anything that stretches or compresses can store elastic energy.
most common example is a coil spring. It has an equilibrium position, and you must do work (add energy) on it to move it from that position. That energy input is stored in the form of 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.
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.
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.
there is actually no non examples of geothermal
Most earthquakes are caused by the rapid release of elastic strain energy stored in rock that has been subjected to great forces. This energy is released in the form of seismic waves that propagate through the Earth's crust, causing the ground to shake.
Some non-examples of elastic potential energy include gravitational potential energy, kinetic energy, and thermal energy. These types of energy are different from elastic potential energy as they are not associated with the deformation or stretching of an elastic material.
catapault elastic band hairband
Examples of elastic energy include a stretched rubber band, a compressed spring, a bent bow, and a balloon that is inflated. These objects store potential energy as a result of their deformation or stretching, which can be released to do work when the object returns to its original shape.
A stretched rubber band has elastic potential energy. Water stored behind a dam has gravitational potential energy. A compressed spring in a toy car has elastic potential energy. A book placed on a shelf has gravitational potential energy.
In stretched elastic, the primary forms of energy present are elastic potential energy, which is the energy stored in the elastic material due to its deformation, and kinetic energy, if the elastic material is moving.
Elastic energy is the energy stored in an object when it is compressed, stretched, or deformed. It is a form of potential energy that can be released when the object returns to its original shape. Examples include a stretched rubber band or a compressed spring.
Examples of super elastic collisions include collisions between two superballs or collisions between an electron and a positron. In these collisions, kinetic energy is increased after the collision due to the conservation of momentum and conservation of kinetic energy principles.
The energy stored in a stretched elastic is potential energy, specifically elastic potential energy. When the elastic is stretched, work is done to stretch it, and this work is stored as potential energy in the elastic material.
Elastic energy, for example, a stretched spring.
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Stretching a rubber band or spring stores elastic potential energy that can be released when the band or spring snaps back to its original shape. Compressing a tennis ball or squeezing a stress ball stores elastic potential energy that can be released when the ball returns to its original shape.
A joule is simply a unit to measure energy. Examples of energy include gravitational potential energy, kinetic energy, sound energy, light energy, elastic energy, nuclear energy.