1897 - Assam,
India, Mw 8.0
Date 12th June 1897
Epicentre: 14 kilometres ESE of Sangsik (Meghalaya), India
Latitude: 25.50o N (2), Longitude: 91.00o E (2), Origin Time:
11:41 UTC (2) / 17:11 IST, Magnitude: Mw 8.0 (2), Mw 8.1 (3), Ms
8.0 (2), Moment: 1.28*10*21 Nm (2)
1,542 people were killed and
hundreds injured in Assam, in this earthquake. It had a
magnitude estimated variously between Ms 8.0 and Mo 8.1. The
earliest report of extreme ground acceleration is recorded for
this earthquake, where stones on the roads of Shillong as said
to have "vibrated like peas on a drum". Recent studies also
indicate that this might have been a blind earthquake, therefore
making it the largest blind earthquake ever known.
The earthquake was centred 14 kms ESE of Sangsik (Meghalaya),
India, Mystery of Assam Earthquake (1897) solved April 12, 2001
The cause of the great earthquake in north east India that
killed thousands and reduced buildings to rubble in a region the
size of England appears to have been settled.
Estimated to be an 8.1 magnitude quake, the extremely violent
event caused part of the overlying Shillong Plateau to shoot up
nearly 15m in just three seconds. Prof. Roger Bilham (University
of Colorado at Boulder) and Oxford University Prof. Philip
England believe the Assam earthquake was most likely caused by
two adjacent faults rupturing beneath the Earth’s surface in
India near Bangladesh.
Assam , 1950 August 15
14:09 UTC 8.6M
This great earthquake,
destructive in Assam, has a calculated magnitude of 8.6 and
Strasbourg regards it as the most important since the
introduction of seismological observing stations. Alterations of
relief were brought about by many rock falls in the Mishmi Hills
and destruction of forest areas. In the Arbor Hills 70 villages
were destroyed with 156 casualties due to landslides. Dykes
blocked the tributaries of the Brahmaputra; that in the Dibang
valley broke without causing damage, but that at Subansiri
opened after an intermal of 8 days and the wave, 7 metres high,
submerged several villages and killed 532 persons.
Two thousand homes, temples and mosques destroyed. Hardest hit
is the Brahmaputra Basin in NE India This shock was more
damaging in Assam, in terms of property loss, than the
earthquake of 1897. To the effects of shaking were added those
of flood; the rivers rose high after the earthquake, bringing
down sand, mud, trees, and all kinds of
debris. Pilots flyng over the meizoseismal area reported great
changes in topography; this was largely due to enormous slides,
some of which were photographed.
Earthquakes in Cachar
1984 - Cachar (Assam),
India, Mw 6.0
Date: 31st December 1984
Epicentre: 4.9 kilometers W of Palanghat (Assam), India
Latitude: 24.66o N (3), Longitude: 92.85o E (3), Origin Time:
23:33:35 UTC / 06:03:35 IST (3), Magnitude: Mw 6.04, Mb 5.9 (3),
Moment: 1.3*10*18 Nm (3)
The earthquake was centred 4.9 kilometres W of Palanghat
(Assam), India, The shock was felt in much of North-east India
and Bangladesh. In the Cachar district, 20 persons were killed
and 100 were injured. There was extensive damage in southern
Assam. Underground pipes were broken and the ground was
cracked. Sand, mud and water spewed forth and subsidence
occurred along wide stretches of the Sonai River. Two bridges
on the Sonai - Kachidharan road collapsed and others were
damaged. It was felt with an intensity of VI at Banskandi and
Palanghat, Kumbhirgram, Lakhipur, Rajabazar, Silchar and
Udarband.
1869 - Cachar (Assam),
India, M 7.5
Date 10th January 1869
Epicentre: 9.4 kilometers N of Kumbhir (Assam), India
Latitude: 25.00o N (2), Longitude: 93.00o E (2), Origin Time:
11:45 UTC / 17:15 IST (3)
Magnitude: 7.5 (2) Max. Intensity: VIII (1)
This earthquake was centred 9.4 kilometres N of Kumbhir (Assam),
India. There was heavy damage in the towns of Cherrapunji,
Silchar, Shillong and Sylhet and also in Manipur. Fissures
opened on the banks of the Surma river and sand vents threw up
great amounts of sand and water. The epicentral tract was 30 -
45 kilometres long and 5 - 6 kilometres wide lying on the
northern border of the Jaintia Hills. The hypocentre had a depth
of 50 kilometres.
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