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Sudden return of elastically deformed rock to its unformed shape?
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.
When does an elastic rebound happen?
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.
What word type is sudden?
The word 'sudden' is an adjective, a word that describes a noun as happening or done quickly and unexpectedly or without warning. Example:A sudden storm ended our picnic quickly.Note: The word 'sudden' functions as a noun in the expression, 'all of a sudden', as the object of the preposition 'of'.
What type of word is sudden?
The word 'sudden' is an adjective, a word that describes a noun as happening or done quickly and unexpectedly or without warning. Example:A sudden storm ended our picnic quickly.Note: The word 'sudden' functions as a noun in the expression, 'all of a sudden', as the object of the preposition 'of'.
What is sudden storm?
When the CMEs impact the Earth's magnetosphere, a storm sudden commencement or sudden impulse (SSC or SI), a sudden increase in the magnetic field strength detected at the surface, almost instantaneously occurs.
Sudden return of elastically deformed rock to an undeformed shape?
No
Sudden return of elastically deformed rock?
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.
Sudden return of elastically deformed rock to its undeformed shape?
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.
Sudden return of elastically deformed rock to its unformed shape?
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.
When does an elastic rebound happen?
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.
How does the elastic rebound theory explain the occurrence of earthquakes?
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.
What happens to someone with periodic paralysis?
A person with periodic paralysis experiences sudden onset of weakness, which gradually subsides, only to return again later.
Why does you body temperature drop during flu?
Body temperature drops when someone has gotten swine flu. The virus causes a spike in fever and a sudden drop -hypothermia - which results in chills. The sudden drop requires outside measures to return the body temperature to rise to normal.
What is the medical term for return of disease symptoms?
Relapse is the medical term meaning the return of symptoms of disease. For instance, some people with multiple sclerosis have a relapsing/remitting pattern of disease, with periods of symptoms interspersed with periods of no symptoms.
Is sudden a noun?
No, the word 'sudden' is not a noun; sudden is an adjective, a word that describes a noun (a sudden storm).The noun form for the adjective sudden is suddenness.
Is sudden a verb?
Sudden is an adjective, not a verb.
In the process of elastic rebound as a rock becomes stressed it first?
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.
