A big news is coming out from Tibet. Where the earthquake was felt in the earthquake at 2:41 pm Indian time after midnight on Sunday. According to the National Center for Sisamology (NCS), the intensity of the earthquake was measured 5.7 on the Richter scale. The epicenter of the earthquake was located in the Tibet region. However, no information has been revealed about the loss of any kind of life and property so far. Giving information, NCS said that they are constantly monitoring the geological movements of the area. At the same time, administration and disaster management teams are cautious and are monitoring the situation.
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An Earthquake with a magnitude of 5.7 on the richter scale hit at 02.41 am (IST) Today: National Center for Seismology (NCS) pic.twitter.com/nihqvltwwi
There are 7 plates inside the earth, which continue to rotate. Where these plates collide more, it is called Zone Fault Line. Repeated collisions turn corners of plates. When there is more pressure, the plates start to break. The bottom energy finds a way to come out and the disturbance leads to an earthquake.
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Learn what is the center and intensity of earthquake?
The center of the earthquake is the place that removes geological energy in the plates just below. Earthquake vibrations at this place. As the frequency of vibration goes away, its effect decreases. However, if there is an earthquake of 7 or more on the Richter scale, then the shock of 40 km around is intensified. But it also depends on whether the seismic frequency is upwards or in the scope. If the frequency of vibration is up to the top, the less area will be affected.
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How is measured earthquake and what is measuring measuring measuring?
The earthquake is investigated by the Richter scale. This is called Richter Magnitured Test Scale. The earthquake on the Richter scale is measured from 1 to 9. The earthquake is measured by its center ie epicenter. The intensity of the energy that comes out from within the earth during the earthquake is measured by it. With this intensity, there is an idea of ​​the magnitude of earthquake shock.
