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The elastic rebound theory was developed by Harry Fielding Reid, an American geophysicist who was studying the 1906 San Francisco earthquake.

He observed that points on the Earth's surface distant from the San Andreas fault had gradually moved prior to the earthquake whereas points on the surface directly on and around the fault had not.

During the earthquake the points next to the fault zone which had originally been static had suddenly shifted to match up with the points at a greater distance from the locked fault zone.

He concluded that this was due to the accumulation of elastic strain within the Earth's crust around the fault zone and that when the stress that caused this strain exceeded the strength of the rock mass or fault zone in the crust it suddenly ruptured. This caused the stored energy (termed elastic potential energy) to be released in one instant, causing an earthquake, and also meant that the rock mass around the fault zone that had originally been locked in position, snapped or rebounded to match the position of the rock mass at a greater distance from the fault. As such he coined the term "elastic rebound" to describe this phenomenon.

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8y ago
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11y ago

When the rocks break or move, a fault is produced. As the rocks break energy is released in the form of waves this causes the crust of the Earth to actually shake This explanation of how earthquakes occur is known as the elastic rebound theory

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9y ago

The Elastic rebound theory is the explanation for how energy is spread during earthquakes. As rocks are forced to shift by faults, they accumulate energy until they are forced to slowly deform.

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13y ago

the sudden return of elastically deformed rock to its original shape

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13y ago

The explanation starting that when rocks are deformed, they break, releasing the stored energy that results in the vibrations of an earthquake.

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11y ago

caca

response: yeah right

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11y ago

harry reid

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Q: Can you briefly describe the elastic rebound theory of earthquake?
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Related questions

The hypothesis that explains the release of energy during an earthquake is the?

elastic rebound theory


The mechanism by which rocks store and eventually release energy in the form of an earthquake is?

The answer is C: Elastic Rebound a fault displacement b stress fracture c elastic rebound or seismic rebound one of those


What is the hypothesis that explains the release of energy during an earthquake is called?

elastic rebound hypothesis


The hypothesis that explains the release of energy during an earthquake is called the.?

elastic rebound theory


The hypothesis that explains the release of energy during an earthquake is called the?

elastic rebound theory


What builds stress up and helps release that stress during an earthquake?

the elastic rebound theory


What scientific discoveries were made from the 1906 San Francisco Earthquake?

The elastic-rebound theory was found from the 1906 San Francisco earthquake


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 is the definition for the word earthquake?

An Earthquake is a series of vibrations induced in the earth's crust by the abrupt rupture and rebound of rocks in which elastic strain has been slowly accumulating.


elastic rebound?

the tendency for the deformed rock along a fault to spring back after an earthquake


The elastic rebound theory for the origin of earthquakes was first proposed by?

H. Reid, following after the 1906 San Francisco earthquake


What are the 4 stages of elastic rebound hypothesis?

1) zero stress on elastic material/it's at original position 2) stress is applied/deformation occurs 3) release of energy (earthquake) 4) elastic material rebounds