seismic waves
Energy is stored in the form of stress as tectonic plates move and become locked against each other. As the plates continue to move and the stress builds up, the stored energy increases until it reaches a point where the rocks break and release the energy in the form of seismic waves, causing an earthquake.
Energy is stored in rocks along faults as stress builds up from tectonic plate movements. This stress gradually deforms the rocks until they can no longer hold the energy, leading to a sudden release in the form of an earthquake.
The hypothesis that explains the release of energy during an earthquake is called the elastic rebound theory. According to this theory, stress builds up along a fault line until it exceeds the strength of the rocks, causing them to suddenly break and release accumulated energy in the form of seismic waves.
An earthquake is a violent disturbance in the Earth's crust.
The point within Earth where an earthquake begins is called the focus or hypocenter. This is usually located along a fault line, where stress in the Earth's crust causes a sudden release of energy in the form of seismic waves.
Energy is stored in the form of stress as tectonic plates move and become locked against each other. As the plates continue to move and the stress builds up, the stored energy increases until it reaches a point where the rocks break and release the energy in the form of seismic waves, causing an earthquake.
yes
A shift in the earth's crust to relieve pressure, and therefore release energy, is an earthquake.
An earthquake deep underground releases seismic energy in the form of seismic waves. These waves carry energy from the point of the earthquake's origin (the focus) and cause the ground to shake as they propagate through the Earth's crust.
False. An earthquake is a seismic wave caused by a sudden release of energy.
Energy is stored in rocks along faults as stress builds up from tectonic plate movements. This stress gradually deforms the rocks until they can no longer hold the energy, leading to a sudden release in the form of an earthquake.
The hypothesis that explains the release of energy during an earthquake is called the elastic rebound theory. According to this theory, stress builds up along a fault line until it exceeds the strength of the rocks, causing them to suddenly break and release accumulated energy in the form of seismic waves.
The point where rocks break and release stored energy is called the focus. This is the exact location within the Earth where an earthquake originates due to the sudden release of accumulated stress along a fault line. The energy released then radiates outwards in the form of seismic waves, causing the ground to shake during an earthquake.
The hypothesis that explains the release of energy during an earthquake is called the elastic rebound theory. This theory states that rocks on either side of a fault are deformed by tectonic stresses until they reach a breaking point. Once this breaking point is exceeded, energy is released in the form of seismic waves, causing an earthquake.
An earthquake is a violent disturbance in the Earth's crust.
When rocks break and tilt or slide down the break and move, energy is released in the form of seismic waves. Sometimes we feel this release as an earthquake. It is basically an earthquake, but it can also cause a tidal wave or even a tsunami.
The point within Earth where an earthquake begins is called the focus or hypocenter. This is usually located along a fault line, where stress in the Earth's crust causes a sudden release of energy in the form of seismic waves.