When the stress within the rock mass exceeds the elastic limit, then either a slip will occur along a pre-existing fault to releases the accumulated strain energy. This release of energy is more commonly known as an earthquake!
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.
At collision zones, tectonic plates converge and interact in different ways. This can result in the creation of mountain ranges, earthquakes, and the subduction of one plate beneath another. The intense pressure and friction at collision zones lead to the deformation and uplift of the Earth's crust.
Folds indicate that deformation has occurred because they are curved or wavy layers of rock that form due to the application of stress and pressure over time. These folds are most commonly found in sedimentary rocks, and they provide evidence of the tectonic forces that have shaped the Earth's crust. By studying the orientation and shape of folds, geologists can better understand the history of mountain building and other geologic processes.
Rocks along a fault line can break and shift due to tectonic forces, causing movements such as sliding past each other or being compressed together. The friction and pressure along the fault line can lead to earthquakes when the accumulated stress is released suddenly. Over time, the rocks along a fault line can also undergo deformation, such as folding and faulting.
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.
When the stress and strain along tectonic plates reach the breaking point, it can result in an earthquake. This is when the stored elastic energy is released as seismic waves, causing the rocks on either side of the fault to move, releasing the built-up stress.
Elastic deformation occurs when an opposing force is applied to the drug after particle rearrangement (i.e. the initial repacking of the particles). If the force is released before the yield point is reached, the particles of the drug will return to their original shape. However, if the force goes beyond the yield point, the powder will undergo plastic deformation or brittle fracture.
When an object reaches its elastic limit, it loses its ability to return to its original shape after deformation and becomes permanently deformed. This means that even when the force is removed, the object will retain its new shape.
Elastic deformation returns to it's original shape after a strain is applied. Plastic deformation returns to a deformed shape after a strain is applied. The material's molecular bonds are strained to the point of fracture, making it not possible to return to the same state. Elastic deformation will return to its original shape. Plastic deformation is when you alter the original form. To understand more on this subject you might investigate failure analysis literature. Lots of good stuff there ratchet marks, beach marks, reverse bending etc... I believe the U.S. metallurgical society has the best reference material on this subject. A temporary shape change that is self-reversing after the force is removed, so that the object returns to its original shape, is called elastic deformation. In other words, elastic deformation is a change in shape of a material at low stress that is recoverable after the stress is removed. Examples would be the loading of a bridge or building support beam where the loads remain within the original design parameters, or the use of a safety pin where when it is opened it returns to it's unloaded shape. When the stress is sufficient to permanently deform the metal, it is called plastic deformation. Examples would be the building support beams for the twin towers, where the heat generated by the fires decreased the strength of the steel and allowed it to deform plastically, or the loads that are applied to a section of electrical conduit or mechanical piping in order to bend them into a specific shape. in elastic def. , the material returns to its original shape once force is removed. in plastic, the deformation is permanent and the material doesn't return to its original shape the elastic deformation happens in yield point and elastic deformation back to original size but plastic deformation will not back tto original size.
When you stretch a spring, it stores potential energy in the form of elastic potential energy. The spring will exert a restoring force trying to return to its original shape. The amount of force required to stretch the spring is directly proportional to the amount of deformation.
An Earthquake happens.
the tire will bounce
Weight causes the elastic material to stretch. The material may be stretched beyond its elastic limit. If this happens, then the material rips or tears, or it does not return to its original size.
When Demand is perfectly elastic, Marginal Revenue is identical with price.
When tectonic plates collide with oceanic plates, the denser oceanic plate is usually forced beneath the less dense continental plate in a process called subduction. This can lead to the formation of volcanic arcs and deep ocean trenches. The collision can also cause earthquakes and crustal deformation.
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Braking reduces speed.