they release energy because its like a rubber band being stretched then being released
Think of it as a rubber band
not exacltly
The elastic rebound theory explains how energy is stored in rocks as they deform under stress until they reach a breaking point. When the rocks finally fracture along a fault line, the accumulated energy is released suddenly, causing the rocks to snap back to their original shape. This rapid release of energy generates seismic waves that propagate through the Earth, leading to the shaking felt during an earthquake. Thus, the elastic rebound process is key to the transfer of energy that produces seismic activity.
they release energy because its like a rubber band being stretched then being released Think of it as a rubber band not exacltly
they release energy because its like a rubber band being stretched then being released Think of it as a rubber band not exacltly
the rocks are deformed they break relasing the stored energy
elastic rebound theory
The sudden return of elastically deformed rock to sit original shape is called elastic rebound. Elastic rebound happens when stress on rock along a fault becomes so grat that the rock breaks or fails. This failure causes the rocks on either side of the fault to jerk past one another. During this sudden motion, large amounts of energy are released. This energy travels through rock as seismic waves. These waves cause earthquakes. The strength of an earthquake is related to the amount of energy that is released during elastic rebound.
elastic rebound theory
elastically
The four stages of the elastic rebound hypothesis are: (1) rocks on either side of a fault are deformed by stress, (2) stress overcomes friction causing rocks to break and shift, (3) stored elastic energy is released as the rocks rebound to their original shape, and (4) seismic waves are generated causing an earthquake.
In the process of elastic rebound, as a rock becomes stressed it first deforms elastically, storing energy in the form of strain in the rock. Once the stress exceeds the rock's strength, it suddenly breaks and releases the stored elastic energy, causing an earthquake. This sudden release of energy results in the rock snapping back to its original shape, causing the ground to shake.
Elastic collision transfers more energy into motion while inelastic transfers energy into deformation of the objects. Elastic could be called more efficient transfer.
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.