A normal fault is the result of the downward movement of rock along the fault line.
A reverse fault occurs when rock above the fault moves upward at the fault line. This type of fault is associated with compressional stress where the hanging wall moves up relative to the footwall. Reverse faults are common in regions undergoing compression, such as convergent plate boundaries.
In a lateral fault, the hanging wall moves horizontally in relation to the footwall. This type of fault occurs when the blocks of rock on either side of the fault move horizontally past each other. The hanging wall moves in the direction of the fault line, while the footwall remains relatively stationary.
Fault-block mountains are caused by normal faults, where blocks of the Earth's crust are tilted and uplifted along a fault line. As the hanging wall block moves downward relative to the footwall block, it creates a steep mountain range with a characteristic block-like appearance.
The San Andreas Fault is a strike-slip fault, where the movement occurs horizontally along the fault line. It is located in California and is formed by the movement between the Pacific Plate and the North American Plate.
This is a strike-slip fault.
A reverse fault occurs when rock above the fault moves upward at the fault line. This type of fault is associated with compressional stress where the hanging wall moves up relative to the footwall. Reverse faults are common in regions undergoing compression, such as convergent plate boundaries.
In a normal fault the hanging wall moves downward. With this type of fault, the hanging wall also shifts horizontally away from the fault line.
The hanging wall typically moves upward in a reverse fault or downward in a normal fault, due to the movement along the fault line causing one block to move relative to the other. This movement is a result of the stress and deformation within the Earth's crust.
these are the faults that occur in transmission line: 1. line to line fault 2. line to ground fault-this is the most common fault that occurs in tr. line(75%) 3. double line to ground fault 4. triple line to ground (or) 3 phase fault- this is the most serious and dangerous fault that occurs in transmission line.(but rarely occurs)
In a lateral fault, the hanging wall moves horizontally in relation to the footwall. This type of fault occurs when the blocks of rock on either side of the fault move horizontally past each other. The hanging wall moves in the direction of the fault line, while the footwall remains relatively stationary.
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A fault called a normal fault occurs when tectonic plates pull apart and tensional stress causes the rock layers to break and move along the fault line. In a normal fault, the hanging wall moves down relative to the footwall due to the extensional forces acting on the rocks.
Fault-block mountains are caused by normal faults, where blocks of the Earth's crust are tilted and uplifted along a fault line. As the hanging wall block moves downward relative to the footwall block, it creates a steep mountain range with a characteristic block-like appearance.
A strike-slip fault occurs when rocks along a fault line move horizontally past each other, with minimal vertical movement. In contrast, a normal fault is characterized by one block of rock moving downward relative to the other block due to tensional forces pulling them apart.
Fault line.