The elastic-rebound theory of faulting through a sketched map and the way it has been modified in recent years.

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Answer 1

Question

Chapter 5, Problem 1QR

To determine

The elastic-rebound theory of faulting through a sketched map and the way it has been modified in recent years.

Expert Solution & Answer

Answer to Problem 1QR

The elastic-rebound theory explains movement of faults by the rupture in rock through overpowering stress caused by Earth. The modification in this theory suggests that a considerable time is required to create another earthquake after a big earthquake.

Explanation of Solution

Pictorial representation: Fig.1 shows the elastic-rebound theory where (a) represents an active fault with a road, (b) represents occurrence of deformation along the fault, and (c) represents the final occurrence of deformation.

EBK NATURAL DISASTERS, Chapter 5, Problem 1QR

Fig.1 Schematic representation of elastic-rebound theory

After the San Francisco earthquake, the elastic-rebound theory was developed to explain movement of faults. According to seismic studies from San Andreas faults, the stress of Earth causes deformation and movement around both sides of a fault. However, rocks do not move due to this stress along the fault because of their roughness and irregularity. It results in the retardation of the movement of rocks with friction by making strong interlocking bonds. The land masses that are far from faults continue to move. The overpowering stress causes rupture in rocks at fault and both sides of fault move forward to catch or pass the rock which is away from fault. After this movement of fault, complete elastic strain is removed and new one is build up.

The former elastic bound theory still works but some modifications have emerged in recent years. These modifications suggest that most of the elastic strain is removed from the rocks after a large earthquake. A considerable time is needed to build a strain high enough to create another big earthquake.

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Answer 2

Question

Chapter 5, Problem 1QR

To determine

The elastic-rebound theory of faulting through a sketched map and the way it has been modified in recent years.

Expert Solution & Answer

Answer to Problem 1QR

The elastic-rebound theory explains movement of faults by the rupture in rock through overpowering stress caused by Earth. The modification in this theory suggests that a considerable time is required to create another earthquake after a big earthquake.

Explanation of Solution

Pictorial representation: Fig.1 shows the elastic-rebound theory where (a) represents an active fault with a road, (b) represents occurrence of deformation along the fault, and (c) represents the final occurrence of deformation.

EBK NATURAL DISASTERS, Chapter 5, Problem 1QR

Fig.1 Schematic representation of elastic-rebound theory

After the San Francisco earthquake, the elastic-rebound theory was developed to explain movement of faults. According to seismic studies from San Andreas faults, the stress of Earth causes deformation and movement around both sides of a fault. However, rocks do not move due to this stress along the fault because of their roughness and irregularity. It results in the retardation of the movement of rocks with friction by making strong interlocking bonds. The land masses that are far from faults continue to move. The overpowering stress causes rupture in rocks at fault and both sides of fault move forward to catch or pass the rock which is away from fault. After this movement of fault, complete elastic strain is removed and new one is build up.

The former elastic bound theory still works but some modifications have emerged in recent years. These modifications suggest that most of the elastic strain is removed from the rocks after a large earthquake. A considerable time is needed to build a strain high enough to create another big earthquake.

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Answer 3

Question

Chapter 5, Problem 1QR

To determine

The elastic-rebound theory of faulting through a sketched map and the way it has been modified in recent years.

Expert Solution & Answer

Answer to Problem 1QR

The elastic-rebound theory explains movement of faults by the rupture in rock through overpowering stress caused by Earth. The modification in this theory suggests that a considerable time is required to create another earthquake after a big earthquake.

Explanation of Solution

Pictorial representation: Fig.1 shows the elastic-rebound theory where (a) represents an active fault with a road, (b) represents occurrence of deformation along the fault, and (c) represents the final occurrence of deformation.

EBK NATURAL DISASTERS, Chapter 5, Problem 1QR

Fig.1 Schematic representation of elastic-rebound theory

After the San Francisco earthquake, the elastic-rebound theory was developed to explain movement of faults. According to seismic studies from San Andreas faults, the stress of Earth causes deformation and movement around both sides of a fault. However, rocks do not move due to this stress along the fault because of their roughness and irregularity. It results in the retardation of the movement of rocks with friction by making strong interlocking bonds. The land masses that are far from faults continue to move. The overpowering stress causes rupture in rocks at fault and both sides of fault move forward to catch or pass the rock which is away from fault. After this movement of fault, complete elastic strain is removed and new one is build up.

The former elastic bound theory still works but some modifications have emerged in recent years. These modifications suggest that most of the elastic strain is removed from the rocks after a large earthquake. A considerable time is needed to build a strain high enough to create another big earthquake.

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Subscribe now to access step-by-step solutions to millions of textbook problems written by subject matter experts!

Answer 4

Question

Chapter 5, Problem 1QR

To determine

The elastic-rebound theory of faulting through a sketched map and the way it has been modified in recent years.

Expert Solution & Answer

Answer to Problem 1QR

The elastic-rebound theory explains movement of faults by the rupture in rock through overpowering stress caused by Earth. The modification in this theory suggests that a considerable time is required to create another earthquake after a big earthquake.

Explanation of Solution

Pictorial representation: Fig.1 shows the elastic-rebound theory where (a) represents an active fault with a road, (b) represents occurrence of deformation along the fault, and (c) represents the final occurrence of deformation.

EBK NATURAL DISASTERS, Chapter 5, Problem 1QR

Fig.1 Schematic representation of elastic-rebound theory

After the San Francisco earthquake, the elastic-rebound theory was developed to explain movement of faults. According to seismic studies from San Andreas faults, the stress of Earth causes deformation and movement around both sides of a fault. However, rocks do not move due to this stress along the fault because of their roughness and irregularity. It results in the retardation of the movement of rocks with friction by making strong interlocking bonds. The land masses that are far from faults continue to move. The overpowering stress causes rupture in rocks at fault and both sides of fault move forward to catch or pass the rock which is away from fault. After this movement of fault, complete elastic strain is removed and new one is build up.

The former elastic bound theory still works but some modifications have emerged in recent years. These modifications suggest that most of the elastic strain is removed from the rocks after a large earthquake. A considerable time is needed to build a strain high enough to create another big earthquake.

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Subscribe now to access step-by-step solutions to millions of textbook problems written by subject matter experts!

Answer 5

Chapter 5, Problem 1QR

To determine

The elastic-rebound theory of faulting through a sketched map and the way it has been modified in recent years.

Expert Solution & Answer

Answer to Problem 1QR

The elastic-rebound theory explains movement of faults by the rupture in rock through overpowering stress caused by Earth. The modification in this theory suggests that a considerable time is required to create another earthquake after a big earthquake.

Explanation of Solution

Pictorial representation: Fig.1 shows the elastic-rebound theory where (a) represents an active fault with a road, (b) represents occurrence of deformation along the fault, and (c) represents the final occurrence of deformation.

EBK NATURAL DISASTERS, Chapter 5, Problem 1QR

Fig.1 Schematic representation of elastic-rebound theory

After the San Francisco earthquake, the elastic-rebound theory was developed to explain movement of faults. According to seismic studies from San Andreas faults, the stress of Earth causes deformation and movement around both sides of a fault. However, rocks do not move due to this stress along the fault because of their roughness and irregularity. It results in the retardation of the movement of rocks with friction by making strong interlocking bonds. The land masses that are far from faults continue to move. The overpowering stress causes rupture in rocks at fault and both sides of fault move forward to catch or pass the rock which is away from fault. After this movement of fault, complete elastic strain is removed and new one is build up.

The former elastic bound theory still works but some modifications have emerged in recent years. These modifications suggest that most of the elastic strain is removed from the rocks after a large earthquake. A considerable time is needed to build a strain high enough to create another big earthquake.

Answer 6

Chapter 5, Problem 1QR

To determine

The elastic-rebound theory of faulting through a sketched map and the way it has been modified in recent years.

Expert Solution & Answer

Answer to Problem 1QR

The elastic-rebound theory explains movement of faults by the rupture in rock through overpowering stress caused by Earth. The modification in this theory suggests that a considerable time is required to create another earthquake after a big earthquake.

Explanation of Solution

Pictorial representation: Fig.1 shows the elastic-rebound theory where (a) represents an active fault with a road, (b) represents occurrence of deformation along the fault, and (c) represents the final occurrence of deformation.

EBK NATURAL DISASTERS, Chapter 5, Problem 1QR

Fig.1 Schematic representation of elastic-rebound theory

After the San Francisco earthquake, the elastic-rebound theory was developed to explain movement of faults. According to seismic studies from San Andreas faults, the stress of Earth causes deformation and movement around both sides of a fault. However, rocks do not move due to this stress along the fault because of their roughness and irregularity. It results in the retardation of the movement of rocks with friction by making strong interlocking bonds. The land masses that are far from faults continue to move. The overpowering stress causes rupture in rocks at fault and both sides of fault move forward to catch or pass the rock which is away from fault. After this movement of fault, complete elastic strain is removed and new one is build up.

The former elastic bound theory still works but some modifications have emerged in recent years. These modifications suggest that most of the elastic strain is removed from the rocks after a large earthquake. A considerable time is needed to build a strain high enough to create another big earthquake.

Answer 7

Chapter 5, Problem 1QR

To determine

The elastic-rebound theory of faulting through a sketched map and the way it has been modified in recent years.

Answer 8

Expert Solution & Answer

Answer to Problem 1QR

The elastic-rebound theory explains movement of faults by the rupture in rock through overpowering stress caused by Earth. The modification in this theory suggests that a considerable time is required to create another earthquake after a big earthquake.

Answer 9

Expert Solution & Answer

Answer 10

Expert Solution & Answer

Answer 11

Explanation of Solution

Pictorial representation: Fig.1 shows the elastic-rebound theory where (a) represents an active fault with a road, (b) represents occurrence of deformation along the fault, and (c) represents the final occurrence of deformation.

EBK NATURAL DISASTERS, Chapter 5, Problem 1QR

Fig.1 Schematic representation of elastic-rebound theory

After the San Francisco earthquake, the elastic-rebound theory was developed to explain movement of faults. According to seismic studies from San Andreas faults, the stress of Earth causes deformation and movement around both sides of a fault. However, rocks do not move due to this stress along the fault because of their roughness and irregularity. It results in the retardation of the movement of rocks with friction by making strong interlocking bonds. The land masses that are far from faults continue to move. The overpowering stress causes rupture in rocks at fault and both sides of fault move forward to catch or pass the rock which is away from fault. After this movement of fault, complete elastic strain is removed and new one is build up.

The former elastic bound theory still works but some modifications have emerged in recent years. These modifications suggest that most of the elastic strain is removed from the rocks after a large earthquake. A considerable time is needed to build a strain high enough to create another big earthquake.

Answer 12

Ch. 5 - Prob. 1QR Ch. 5 - Prob. 2QR Ch. 5 - Prob. 3QR Ch. 5 - Prob. 4QR Ch. 5 - Prob. 5QR Ch. 5 - Prob. 6QR Ch. 5 - Prob. 7QR Ch. 5 - Prob. 8QR Ch. 5 - Prob. 9QR Ch. 5 - Prob. 10QR

The elastic-rebound theory of faulting through a sketched map and the way it has been modified in recent years.

The elastic-rebound theory of faulting through a sketched map and the way it has been modified in recent years.

Answer to Problem 1QR

Explanation of Solution

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