{"id":311862,"date":"2019-05-03T08:16:38","date_gmt":"2019-05-03T08:16:38","guid":{"rendered":"http:\/\/tehelka.com\/?p=311862"},"modified":"2019-06-26T07:51:15","modified_gmt":"2019-06-26T07:51:15","slug":"mega-earthquake-may-catch-india-unprepared","status":"publish","type":"post","link":"https:\/\/tehelka.com\/mega-earthquake-may-catch-india-unprepared\/","title":{"rendered":"Mega earthquake may catch India unprepared"},"content":{"rendered":"

\"\"<\/a>The Indian subcontinent has a history of earthquakes. The reason for the intensity and high frequency of earthquakes is the Indian plate driving into Asia at a rate of approximately 47 mm\/year. The latest one before this edition went to bed was the strong 6.1-magnitude earthquake that struck the country\u2019s northeastern state of Arunachal Pradesh early on April 24. The epicenter of the shallow quake was about 40 kilometres southeast of Along, and 180 kilometres southwest of the state capital Itanagar.<\/span><\/p>\n

Such quakes are minor. But a mega earthquake of magnitude 8.5 or more is long overdue in the Himalayan region. Sadly, India has not learnt from past mistakes and is far from being prepared for such an eventuality with no strategy to minimise loss of life and property. The government must ensure seismic safety, scientists from all over the country who gathered here last week for a global workshop said.<\/span><\/p>\n

The April 18-20 International Workshop on Climate Change and Extreme Events in Himalayan Region, hosted by the Indian Institute of Technology (IIT) Mandi, was aimed at understanding the effects of climate change, melting of <\/span>glaciers, increased frequency of extreme events, atmospheric pollution, pollution due to crop residue burning in Himalayan region and applications of remote sensing. Scientists from various fields of expertise concurred that an earthquake of the magnitude of 8.5 or more is <\/span>expected to rock the Himalayan region.<\/span><\/p>\n

One of the many topics discussed at the event was that the Himalayan region was not prepared to reduce loss of lives and properties when the \u2018big one\u2019 arrives. Numerous research groups, including one at IIT Roorkee, are in the process of developing earthquake early warning systems which could give people up to a minute of warning before the quake. However, such short term predictions are not best way forward, said Dr Supriyo Mitra from Indian Institute of Science Education and Research (IISER), Kolkata. \u201cI would prefer being a society that is prepared,\u201d Mitra was quoted as saying.<\/span><\/p>\n

Even if seismologists are able to provide an early warning to enable people to safely vacate their buildings before an earthquake, our homes would still be destroyed, turning a whole society into refugees, he said. \u201cWe have the expertise to know what the hazards are. Engineers can work out the vulnerability of the structures and tell you the mechanism by which they can be made resistant,\u201d said Mitra, one of the speakers at the workshop.<\/span><\/p>\n

Implementing these would reduce the risk to human lives and property in the event of a disaster. \u201cScience can tell you where an earthquake may strike, and with what magnitude, but \u2018when\u2019 is a bad question to ask,\u201d Mitra said, adding that earthquake predictions shift the onus of responsibility of disaster preparedness completely to scientists.<\/span><\/p>\n

Heavy damage awaits Delhi-NCR <\/strong><\/span><\/p>\n

If a large magnitude earthquake occurs in the near future in the northwest (NW) Himalayas region as predicted by a recent study, the National Capital Region (NCR) of Delhi would suffer very heavy damage. The 2001 earthquake in Bhuj in Gujarat, which claimed about 10,000 lives, had shown that the destruction by an earthquake is caused by two different types of waves: Shear Waves, confined to about 70 to 100 km from the epicentre and which adversely affect the foundations and basements of structures; and Rayleigh Waves that travel with a velocity between 2.5 to 3 km per second and produce a different type of destructive effect.<\/span><\/p>\n

These Rayleigh Waves from earthquakes of magnitude above 7.5 become active at a distance beyond 150 to 200 km or more from the epicentre and adversely affect tall structures (height more than 17 meters) as was observed at Ahmedabad city located at a distance of about 320 km from the Bhuj earthquake\u2019s epicentre. Another very important observation was that all structures with \u201cstilted\u201d floors (where the ground floor is used for vehicle parking) were severely damaged. A similar damaging effect by Rayleigh waves was observed in Mexico City, located about 500 km from the epicentre of the 1985 earthquake.<\/span><\/p>\n

The Himalayan states had been visited by a number of large magnitude earthquakes and a recent study suggests the NW region (mostly Uttarakhand, Himachal Pradesh and parts of Kashmir) is ripe for one. The Delhi NCR escaped major damage from the destructive Rayleigh Waves from past earthquakes because, prior to 1950, there were no high rise buildings there.<\/span><\/p>\n

But the situation is now different. With its satellite townships of Noida, Greater Noida, Gurugram, Ghaziabad and Faridabad, NCR Delhi forms a big cluster of high-rise buildings with flyovers, bridges and elevated roads. It is also known that some of the high-rise structures have <\/span>collapsed during construction itself. <\/span>Many high-rise buildings have stilted floors. As was witnessed in Ahmedabad after the Bhuj earthquake, all these structures could suffer heavy damage in case <\/span>of a large magnitude earthquake in the NW Himalayan region with its epicentre in the range of 270 to 350 km from NCR Delhi.<\/span><\/p>\n

The Himalayan fault is known to have a potential to generate earthquakes up to a magnitude of 8 or more. The foundations in Delhi are not on solid rock but there is excess of soil and crushed rock (murrum) on the ground. In case of a powerful earthquake in the Himalayas, the long scissors of Rayleigh Waves could wildly chop the tall concrete structures in Delhi and neighbouring areas. The possibility that these buildings may collapse like a pack of cards in \u201cAhmedabad Fashion\u201d cannot be ruled out.<\/span><\/p>\n

Fluctuations in the Earth\u2019s rotation are tiny – changing the length of the day by several milliseconds – but could be enough to release vast amounts of underground energy, they have said. It has been reported that on five occasions in the past century, a 25-30 per cent increase in annual number of earthquakes (of magnitude 7 or greater) coincided with a slowing in the mean <\/span>rotation velocity of the Earth. The slowing down of Length of Day (LoD) normally lasts for six years, after which the earth enters a period of enhanced seismicity. In this century, the LoD started in 2011 and now the year 2018 could be considered a period of higher seismic activity. While <\/span>the research did not indicate precisely when and where these future earthquakes will occur, it showed that most of the intense earthquakes that responded to changes in day length seemed to occur near the equator.<\/span><\/p>\n

Public involvement<\/strong><\/span><\/p>\n

However, to ensure preparedness, the public needs to be involved in questioning whether their buildings are safe. Participants at the workshop, as per a news agency report, also raised questions on how socio-economically weaker sections would invest in building earthquake resistant buildings. Dr Durgesh C Rai from IIT Kanpur said it is the right of every individual to have seismic safety, and the government has to ensure that. \u201cSeismic safety should not be an optional requirement,\u201d he said.<\/span><\/p>\n

While presenting his research, Rai <\/span>focused on how publicly-funded government buildings in Himalayan states such as Sikkim and Manipur could not survive even low intensity earthquakes. According to him, we continue to repeat the same mistakes time and again, and have not learnt any lessons from the failures of the past. Giving the example of the 1993 earthquake that struck Latur, Maharashtra \u2014 killing over 9,000 people \u2014 Rai said <\/span>government agencies and academicians were of the view that buildings which collapsed were non-engineered. \u201cSo the deaths of people were linked to their poverty,\u201d he added.<\/span><\/p>\n

\u201cIn 2001, the Bhuj earthquake \u2014 120 multi-storey buildings collapsed in Ahmedabad \u2014 killed over 900. This was engineered construction. The investigations showed that every building code was flouted,\u201d Rai said. \u201cEarthquakes need not be deadly or destructive if we use the right designs and materials.\u201d He added that seismic safety should not be an optional feature that people have to ask for. Rather, all buildings should be built to be earthquake safe by default \u2014 much like medical instruments are sterilised before use, irrespective of whether a patient is rich or poor. He pointed out that many older buildings in the Himalayan arc have survived earthquakes for decades, and these could serve as lessons for our future. \u201cLoss of life occurs due to building collapse and damage, we need to engineer structures with proper building codes,\u201d said Ramesh P Singh, coordinator of the workshop, and visiting professor at IIT Mandi.<\/span><\/p>\n

\n

letters@tehelka.com<\/span><\/p>\n","protected":false},"excerpt":{"rendered":"

The Indian subcontinent has a history of earthquakes. The reason for the intensity and high frequency of earthquakes is the Indian plate driving into Asia at a rate of approximately 47 mm\/year. The latest one before this edition went to bed was the strong 6.1-magnitude earthquake that struck the country\u2019s northeastern state of Arunachal Pradesh […]<\/p>\n","protected":false},"author":6,"featured_media":311882,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":[],"categories":[23,2205],"tags":[],"_links":{"self":[{"href":"https:\/\/tehelka.com\/rest-api\/wp\/v2\/posts\/311862"}],"collection":[{"href":"https:\/\/tehelka.com\/rest-api\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/tehelka.com\/rest-api\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/tehelka.com\/rest-api\/wp\/v2\/users\/6"}],"replies":[{"embeddable":true,"href":"https:\/\/tehelka.com\/rest-api\/wp\/v2\/comments?post=311862"}],"version-history":[{"count":2,"href":"https:\/\/tehelka.com\/rest-api\/wp\/v2\/posts\/311862\/revisions"}],"predecessor-version":[{"id":311884,"href":"https:\/\/tehelka.com\/rest-api\/wp\/v2\/posts\/311862\/revisions\/311884"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/tehelka.com\/rest-api\/wp\/v2\/media\/311882"}],"wp:attachment":[{"href":"https:\/\/tehelka.com\/rest-api\/wp\/v2\/media?parent=311862"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/tehelka.com\/rest-api\/wp\/v2\/categories?post=311862"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/tehelka.com\/rest-api\/wp\/v2\/tags?post=311862"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}