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Earthquake Hazards and
Disaster Management
H.S.VIRK
#360 Sector 71,SAS Nagar (Pb.), India
India: A Country Profile on
Disasters
• During the decade 1988-97, disasters in
India affected over 24 million people and
killed 5116 each year, on the average.
The economic loss amounted to 1884
million US $ per year.
• In India, 11.2 percent area is flood-prone,
28 percent of total cultivable area is
drought-prone and it is estimated that 57
percent of India is earthquake-prone.
Natural Hazards, Disasters and
Vulnerability
• Natural hazards become disasters when they
impact on the vulnerabilities of an area/region
and its people. For example, cigarette smoking
or drug-addiction is a health hazard, which can
become a disaster if the vulnerable section of
population is exposed to it freely.
The
vulnerability of a region is a complex
phenomenon; it is defined as the influence on it
by heterogeneity of social, political and
economic factors.
Natural or man-made
hazards impact differently in different parts of
the world depending upon vulnerability.
What is Vulnerability?
• The 1993, Latur earthquake of 6.3 M left
over 10,000 dead and destroyed 200, 000
households.
However,
much
more
powerful (7.5 M) Los Angeles earthquake
of 1971 killed only 55 persons. In India,
with a fast growing population, the disaster
mitigation and management must take into
account the assessment of risk and
vulnerability
of
the
area
under
consideration.
Indian Response to Disasters
• Keeping in view, the objectives of IDNDR and
Yokohoma Declaration, Indian Government has
planned for disaster preparedness, mitigation
and management at the national, state and
district level by creating infrastructure, namely
National Centre for Disaster Management
(NCDM), Calamity Relief Fund (CRF) at state
level and National Fund for calamity Relief
(NFCR) at national level.
Forecasting and
warning systems to deal with floods, cyclones,
droughts and earthquakes are being upgraded.
Disaster Mitigation & Management:
What is Our Contribution?
• Our Group in GND University was
involved in Earthquake Prediction studies
in Punjab and HP (Kangra & Chamba
valleys). We failed to predict Earthquakes
but our research has set some
benchmarks in this field.
• Radiation survey of Punjab was carried
out under DAE Project to determine effect
of Environmental Natural Radiation on the
health of its people.
Causes of Earthquakes
• Earthquakes (EQs) are caused by sudden
releases of strain energy accumulated during
long intervals due to relative motion of Tectonic
plates of earth; 6 major and 6 minor. EQs are of
two types: Tectonic and Volcanic. Tectonic EQs
are of three types: Interplate, Intraplate and
SCR(Stable Continental Region). Magnitude of
EQs is measured on Richter scale. EQ of 6.3M
is equivalent to the Atomic Bomb thrown on
Hiroshima in its destructive power.
Concept of Tectonic Plates
Global Frequency of Earthquakes
Magnitude

Description

No. of Earthquakes/Year

8.5 and up

Great

0.3

8-8.4

Great

1

7.5-7.9

Major

3

7-7.4

Major

15

6.6-6.9

Destructive

56

6-6.5

Destructive

210

5-5.9

Damaging

800

4-4.9

Minor

6200

3-3.9

Minor

49000

2-2.9

Minor

300000

0-1.9

Minor

700000
Population Growth and Fatalities
due to Earthquake Hazards
San Francisco Earthquake of 1906
The Great Kanto Earthquake(1923)
LIST OF SOME SIGNIFICANT EARTHQUAKES IN INDIA AND ITS NEIGHBOURHOOD
DATE

EPICENTRE

LOCATION

Lat( Deg N )

Long( Deg E )

1819 JUN 16

23.6

68.6

1869 JAN 10

25

93

1885 MAY 30

34.1

74.6

1897 JUN 12

26

91

1905 APR 04

32.3

1918 JUL 08

MAGNITUDE

KUTCH,GUJARAT

8.0

NEAR CACHAR, ASSAM

7.5

SOPOR, J&K

7.0

SHILLONGPLATEAU

8.7

76.3

KANGRA, H.P

8.0

24.5

91.0

SRIMANGAL, ASSAM

7.6

1930 JUL 02

25.8

90.2

DHUBRI, ASSAM

7.1

1934JAN 15

26.6

86.8

BIHAR-NEPALBORDER

8.3

1941 JUN 26

12.4

92.5

ANDAMAN ISLANDS

8.1

1943 OCT 23

26.8

94.0

ASSAM

7.2

1950 AUG 15

28.5

96.7

ARUNACHAL PRADESH-CHINA BORDER

8.5

1956 JUL 21

23.3

70.0

ANJAR, GUJARAT

7.0

1967 DEC 10

17.37

73.75

KOYNA, MAHARASHTRA

6.5

1975 JAN 19

32.38

78.49

KINNAUR, HP

6.2

1988 AUG 06

25.13

95.15

MANIPUR-MYANMAR BORDER

6.6

1988 AUG 21

26.72

86.63

BIHAR-NEPAL BORDER

6.4

1991 OCT 20

30.75

78.86

UTTARKASHI, UP HILLS

6.6

1993 SEP 30

18.07

76.62

LATUR-OSMANABAD, MAHARASHTRA

6.3

1997 MAY 22

23.08

80.06

JABALPUR,MP

6.0

1999 MAR 29

30.41

79.42

CHAMOLI DIST, UP

6.8

2001 JAN 26

23.40

70.28

BHUJ , GUJARAT

6.9
What is Earthquake Prediction?
• The ultimate aim of EQ prediction is to
establish reliability to issue timely warning
so as to save life and property. A valid
prediction should be based on four
essential elements:
• Time window in which the Event will occur.
• Location of the Event with all coordinates.
• Magnitude range, and
• Statistical probability of the Event.
Chamba (1995)

Uttarkashi (1991)

Chamoli
(1999)
Soil-Gas Emanometry

Radon Emanometer used for radon
sampling

Soil-gas probe used for radon sampling
Groundwater Emanometry

Groundwater radon sampling methodolgy
Radon Survey in Groundwater at Palampur
(Virk, Randhawa & Ramola)
Radon Monitoring in Chamba
(Virk, Walia & Santokh)
12

Dalhousie

Chamba
Eq. (M=5.1)

8
Soil-Gas

6

Groundwat er

Χ +2 σ=4.73

4

Χ+2 σ=4.52
Χ

2

Χ

Time Window (March 1995)

31

28

25

22

19

16

13

7

4

0

10

Χ −2 σ

MAR'95

Radon Conc. (Bq/L)

10

(Virk et al., 1995)
Palampur

80
Χ+2σ =69.66

70

Χ = 56.69
Χ+2σ = 46.63

40
30

Χ= 24.31

20
Groundwater
Soil-gas

10

31

29

27

25

23

21

19

17

15

13

11

9

7

5

3

0
Mar. 99

Radon Conc. (Bq/L)

60
50

Chamoli Eq
M=6.8

M=3.2
Ep = 87 km

Time window (March 1999)
(Virk et al. 2001)
5.6

Palampur

Chamoli Eq

5.5

5.3
5.2
5.1
5
4.9
4.8
4.7
Mar. 99
2
3
4
5
6
7
8
9
10
11
12
13
14
15
16
17
18
19
20
21
22
23
24
25
26
27
28
29
30
31

Helium Conc. (ppm)

5.4

Time window (March 99)

(Virk et al. 2001)
Variation of Radon Conc. with Microseismicity
in the region
90

30
Seismic Events/year
Avg. Rn conc./year

80

83

25

70

No. of Events/Year

60

70

80

20

50
15
40

40
30
20

10

Avg. Radon Conc./Year

79

27
19

5

20

10
0

0
1992

1993

1994

1995

1996

Time Window

1997

1998

1999

(Walia et al. 2003)
Proposed Earthquake Monitoring
Network for India
Latur- Killari Earthquake 6.3M
(1993)
Bhuj Earthquake 6.9M (2001)
Future Scenario of Earthquakes
Another Scenario (2002)
Learning Punjabi Folk Dance
ICRGG Conference, Amritsar
(1995)
ICGG Conference Besancon,
France(1993)
Thank You !!!

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Earthquake Hazards and Disaster Management in India

  • 1. Earthquake Hazards and Disaster Management H.S.VIRK #360 Sector 71,SAS Nagar (Pb.), India
  • 2. India: A Country Profile on Disasters • During the decade 1988-97, disasters in India affected over 24 million people and killed 5116 each year, on the average. The economic loss amounted to 1884 million US $ per year. • In India, 11.2 percent area is flood-prone, 28 percent of total cultivable area is drought-prone and it is estimated that 57 percent of India is earthquake-prone.
  • 3. Natural Hazards, Disasters and Vulnerability • Natural hazards become disasters when they impact on the vulnerabilities of an area/region and its people. For example, cigarette smoking or drug-addiction is a health hazard, which can become a disaster if the vulnerable section of population is exposed to it freely. The vulnerability of a region is a complex phenomenon; it is defined as the influence on it by heterogeneity of social, political and economic factors. Natural or man-made hazards impact differently in different parts of the world depending upon vulnerability.
  • 4. What is Vulnerability? • The 1993, Latur earthquake of 6.3 M left over 10,000 dead and destroyed 200, 000 households. However, much more powerful (7.5 M) Los Angeles earthquake of 1971 killed only 55 persons. In India, with a fast growing population, the disaster mitigation and management must take into account the assessment of risk and vulnerability of the area under consideration.
  • 5. Indian Response to Disasters • Keeping in view, the objectives of IDNDR and Yokohoma Declaration, Indian Government has planned for disaster preparedness, mitigation and management at the national, state and district level by creating infrastructure, namely National Centre for Disaster Management (NCDM), Calamity Relief Fund (CRF) at state level and National Fund for calamity Relief (NFCR) at national level. Forecasting and warning systems to deal with floods, cyclones, droughts and earthquakes are being upgraded.
  • 6. Disaster Mitigation & Management: What is Our Contribution? • Our Group in GND University was involved in Earthquake Prediction studies in Punjab and HP (Kangra & Chamba valleys). We failed to predict Earthquakes but our research has set some benchmarks in this field. • Radiation survey of Punjab was carried out under DAE Project to determine effect of Environmental Natural Radiation on the health of its people.
  • 7. Causes of Earthquakes • Earthquakes (EQs) are caused by sudden releases of strain energy accumulated during long intervals due to relative motion of Tectonic plates of earth; 6 major and 6 minor. EQs are of two types: Tectonic and Volcanic. Tectonic EQs are of three types: Interplate, Intraplate and SCR(Stable Continental Region). Magnitude of EQs is measured on Richter scale. EQ of 6.3M is equivalent to the Atomic Bomb thrown on Hiroshima in its destructive power.
  • 9. Global Frequency of Earthquakes Magnitude Description No. of Earthquakes/Year 8.5 and up Great 0.3 8-8.4 Great 1 7.5-7.9 Major 3 7-7.4 Major 15 6.6-6.9 Destructive 56 6-6.5 Destructive 210 5-5.9 Damaging 800 4-4.9 Minor 6200 3-3.9 Minor 49000 2-2.9 Minor 300000 0-1.9 Minor 700000
  • 10. Population Growth and Fatalities due to Earthquake Hazards
  • 12. The Great Kanto Earthquake(1923)
  • 13. LIST OF SOME SIGNIFICANT EARTHQUAKES IN INDIA AND ITS NEIGHBOURHOOD DATE EPICENTRE LOCATION Lat( Deg N ) Long( Deg E ) 1819 JUN 16 23.6 68.6 1869 JAN 10 25 93 1885 MAY 30 34.1 74.6 1897 JUN 12 26 91 1905 APR 04 32.3 1918 JUL 08 MAGNITUDE KUTCH,GUJARAT 8.0 NEAR CACHAR, ASSAM 7.5 SOPOR, J&K 7.0 SHILLONGPLATEAU 8.7 76.3 KANGRA, H.P 8.0 24.5 91.0 SRIMANGAL, ASSAM 7.6 1930 JUL 02 25.8 90.2 DHUBRI, ASSAM 7.1 1934JAN 15 26.6 86.8 BIHAR-NEPALBORDER 8.3 1941 JUN 26 12.4 92.5 ANDAMAN ISLANDS 8.1 1943 OCT 23 26.8 94.0 ASSAM 7.2 1950 AUG 15 28.5 96.7 ARUNACHAL PRADESH-CHINA BORDER 8.5 1956 JUL 21 23.3 70.0 ANJAR, GUJARAT 7.0 1967 DEC 10 17.37 73.75 KOYNA, MAHARASHTRA 6.5 1975 JAN 19 32.38 78.49 KINNAUR, HP 6.2 1988 AUG 06 25.13 95.15 MANIPUR-MYANMAR BORDER 6.6 1988 AUG 21 26.72 86.63 BIHAR-NEPAL BORDER 6.4 1991 OCT 20 30.75 78.86 UTTARKASHI, UP HILLS 6.6 1993 SEP 30 18.07 76.62 LATUR-OSMANABAD, MAHARASHTRA 6.3 1997 MAY 22 23.08 80.06 JABALPUR,MP 6.0 1999 MAR 29 30.41 79.42 CHAMOLI DIST, UP 6.8 2001 JAN 26 23.40 70.28 BHUJ , GUJARAT 6.9
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  • 19. What is Earthquake Prediction? • The ultimate aim of EQ prediction is to establish reliability to issue timely warning so as to save life and property. A valid prediction should be based on four essential elements: • Time window in which the Event will occur. • Location of the Event with all coordinates. • Magnitude range, and • Statistical probability of the Event.
  • 21. Soil-Gas Emanometry Radon Emanometer used for radon sampling Soil-gas probe used for radon sampling
  • 23. Radon Survey in Groundwater at Palampur (Virk, Randhawa & Ramola)
  • 24. Radon Monitoring in Chamba (Virk, Walia & Santokh)
  • 25. 12 Dalhousie Chamba Eq. (M=5.1) 8 Soil-Gas 6 Groundwat er Χ +2 σ=4.73 4 Χ+2 σ=4.52 Χ 2 Χ Time Window (March 1995) 31 28 25 22 19 16 13 7 4 0 10 Χ −2 σ MAR'95 Radon Conc. (Bq/L) 10 (Virk et al., 1995)
  • 26. Palampur 80 Χ+2σ =69.66 70 Χ = 56.69 Χ+2σ = 46.63 40 30 Χ= 24.31 20 Groundwater Soil-gas 10 31 29 27 25 23 21 19 17 15 13 11 9 7 5 3 0 Mar. 99 Radon Conc. (Bq/L) 60 50 Chamoli Eq M=6.8 M=3.2 Ep = 87 km Time window (March 1999) (Virk et al. 2001)
  • 28. Variation of Radon Conc. with Microseismicity in the region 90 30 Seismic Events/year Avg. Rn conc./year 80 83 25 70 No. of Events/Year 60 70 80 20 50 15 40 40 30 20 10 Avg. Radon Conc./Year 79 27 19 5 20 10 0 0 1992 1993 1994 1995 1996 Time Window 1997 1998 1999 (Walia et al. 2003)
  • 32. Future Scenario of Earthquakes