh
Bangladesh Environment Facing the 21st Century:SEHD
Peoples Report 2002-2003: Unnayan Shamannay
Compendium of Environment Statistics of Bangladesh: BBS |