A growth fault is a type of normal fault that occurs in sedimentary basins, where the faulting process happens concurrently with sediment deposition. As sediments accumulate, the weight can lead to subsidence along the fault plane, creating a situation where the hanging wall moves downward relative to the footwall. This results in a fault that is actively forming and growing as new layers of sediment are deposited, often creating a characteristic wedge-shaped geometry. Growth faults are commonly associated with tectonic activity and can influence the structure and stratigraphy of the basin.
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.
The most common type of fault is a strike-slip fault, where two blocks of rock move horizontally past each other. This type of fault is often associated with transform plate boundaries, such as the San Andreas Fault in California.
The Hayward Fault is a Strike-slip Fault.
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a strike slip fault
It is a strike-slip fault.
The Hayward Fault is a Strike-slip Fault.
The Owens Valley fault is a normal fault
reverce fault.....
normal fault
Reverse Fault
Normal Fault
A strike-slip fault
Strike-slip faults are the most common fault type around the San Andreas Fault.