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earthquakes, Frequency, Magnitude and
intensity of earthquakes.,…
earthquakes
Richter
The Richter scale was developed in 1935, in
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Mercalli
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seismic intensity measurement. Take your name from its creator, Szuzupe
Mercury, an Italian volcanologist who invented it in 1902
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The magnitude of our earthquake shows how much energy was released from the epicenter of the earthquake at the time the rocks were broken, that is, how strong the earthquake is.
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Artificial: Artificial earthquakes are caused by explosions or hitting the surface of the earth's crust. They are usually used for submucosal tomography.
Volcanic: Volcanic is the name given to an earthquake that is the result of a change in pressure inside the earth due to the inflow or outflow of magma. The signal of such earthquakes is called volcanic vibration.
Installed earthquakes:
Installed earthquakes are due to the erosion of roofs of underground pits due to corrosion. They are usually small and local earthquakes.
Cold:
When its temperature drops below the critical point where liquid water becomes ice, the expansion caused by the water phase change compresses the rocks and it is possible that they will break.
Masonic:
Lithosphere consists of many lithospheric tectonic plates that are in constant motion floating on the fluid substrate of the patiosphere. The plates exert pressure on each other mainly due to the movements of the magma below those that carry them and less than the tidal forces that deform the earth by compressing and pulling it, the gravity that tends to sink the heaviest of them.
Frequency
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When an earthquake occurs, there is a release
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