Aftershocks don't occur in the same place since the pressure right there has alreadybeen relieved.
Earthquakes can pressure highly stressed fault lines and trigger subsequent seismic events. If correct, so-called stress triggering theory could help scientists pinpoint areas where earthquakes are imminent. The earthquakes immediately following one earthquake are called aftershocks. Tectonic plates are moving all the time. The aftershocks can occur because the initial earthquake may have moved things into another position. Then the plates will make additional small adjustments (the aftershocks) to release new pressures that the initial earthquake caused between tectonic plates when they moved. The fault line between the plates may become less stable and then later an entirely new earthquake may occur at the same or at a close by site. It is the instability of the tectonic plates left after one earthquake that can cause others.
It is possible but extremely unlikely. If a tornado an earthquake were to strike at the same time it would be purely by coincidence.
What is an earthquake?An earthquake is what happens when two blocks of the earth suddenly slip past one another. The surface where they slip is called the fault or fault plane. The location below the earth's surface where the earthquake starts is called the hypocenter, and the location directly above it on the surface of the earth is called the epicenter. Sometimes an earthquake has foreshocks. These are smaller earthquakes that happen in the same place as the larger earthquake that follows. Scientists can't tell that an earthquake is a foreshock until the larger earthquake happens. The largest, main earthquake is called the mainshock. Mainshocks always have aftershocks that follow. These are smaller earthquakes that occur afterwards in the same place as the mainshock. Depending on the size of the mainshock, aftershocks can continue for weeks, months, and even years after the mainshock!
please you people give answer
No.The magnitude is a measure of the total energy released by an earthquake.The intensity is a measure of the violence of ground shaking at a particular point. This is based on the statements of witnesses, damage to buildings and the ground acceleration as measured by a seismometer. As such it varies from place to place for a given earthquake.
The earthquakes after a major earthquake in the same area are called aftershocks.
I am looking for the same question
Not exactly, aftershocks are (as the name suggests) after the earthquake and their magnitude is only 1-2 on the scale (normally a lot less than the earthquake it self) :)
Aftershocks are smaller earthquakes that occur after a larger earthquake in the same area. They are a result of the earths crust near the fault rupture readjusting as a result of the main earthquake (also known as the "main shock").
Small quakes after a bigger one are commonly referred to as aftershocks.
because they only happen because they do
after shocks don't occur in the same place due to ex tonic faults occuring in the ground
I think you may be referring to aftershocks. Aftershocks are smaller tremors that can occur at any time for months after an earthquake as the pressure within Earth's crust is gradually released.
They are quite common; they are called aftershocks. An earthquake redistributes the stress that creates the quake across the fault line, which then creates new points of stress, which result in additional earthquakes, which further redistribute the stress again, and so on and so forth until all the energy is spent.
Aftershocks are smaller earthquakes that occur after a larger event (the mainshock) in the same area. If an even larger earthquake occurs, then the original mainshock becomes a foreshock and the bigger event becomes the mainshock.
Earthquakes can pressure highly stressed fault lines and trigger subsequent seismic events. If correct, so-called stress triggering theory could help scientists pinpoint areas where earthquakes are imminent. The earthquakes immediately following one earthquake are called aftershocks. Tectonic plates are moving all the time. The aftershocks can occur because the initial earthquake may have moved things into another position. Then the plates will make additional small adjustments (the aftershocks) to release new pressures that the initial earthquake caused between tectonic plates when they moved. The fault line between the plates may become less stable and then later an entirely new earthquake may occur at the same or at a close by site. It is the instability of the tectonic plates left after one earthquake that can cause others.
A strong earthquake may be followed by weaker, but still potentially dangerous earthquakes called aftershocks. Aftershocks may be potentially more dangerous than other earthquakes of the same intensity because some buildings may have been weakened during the main shock.