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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.
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The springing back of rock after it has been deformed is known as?
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.
Who was the first to explain the actual mechanism by which earthquakes are generated?
The first to explain the actual mechanism by which earthquakes are generated was the British geologist John Milne. In the late 19th century, he proposed the theory of elastic rebound, which suggests that tectonic stress slowly builds up in rocks until it exceeds their strength, causing them to break and suddenly release energy in the form of seismic waves.
What theory explains the occurrence of earthquakes?
The theory that explains the occurrence of earthquakes is called plate tectonics. It states that the Earth's outer shell is divided into several large plates that are constantly moving, causing stress to build up along their boundaries. When this stress is released, it results in the shaking of the ground known as an earthquake.
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.
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.
What can happen when rocks pass their elastic limit break and snap in elastic rebound?
Earthquakes will happen.
What can happen when rocks pass their elastic limit breaks and snap back in elastic rebound?
Earthquakes will happen.
The springing back of rock after it has been deformed is known as?
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.
What has the author Harry Fielding Reid written?
Harry Fielding Reid has written: 'The elastic-rebound theory of earthquakes' -- subject(s): Earthquakes
What is a synonym for elastic rebound?
elastically
Who was the first to explain the actual mechanism by which earthquakes are generated?
The first to explain the actual mechanism by which earthquakes are generated was the British geologist John Milne. In the late 19th century, he proposed the theory of elastic rebound, which suggests that tectonic stress slowly builds up in rocks until it exceeds their strength, causing them to break and suddenly release energy in the form of seismic waves.
The elastic rebound theory for the origin of earthquakes was first proposed by?
The elastic rebound theory for the origin of earthquakes was first proposed by American geologist Harry Fielding Reid in 1910. This theory states that tectonic stress builds up along faults until it exceeds the strength of the rocks, causing them to suddenly break and release energy in the form of an earthquake.
What theory explains the occurrence of earthquakes?
The theory that explains the occurrence of earthquakes is called plate tectonics. It states that the Earth's outer shell is divided into several large plates that are constantly moving, causing stress to build up along their boundaries. When this stress is released, it results in the shaking of the ground known as an earthquake.
Elastic rebound is similar to what happens when you?
A stretched rubber band
What is elasticity and in-elasticity?
Inelastic things can not be stretched or do not rebound while elastic things will stretch, bounce, rebound, etc..
Why does land separate?
There is a theory called plate tetonics, which is basically that the earth has many different plates that sometimes move. When they move, they take the land above them with them. The elastic rebound theory is one of the reasons for earthquakes.
What is the snapping back of deformed rocks to its previous shape?
Elastic rebound
