the energy is stored before the earthquake in the exinstle manner of the earthquake. The exinstile manner is below the earthquake where the rumble happens.
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 release of stored energy in Earth's outer layer that causes movements is called an earthquake. This release of energy typically occurs along fault lines where tectonic plates are in contact with each other and can result in vibrations felt on the Earth's surface.
The stored energy is released during an earthquake when accumulated stresses in the Earth's crust exceed the strength of the rocks, causing the rocks to break along a fault. This sudden release of energy generates seismic waves that radiate outward from the fault, causing the ground to shake.
It depends! Depending upon the built-in energy at the epicenter before and after the earthquake (main shock), and/or the energy (especially stored at some weaker places) generated after the earthquake, aftershocks of an earthquake range in their time.For more details, refer: http://www.answers.com/library/Wikipedia-cid-1349 Aftershock
The term you are looking for is "elastic rebound." This process occurs when rocks accumulate stress and deform, eventually reaching their breaking point and releasing the stored energy in the form of seismic waves, resulting in an earthquake.
The energy of an earthquake is stored as elastic strain energy in the Earth's crust along the fault line prior to the earthquake. This energy is released when the stress on the fault exceeds the strength of the rocks, causing them to break and the energy to be radiated as seismic waves.
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.
Energy is stored in rocks adjacent to the site of a future earthquake as elastic potential energy due to the stress and strain built up in the rocks. This stored energy is released suddenly when the rocks undergo sudden movement along a fault line, resulting in an earthquake.
Potential energy is the energy stored in a rock before its fall from a hill.
earthquake
Elastic potential energy stored in the rock is released in the form of vibrations and heat.
The energy in an earthquake is primarily released as seismic waves, which are a combination of kinetic and potential energy. As tectonic plates undergo stress and strain, they accumulate potential energy in the form of stored elastic energy. When this energy is suddenly released, it transforms into kinetic energy, causing the ground to shake.
The concentration of energy before it is transferred can vary depending on the system. In a closed system, the energy is typically stored and transferred as potential or kinetic energy. For example, in a battery, energy is stored as chemical potential energy before being transferred as electrical energy.
The release of stored energy in Earth's outer layer that causes movements is called an earthquake. This release of energy typically occurs along fault lines where tectonic plates are in contact with each other and can result in vibrations felt on the Earth's surface.
the rocks are deformed they break relasing the stored energy
Binding energy. and some is even stored in particles, such as the neutron which has a half-life of about ten minutes before it disintegrates with the release of energy.
The stored energy is released during an earthquake when accumulated stresses in the Earth's crust exceed the strength of the rocks, causing the rocks to break along a fault. This sudden release of energy generates seismic waves that radiate outward from the fault, causing the ground to shake.