Another quake of magnitude 3.4 was recorded in the city in 2001, according to official data.

It is principally due to the transfer of the Ground rupture is a visible breaking and displacement of the Earth's surface along the trace of the fault, which may be of the order of several meters in the case of major earthquakes.

This effect is called site or local amplification. The National Centre for Seismology said that the earthquake occurred at 5.45 pm and the epicentre in NCT Delhi at the depth of 8 km.

The velocity of S-waves ranges from 2–3 km (1.2–1.9 mi) per second in light sediments and 4–5 km (2.5–3.1 mi) per second in the Earth's crust up to 7 km (4.3 mi) per second in the deep mantle. The quake occurred at 1.11 pm, it added. Also the effects of strong ground motion make it very difficult to record information close to a nucleation zone.Most earthquakes form part of a sequence, related to each other in terms of location and time.An aftershock is an earthquake that occurs after a previous earthquake, the mainshock. In the lower crust, they travel at about 6–7 km (3.7–4.3 mi) per second; the velocity increases within the deep mantle to about 13 km (8.1 mi) per second. Another quake of magnitude 3.4 was recorded in the city in 2001, according to official data.The major quakes recorded near the national capital were at Bulandshahr of magnitude 6.7 on October 10,1956, and at Mordabad of magnitude 5.8 on August 15, 1966. The world is divided into 754 Although relatively slow seismic waves have traditionally been used to detect earthquakes, scientists realized in 2016 that gravitational measurements could provide instantaneous detection of earthquakes, and confirmed this by analyzing gravitational records associated with the The effects of earthquakes include, but are not limited to, the following: In Delhi's adjoining western Uttar Pradesh, Bulandshahr had recorded an earthquake of magnitude 6.7 on October 10, 1956, while Mordabad registered a 5.8 magnitude quake on August 15, 1966. In Earthquakes often occur in volcanic regions and are caused there, both by A tectonic earthquake begins by an initial rupture at a point on the fault surface, a process known as nucleation. Parts of New Delhi and its adjoining areas also felt tremors at around 1.45 pm.

For seismic migration, see Shaking of the surface of the earth caused by a sudden release of energy in the crustIntensity of earth quaking and magnitude of earthquakesSibson, R.H. (2002) "Geology of the crustal earthquake source" International handbook of earthquake and engineering seismology, Volume 1, Part 1, p. 455, eds.

Praying for everyone’s safety.Delhi Chief Minister Arvind Kejriwal also tweeted, saying he was praying for the safety of the people.On April 12, a similar medium intensity earthquake of magnitude 3.5 struck the national capital and tremors were felt in Noida and Ghaziabad as well. “Earthquake of magnitude 4.5 on the Richter scale struck 119 km North-Northwest of Kargil, Ladakh,” the NCS said. Thrust faults are generated by the highest, strike-slip by intermediate, and normal faults by the lowest stress levels.All tectonic plates have internal stress fields caused by their interactions with neighboring plates and sedimentary loading or unloading (e.g., deglaciation).The majority of tectonic earthquakes originate at the ring of fire in depths not exceeding tens of kilometers. On average, the kilometer distance to the earthquake is the number of seconds between the P- and S-wave S-waves and later arriving surface waves do most of the damage compared to P-waves. An aftershock is in the same region of the main shock but always of a smaller magnitude. A Comparative Seismology. When the Tectonic earthquakes occur anywhere in the earth where there is sufficient stored elastic strain energy to drive fracture propagation along a There are three main types of fault, all of which may cause an This is so because the energy released in an earthquake, and thus its magnitude, is proportional to the area of the fault that rupturesThe most important parameter controlling the maximum earthquake magnitude on a fault, however, is not the maximum available length, but the available width because the latter varies by a factor of 20. The possibility that the nucleation involves some sort of preparation process is supported by the observation that about 40% of earthquakes are preceded by foreshocks. "Earthquake of Magnitude: 3.5 just happened in Delhi NCR. A medium-intensity earthquake of magnitude 4.5 hit Ladakh on Thursday afternoon, the National Centre for Seismology said. About 100,000 of these can be felt.The number of seismic stations has increased from about 350 in 1931 to many thousands today. Parts of New Delhi and its adjoining areas also felt tremors at around 1.45 pm. The tremors were felt for several seconds and many people rushed out of their homes.An earthquake of magnitude 2.8 had hit the national capital in 2004.

Specific local geological, geomorphological, and geostructural features can induce high levels of shaking on the ground surface even from low-intensity earthquakes.

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