A weak area below Jheel Park in Dhaula Kuan led to an earthquake: NCS | The latest news of India

The 4.0 earthquake that fled Delhi waking up early on Monday had a center under the garden of a generation in the southwest of Dawala Kwan and experts believed that the nature of the rocks deeply inside the earth – about 5 kilometers, where Tippolor – an unusual event.

A 20 -year -old tree was stormed at Jheel Park after the earthquake. (Al -Ani)

A preliminary analysis by the National Center for Seismology (NCS) said on a mistake that was a weak area in the Earth's crust, a feature known as “lineage”, different – especially less anxious – from the Tktone error line.

“The lineage is mainly a weak area. Op Mishra, NCS director said:” These genealogy can become a future error lines but at the present time it is a weak area. ”

Merena added that the origin of the weak region is likely to be in many “water channels with a porphieth and thus porous rocks.” “Hydrostatic cracking has occurred. This may have led to the earthquake. We can say that the earthquake did not happen on the limits of any error. Delhi may historically have these water channels and thus these rocks with pores.”

In other words, the rocks collapsed in the center of the earthquake, or broken, after weakened over the centuries due to the old waterways, which could have been rivers, current or another water body.

Although the water channel may no longer exist, the most porous structures that they left behind are filled with groundwater. This water, under gravity, finally accumulated what Merya noticed as hydrostatic pressure, leading to a “hydrostatic break” of the rocks that are manifested in the earthquake.

“The shaking was strong because this was a deeper shallow earthquake,” he added.

The analysis found that the geological features located below the surface in the surrounding area are varied, which are likely to contribute to the type of stress that led to the breaking of the rocks. In fact, an earthquake of 4.6 sized in December 2007, just 6 km from the Monday earthquake center.

The analysis said that this reveals a “natural pattern of seismic formation” associated with the unique structure of its kind underground, which the report describes as “a homogeneity under the surface of the weakest category”-mainly, the areas where the old rocks that occupy water occupy natural weaknesses In Delhi, the geological basis.

NCS experts saw positive signs in Monday's earthquake readings. “M4.0 earthquake is a good signature, as the rock materials of the source area that were launched before reaching the maximum credibility of its earthquake [intensity, of M4.6 of 2007]… “The report concluded.

Part of the positive sign was the sound that heard, which means that seismic waves had reached the surface and interacted with the air.

However, there are two known regional errors about the capital, which can be a source of more serious seismic activity: Mathura error and Sohna error.

Experts said that the earthquakes cannot be predicted, a greater threat to the national capital lies in the capabilities of Himalayas. “The Himalayas Mountains are region 5 and Delhi is region 4 mainly due to the proximity of the Himalayas and the high danger to the hemalayas earthquakes. This can be very intense due to the energy that is possible To 6.7 it happened in UT of Delhi, ”said JL Gutam, the former head of the office, NCS.

Delhi in both an active seismic area due to errors around the Delhi NCR region and its proximity to the Himalayas, which is very active.

Experts said that Delhi, classified in the fourth seismic region – is the second highest risk category – should be on alert due to many malfunctions and weak areas and near the Himalayas Mountains.

“When we have new construction, their construction and design must be flexible for the earthquake. For the current inventory of buildings, the update modification must be made after the evaluation. We also need to evaluate what can be allowed to constructions in the weak areas of the earthquake that has small bleeding maps. Most importantly, most of this There is a strict implementation of earthquake rules. Calashnd Sain, the former director of the Wadi Institute for Himalayas (Diedon) last year, said after the Nepal earthquake in October, we must live with earthquakes and we have to find a way to do so.

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