They will begin to deform plastically. That is the deformation will be permanent. Depending on the pressure and temperature conditions the rock will either continue to deform very slowly and "flow" (this occurs at great depth under high pressure and temperature conditions) or the rock will undergo brittle failure where fractures form - this occurs at shallow depths with low temperatures and low confining pressures.
The rock breaks
They will begin to deform plastically. That is the deformation will be permanent. Depending on the pressure and temperature conditions the rock will either continue to deform very slowly and "flow" (this occurs at great depth under high pressure and temperature conditions) or the rock will undergo brittle failure where fractures form - this occurs at shallow depths with low temperatures and low confining pressures.The rock breaks
Earthquakes will happen.
Earthquakes will happen.
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.
Yes it is called the elastic rock.
Elastic rebound
elastic change
the rocks are deformed they break relasing the stored energy
Some mechanisms that can release accumulated elastic energy in rocks include faulting, folding, landslides, and earthquakes. These processes can occur when the stress on rocks exceeds their strength, causing them to deform or fracture and release the stored energy.
elastic energy
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.
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.