1885 Kashmir Earthquake
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The 1885 Kashmir earthquake, also known as the Baramulla earthquake occurred on 30 May in
Srinagar Srinagar (English: , ) is the largest city and the summer capital of Jammu and Kashmir, India. It lies in the Kashmir Valley on the banks of the Jhelum River, a tributary of the Indus, and Dal and Anchar lakes. The city is known for its natu ...
. It had an estimated moment magnitude of 6.3–6.8 and maximum Medvedev–Sponheuer–Karnik scale intensity of VIII (''Damaging''). At least 3,081 people died and severe damage resulted.


Tectonic setting

Northern Pakistan and India is situated at the corner of an active destructive plate boundary that separates the Indian Plate from the Eurasian Plate. The boundary is defined along the Main Himalayan Thrust where the Indian Plate is colliding with the Eurasian Plate. The slightly oblique convergence occur at a rate of 17 ± 2 mm/yr along the Main Himalayan Thrust while the nearby
Karakoram fault system The Karakoram fault is an oblique-slip fault system in the Himalayan region across India and Asia. The slip along the fault accommodates radial expansion of the Himalayan arc, northward indentation of the Pamir Mountains, and eastward lateral ex ...
accommodates right-lateral
strike-slip In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements. Large faults within Earth's crust result from the action of plate tectonic ...
movement at 5 ± 2 mm/yr. The high convergence rate means many of the plate boundary faults are accommodating strain while locked, frequently releasing them in moderate-sized earthquakes, and sometimes in very large events. The occurrence of large earthquakes makes the Kashmir region vulnerable to deadly earthquakes. The region has hosted many large and destructive earthquakes since the beginning of records in 2082–2041 BCE. The most destructive is thought have occurred in
1555 Year 1555 ( MDLV) was a common year starting on Tuesday (link will display the full calendar) of the Julian calendar. Events January–June * January 22 – The Kingdom of Ava in Upper Burma falls. * February 2 – The Diet o ...
, and was the last major event in the
Kashmir Valley The Kashmir Valley, also known as the ''Vale of Kashmir'', is an intermontane valley concentrated in the Kashmir Division of the Indian- union territory of Jammu and Kashmir. The valley is bounded on the southwest by the Pir Panjal Range and ...
.


Earthquake

The earthquake was associated with a
rupture Rupture may refer to: General * Rupture (engineering), a failure of tough ductile materials loaded in tension Anatomy and medicine * Abdominal hernia, formerly referred to as "a rupture" * Achilles tendon rupture * Rupture of membranes, a "wate ...
on a shallow thrust fault, part of the Himalaya convergent boundary. It is located east of the rupture areas of the 2005 earthquake, and west of the 1555 earthquake. The 2005 and 1555 earthquakes are the most catastrophic events in the region with magnitudes estimated at 7.6 . Southeast of the Kashmir Valley are two very large thrust faults; the Main Boundary Thrust and Panjal Thrust. To the northeast of the valley, lies the Main Mantle Thrust. The closest faults to the valley are two out-of-sequence reverse faults known as the Kolbug and Balapur faults. The long Balapur Fault dips northeast at a steep angle of 60°. The parallel Kolbug Fault produced a 5.5 earthquake in 1963. The mainshock generated a surface rupture measuring , with a maximum ground offset of . The seismogenic structure responsible is named the Baramula-Loridor Fault.


Damage and casualties

At 02:24 local time on Sunday, May 30, the
Kashmir Valley The Kashmir Valley, also known as the ''Vale of Kashmir'', is an intermontane valley concentrated in the Kashmir Division of the Indian- union territory of Jammu and Kashmir. The valley is bounded on the southwest by the Pir Panjal Range and ...
was rocked by a strong earthquake with varying Modified Mercalli intensities of VI (''Strong'') to VIII (''Severe''). An assessment of the maximum
seismic intensity Seismic intensity scales categorize the intensity or severity of ground shaking (quaking) at a given location, such as resulting from an earthquake. They are distinguished from seismic magnitude scales, which measure the magnitude or overall stren ...
on the Environmental Seismic Intensity scale indicate a degree of X. A minor foreshock occurred the night before and was felt by several residents. The mainshock was followed by damaging
aftershock In seismology, an aftershock is a smaller earthquake that follows a larger earthquake, in the same area of the main shock, caused as the displaced crust adjusts to the effects of the main shock. Large earthquakes can have hundreds to thousand ...
s that continued till August 1885. On June 15, a strong aftershock was felt. A total of 3,081 people were killed. In
Srinagar Srinagar (English: , ) is the largest city and the summer capital of Jammu and Kashmir, India. It lies in the Kashmir Valley on the banks of the Jhelum River, a tributary of the Indus, and Dal and Anchar lakes. The city is known for its natu ...
with a population of 51,000, the city lost 2,000 residents. In the book ''
The Valley of Kashmir ''The Valley of Kashmir'' (1895) is a book on Kashmir by the English writer Sir Walter Roper Lawrence. The author served in the Indian Civil Service in British India during which he was appointed as a Settlement Commissioner of Kashmir. ''The V ...
'' by
Walter Roper Lawrence Sir Walter Roper Lawrence, 1st Baronet, (9 February 1857 – 25 May 1940) was a member of the British Council of India and an English author who served in the Indian Civil Service in British India and wrote travelogues based on his exper ...
, the death toll was 3,500. Heavy damage and great losses occurred due to the poor quality of homes. Poorly-constructed huts collapsed completely onto sleeping residents. An estimated 75,000 huts were destroyed. Livestock losses were also heavy; 25,000 sheep and goats, as well as 8,000 cattle, died. Many residents at a village were killed when a landslide measuring 800 meters was triggered. Liquefaction events including sand boils and fissures occurred on the banks of the Jhelum River at Pattan. Water flow also increased in natural springs. The towns of Baramulla and Sopore were destroyed. An estimated 67.33% of Baramulla's population was killed. Some 300 to 500 well-constructed wood and brick homes collapsed. Great devastation occurred in Barmulla where many people and cattle were fatally crushed. Vegetation on the nearby hillsides was wiped out by landslides. Many homes were buried. Large scarps formed on the slopes. One such landslide buried Laridura; only seven of the 47 residents survived.


See also

* List of earthquakes in India * List of earthquakes in Pakistan * List of historical earthquakes


References

{{Earthquakes in India 1885 in Asia 1885 in India 1885 disasters in India Earthquakes in India Earthquakes in Pakistan Geology of the Himalaya History of Kashmir