Not sure about the 'sudden' part, but it's called rebound.
Really its called Elastic Rebound.....
The sudden return of elastically deformed rock to its original shape may indicate the occurrence of an earthquake or other tectonic activity that released accumulated stress within the rock. This phenomenon is commonly observed in regions with high seismic activity, where rocks experience deformation due to the build-up of strain energy before ultimately rebounding to their undeformed state when stress is released.
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.
Silicon is generally considered to be inelastic, meaning it does not easily return to its original shape after being deformed. However, silicon can exhibit some elastic properties depending on its structure and how it is processed.
A stress-strain curve typically has two segments because the material first deforms elastically before transitioning to plastic deformation. The initial linear region represents elastic deformation, where the material can return to its original shape after the stress is removed. The second region shows plastic deformation, where the material undergoes permanent deformation due to interatomic sliding or dislocation motion.
The processes that return carbon to the atmosphere include respiration by animals, decomposition of organic matter, and combustion of fossil fuels.
No
The sudden return of elastically deformed rock to its original shape may indicate the occurrence of an earthquake or other tectonic activity that released accumulated stress within the rock. This phenomenon is commonly observed in regions with high seismic activity, where rocks experience deformation due to the build-up of strain energy before ultimately rebounding to their undeformed state when stress is released.
This phenomenon is known as elastic rebound and it occurs when a rock that has been subject to stress suddenly releases that stress, causing it to return to its original shape. This can happen during an earthquake when built-up strain in the rock is released, leading to rapid deformation and rebound.
The "elastic portion" is precisely the part where the material returns to its original shape, and thus returns its energy. Once the material does NOT return to its previous shape, it doesn't exert a force back to the original position, and there is no way to get the energy back.
elastic change
The sudden return of an elastically-deformed rock to its original shape when a load is removed or a stress released. This often occurs in earthquakes, as rocks either side of a slip fault, which have been stressed by friction along the fault plane, overcome static friction and rapidly rebound. Elastic rebound must not be confused with isostatic rebound, which is a much slower process in which mantle material flows under pressure into areas under the crust where large loads such as oceans or ice sheets have been removed, thus forcing the crust to rise where the load has been removed and fall elsewhere. Because of the large scales involved and extremely high viscosity of the mantle material, isostatic rebound very slow. The ground surface in the area of Scandinavia is still rebounding at a measurable rate (about 10mm per year) as a result of the melting of the Weichsel ice sheet ten thousand years ago.
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.
Elasticity describes the ability of a solid to return to its original shape after being deformed or stretched.
Most materials are elastic - or behave elastically - at least a little bit. This means that when you apply forces to them to deform them, they return to their original size and shape after the deforming forces are removed.
elastic
The linear portion of the stress-strain curve represents the elastic deformation of a material. This is where the material behaves elastically and will return to its original shape once the applied stress is removed.
No, elasticity is the ability of a material to return to its original shape after being stretched or deformed. If a substance is unable to stretch, it would lack elasticity.