what is the relationship between earthquake?
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Earthquakes occur on faults - strike-slip earthquakes occur on strike-slip faults, normal earthquakes occur on normal faults, and thrust earthquakes occur on thrust or reverse faults. When an earthquake occurs on one of these faults, the rock on one side of the fault slips with respect to the other.
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Quakes can strike near the surface or deep within the Earth. Most quakes occur at shallow depths, according to the U.S. Geological Survey. ... Shallow quakes generally tend to be more damaging than deeper quakes. Seismic waves from deep quakes have to travel farther to the surface, losing energy along the way.
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The earthquake are more likely to occur in the danger zones of the world like Tibet , Japan . The Brainliest Answer! Earthquakes occur all the time all over the world, both along plate edges and along faults. Most earthquakes occur along the edge of the oceanic and continental plates.
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Earthquake being a natural disaster, when it occurs, the Government has to take very well structured responsibility to ensure help to the effected people,living beings, non-living structures etc,so that the damages caused by earthquake can be minimised.At the national and state level Disester Management Forces work for ...
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Earthquakes with a magnitude of 5.0 or lower occur almost daily in Indonesia, while more major earthquakes have occurred about once a year throughout the nation's history. These earthquakes often trigger tsunamis or floods that devastate communities.
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Subduction zones and earthquakes. Subduction zones are plate tectonic boundaries where two plates converge, and one plate is thrust beneath the other. This process results in geohazards, such as earthquakes and volcanoes.
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Several Chinese researchers believed that there was a certain relation between rainstorm floods and earthquakes [38–40]. They proposed that the occurrence of flood, drought, and other natural calamities after an earthquake might relate to the earth degassing effect which is both the cause and effect of an earthquake.
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Some, but not all, earthquakes are related to volcanoes. For example, most earthquakes are along the edges of tectonic plates. This is where most volcanoes are too. However, most earthquakes are caused by the interaction of the plates not the movement of magma .
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Two of these moving plates meet in western California; the boundary between them is the San Andreas fault. The Pacific Plate (on the west) moves northwestward relative to the North American Plate (on the east), causing earthquakes along the fault.
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Earthquakes can occur at the three different plate boundaries, but some plate boundaries produce more earthquakes. This is due to the amount of friction exerted on the rocks. Transform plate boundaries occur where one plate slides past another. Only strike-slip faults are associated with transform boundaries.
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There are many different types of earthquakes: tectonic, volcanic, and explosion. The type of earthquake depends on the region where it occurs and the geological make-up of that region. The most common are tectonic earthquakes.
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Quakes can strike near the surface or deep within the Earth. Most quakes occur at shallow depths, according to the US Geological Survey. ... Shallow quakes generally tend to be more damaging than deeper quakes. Seismic waves from deep quakes have to travel farther to the surface, losing energy along the way.
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Magnitude is a measure of earthquake size and remains unchanged with distance from the earthquake. Intensity, however, describes the degree of shaking caused by an earthquake at a given place and decreases with distance from the earthquake epicentre.
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The Richter scale rates earthquakes based on the size of their seismic waves, as measured by seismographs. The moment magnitude scale rates earthquakes based on the total amount of energy they release.
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Most earthquakes and volcanoes occur because of the movement of the plates, especially as plates interact at their edges or boundaries. At diverging plate boundaries, earthquakes occur as the plates pull away from each other. ... This process, called subduction, takes place because one plate is denser than the other.
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There is no such thing as "earthquake weather". ... Very large low-pressure changes associated with major storm systems (typhoons, hurricanes, etc) are known to trigger episodes of fault slip (slow earthquakes) in the Earth's crust and may also play a role in triggering some damaging earthquakes.
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Aftershocks are earthquakes that usually occur near the mainshock. ... An earthquake will be called an aftershock as long as the rate of earthquakes is higher than it was before the mainshock. For big earthquakes this might go on for decades. Bigger earthquakes have more and larger aftershocks.