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Task Force Report - Govind Ballabh Pant Institute of Himalayan ...

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Table 2.13. Some Major Earthquake Events <strong>of</strong> the IHR<br />

Year State Epicentre Magnitude Impact<br />

(Richter Scale)<br />

1869 Assam 25 0 N, 93 0 E 7.5<br />

1885 Assam 34.1 0 N, 74.6 0 E 7.0<br />

1897 Assam 26 0 N, 91 0 E 8.7 Caused destruction in 3,70,000 sq. km area and<br />

was responsible for 1542 deaths.<br />

1905 Himachal Pradesh 32.3 0 N, 76.3 0 E 8.0<br />

1943 Assam 26.8 0 N, 94 0 E 7.2<br />

1950 Arunachal Pradesh 28.5 0 N, 96.7 0 E 8.5 Responsible for destruction in 46,000 sq. km.<br />

area. Raised the bed <strong>of</strong> the Brahmaputra river.<br />

1967 Jammu & Kashmir - 5.3-5.7 About 786 houses collapsed and 25,000<br />

partially damaged.<br />

1975 Himachal Pradesh 32.38 0 N, 78.49 0 E 6.2<br />

1986 Himachal Pradesh 32.1 0 N, 76.3 0 E 5.7 Responsible for six deaths.<br />

1988 Manipur 25.13 0 N, 76.3 0 E 6.6<br />

1991 Uttarakhand 30.75 0 N, 78.86 0 E 6.6 About 1000 people died, more than 30000<br />

houses destroyed<br />

1999 Uttarakhand 30.41 0 N, 79.42 0 E 6.8 Responsible for 100 deaths and collapse <strong>of</strong> 170<br />

houses.<br />

Source : Central Statistical Organization & IMD<br />

2.5.2. Avalanches & GLOFs<br />

Avalanches, the fast flow <strong>of</strong> snow or ice descending<br />

from and on mountain slopes, with detritus carry<br />

huge potential and kinetic energy, altering land<br />

forms, wiping out forests and damaging settlements<br />

and infrastructure. The Snow and Avalanche Study<br />

Establishment (SASE) <strong>of</strong> the Defense Research and<br />

Development Organization (DRDO) has estimated<br />

that some 30 people are killed every year due to<br />

avalanches in the IHR. The losses caused by some<br />

major avalanche disasters in IHR are given in Table<br />

2.14.<br />

Global climate change may result in rapid melting<br />

<strong>of</strong> big glaciers, <strong>of</strong>ten forming huge lakes. Due to<br />

the fast rate <strong>of</strong> melting, accumulation <strong>of</strong> water in<br />

these lakes may increase rapidly and may lead to a<br />

sudden rupture, discharging large volumes <strong>of</strong> water<br />

downslope, along with debris. This phenomenon<br />

is known as GLOF (Glacial Lake Outburst Flood)<br />

The resulting flood may be catastrophic in the<br />

downstream areas with loss <strong>of</strong> life and property,<br />

destruction <strong>of</strong> forests, agricultural land, and costly<br />

infrastructure <strong>of</strong> the mountains.<br />

In 2004, in a similar incident, the outlet <strong>of</strong> Pereechu<br />

lake in the Tibet region (35 km from India’s border<br />

with China) had been blocked due to a landslide.<br />

In the last week <strong>of</strong> June 2005, the water pressure<br />

broke through the debris resulting in a very heavy<br />

discharge in the Sutlej River. Considerable damage<br />

to property and infrastructure was caused in the<br />

lower regions <strong>of</strong> the state <strong>of</strong> Himachal Pradesh.<br />

In the north-western part <strong>of</strong> the IHR out <strong>of</strong> 156<br />

Glacial lakes <strong>of</strong> Himachal Pradesh 16 have been<br />

identified 29 as potentially dangerous while in the<br />

State <strong>of</strong> Uttarakhand there are 127 glacial lakes and<br />

29 Ives J.D., Shresstha R.B., and Mool P.K., 2010. Formation <strong>of</strong> Glacial lakes in the Hindu Kush-Himalayas and GLOF Risk Assessment.<br />

ICIMOD, Nepal.<br />

38<br />

<strong>Report</strong> <strong>of</strong> the <strong>Task</strong> <strong>Force</strong>

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