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A fault that occurs on folded rock layers is likely to be a thrust fault, where one block of rock is pushed up and over the other. This type of fault is common in areas where horizontal compression forces have folded the rock layers.
It is a strike-slip fault.
Normal Fault
Strike-slip faults are the most common fault type around the San Andreas Fault.
The fault type is a normal fault, called the Spirit Lake Fault, and it runs approximately 9 miles to the north of Mount St. Helens.
If a fault occurs in an area where rock layers have been folded, it is likely to be a reverse fault. Reverse faults are characterized by compressional stress, causing the rocks to move upward and over each other.
A: raid 0raid 0 is no fault tolerance...coz it writes the data parallely and it doesnot contain any mirror in that.
Faults are distinguished based on the type of movement that occurs along them. For example, a normal fault is caused by extensional stress, where the hanging wall moves down relative to the footwall. In contrast, a reverse fault is caused by compressional stress, where the hanging wall moves up relative to the footwall. Strike-slip faults involve horizontal movement along the fault plane.
The Hayward Fault is a Strike-slip Fault.
A fault that occurs on folded rock layers is likely to be a thrust fault, where one block of rock is pushed up and over the other. This type of fault is common in areas where horizontal compression forces have folded the rock layers.
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It is a strike-slip fault.
a strike slip fault
Probably reverse fault because folding is the result of compressional stres and reverse faults are caused by compression
The Hayward Fault is a Strike-slip Fault.
The Owens Valley fault is a normal fault
Reverse Fault