deforms
Elastic rebound. This phenomenon occurs when stress builds up in a rock mass and causes it to deform, then suddenly release that stress by rebounding to its original shape. Elastic rebound is often associated with earthquakes and fault movements.
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.
This phenomenon is known as elastic rebound. When rocks experiencing elastic deformation reach their limit, they release stored energy and snap back to their original shape, often causing an earthquake. This process is commonly observed along fault lines where tectonic plates meet.
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 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.
elastically
Elastic rebound. This phenomenon occurs when stress builds up in a rock mass and causes it to deform, then suddenly release that stress by rebounding to its original shape. Elastic rebound is often associated with earthquakes and fault movements.
Earthquakes will happen.
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 opposite of elastic is inelastic, where a material cannot stretch and rebound. A material without this quality could be "inflexible" (rigid, stiff) or one that did not rebound, termed "plastic" (deformable).Elastic suggests that the material recovers its original shape after an applied load is removed. Plastic means that it doesn't recover its shape. Steel is an example of an elasticmaterial, when it is loaded within its capacity. It becomes plastic if it is overloaded. Concrete can be considered an elastic material only in compression.
A stretched rubber band
Earthquakes will happen.
Inelastic things can not be stretched or do not rebound while elastic things will stretch, bounce, rebound, etc..
Elastic rebound
A stretched rubber band
This phenomenon is known as elastic rebound. When rocks experiencing elastic deformation reach their limit, they release stored energy and snap back to their original shape, often causing an earthquake. This process is commonly observed along fault lines where tectonic plates meet.
the rocks are deformed they break relasing the stored energy