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Are these tremors? Is a stronger earthquake coming?
New Delhi: The Wadia Institute of Himalayan Geology, affiliated with the Ministry of Science and Technology, said the recent tremors in Delhi – NCR do not indicate a major event, although a strong earthquake cannot be judged. She said that such tremors are not unusual in the Delhi-NCR region but that stress energy is accumulating in the region. Rohtak recorded slight tremors on June 19 and 20. Also read – 2.3 magnitude hits the Rohtak earthquake again, the second time in two days
The institute said in a statement that all earthquakes in Delhi – NCR are due to the release of the stress energy that has accumulated as a result of the northern movement of the Indian tectonic plate and its collision with the Eurasian plate through the rift or weak areas. . Also read – 4.6-magnitude earthquake jolts parts of Delhi NCR, the epicenter of the earthquake in Haryana
There are many weak areas and faults in Delhi-NCR: the Delhi-Haridwar chain, the Mahindra-Dahradon underground error, the Moradadad mistake, the Sauna error, the big boundary fault, the Delhi-Sargodha chain, the Yamuna river line, the Ganga river line,. Also read – Haryana Council Elections 2019: After Bhiwani, Amit Shah Bachs Congress in Rohtak Rally
List of recent earthquakes
All the last 17 earthquakes recorded in the Delhi-NCR region were of low to moderate intensity on the Richter scale.
April 12 – Delhi (3.5) April 13 – Delhi (2.7) April 16 – Delhi (2) May 3 – Delhi (3) May 6 – Faridabad (2.3) May 10 – Delhi (3.4) May 15 – Delhi (2.2) May 28 – Faridabad (2.5) May 29 – Rohtak (4.5 and 2.9) June 1 – Rohtak (1.8 and 3) June 3 – Faridabad (3.2) June 4 – Rohtak (2.1) June 8 – Delhi – Gurgaon border (2.1) June 18 – Rohtech (2.1) June 19 – Rohtech (2.3).
Of these 17, the earthquake in Rohtak was just above 4 on the Richter scale, which is located under a moderate intensity earthquake.
The historical seismological catalog shows that there were strong 6.5 earthquakes in Delhi in 1720; 6.8 at Mathura in 1803; 5.5 near Mathura in 1842; 6.7 near Bulandshahar in 1956; 6 near Faridabad in 1960 and 5.8 near Muradabad in 1966 in Delhi-NCR.
Delhi-NCR was identified as the second highest seismic hazard zone (fourth region).
Of the 14 minor earthquakes in Delhi-NCR, the statement said, “Sometimes the vulnerable area remains calm and suffers from small earthquakes that do not indicate any larger earthquake, or receive a sudden earthquake due to a large earthquake without any call.” It added that the Rohtak earthquake on May 29 had a magnitude of 4.6.
“Since the earthquake cannot be predicted by any mechanism, the tremors cannot be described as a sign of a major event,” she said.
She added that recent events cannot be defined as “aftershocks”. If a major earthquake strikes in an area, all the smaller tremors that occurred in the recent past in that region are classified as earthquakes.
So, scientifically, all of these tremors in Delhi-NCR can only be identified as earthquakes immediately after a major earthquake. The institute said in the statement that although it was unpredictable, a stronger earthquake that posed a threat to people and property could not be ruled out.
“Although our understanding, in terms of when, where and with the amount of energy (or magnitude) that an earthquake can cause, is not clear, but it is possible to understand the region’s weakness from previous earthquakes, computing a budget for pressure, and mapping and adding” active errors. “
The institute added that since any mechanism is unpredictable, the tremors cannot be described as a sign of a major event.
(With PTI input)
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