Earthquake in India, Parts of Uttarakhand Wiki
Earthquake in India, Parts of Uttarakhand According to the information that i have collected data,this time an earthquake occured in India, parts of Uttarakhand, it was came few moments ago around 8:50 pm on 12/6/2017. The data that have collected in which the information is given this earthquake was about 5.1 richter scale. I hope all people are safe. here are some facts about he earthquake. Earthquake is called moving the surface of the earth. This happens due to seismic waves caused by sudden release of energy in the lithosphere of the earth. Earthquakes can be very violent and some have the ability to demolish people by hurting them and destroying the entire city.
Earthquake is measured with seismometer, which is also called seismograph. The magnitude of the magnitude of an earthquake is measured in a modest scale, or related and obsolete Richter magnitude is taken. Earthquake of 3 or less Richter magnitude intensity is often inconsistent, whereas an earthquake of 7-Richter intensity causes severe damage to large areas. The intensity of shaking is measured on the developed Mercalli scale.
On earth's surface, earthquakes reveal themselves by shaking or displacing the land. When a major earthquake occurs in the epicenter offshore, it causes adequate displacement on the shore of the sea, which is the reason for the tsunami. Earthquake shocks can sometimes cause landslides and volcanic activity.
In the most common sense, the word earthquake is used to describe any seismic event, a natural phenomenon]) or a phenomenon caused by humans - which produce seismic waves. Often earthquakes come due to geological flaws, heavy migration of gas, deep methane, earthquake, earthquake, and nuclear testing within the Earth are the main drawbacks.
The starting point of the occurrence of an earthquake is called the center or the hypo center. The word epicenter means the right point at the level of land.
San Andreas fault
In the case of, many earthquakes are produced away from the plate and are related to the increased stress in the wide area of distortion, these defects are due to major irregularities in the defect field. The Northridge earthquake was associated with blind pressure in one such field. Another example is the diagonal centrifugal plate boundary between the Arab and Eurasian plates, where it passes through the northwestern part of the Zagros mountains. The distortion associated with this plate boundary, is divided into nearly pure pressure speeds perpendicular to a large west-south border and nearly pure streak-slip speeds near the main fault near the actual plate boundary. It is demonstrated by the central mechanism of the earthquake.
All tectonic plates have internal pressure areas which are due to interaction with neighboring plates or sedimentary loading or unloading. (Such as deglaciation). These tensions may be due to the failure due to the presence of the present defect surfaces, they give rise to the interplate earthquake. Visit this link to see the earthquake video https://youtu.be/49Xpz79RMsY
Earthquake is measured with seismometer, which is also called seismograph. The magnitude of the magnitude of an earthquake is measured in a modest scale, or related and obsolete Richter magnitude is taken. Earthquake of 3 or less Richter magnitude intensity is often inconsistent, whereas an earthquake of 7-Richter intensity causes severe damage to large areas. The intensity of shaking is measured on the developed Mercalli scale.
On earth's surface, earthquakes reveal themselves by shaking or displacing the land. When a major earthquake occurs in the epicenter offshore, it causes adequate displacement on the shore of the sea, which is the reason for the tsunami. Earthquake shocks can sometimes cause landslides and volcanic activity.
In the most common sense, the word earthquake is used to describe any seismic event, a natural phenomenon]) or a phenomenon caused by humans - which produce seismic waves. Often earthquakes come due to geological flaws, heavy migration of gas, deep methane, earthquake, earthquake, and nuclear testing within the Earth are the main drawbacks.
The starting point of the occurrence of an earthquake is called the center or the hypo center. The word epicenter means the right point at the level of land.
San Andreas fault
In the case of, many earthquakes are produced away from the plate and are related to the increased stress in the wide area of distortion, these defects are due to major irregularities in the defect field. The Northridge earthquake was associated with blind pressure in one such field. Another example is the diagonal centrifugal plate boundary between the Arab and Eurasian plates, where it passes through the northwestern part of the Zagros mountains. The distortion associated with this plate boundary, is divided into nearly pure pressure speeds perpendicular to a large west-south border and nearly pure streak-slip speeds near the main fault near the actual plate boundary. It is demonstrated by the central mechanism of the earthquake.
All tectonic plates have internal pressure areas which are due to interaction with neighboring plates or sedimentary loading or unloading. (Such as deglaciation). These tensions may be due to the failure due to the presence of the present defect surfaces, they give rise to the interplate earthquake. Visit this link to see the earthquake video https://youtu.be/49Xpz79RMsY
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