A fault-block mountain forms where the edges of two plates come together to create a fault. When one plate pushes up over the other one, the upper one can continue up until it is high enough to create a fault-block mountain.
The Alpine Fault is a geological right-lateral strike-slip fault. It forms a transform boundary, so yes.
A lateral fault is when Shearing causes rock blocks to slide horizontally past each other.
A reverse fault forms when a hanging wall moves upward due to compressional forces. This type of fault occurs in areas where the crust is being pushed together, causing the hanging wall to move up and the footwall to move down.
A fault that forms as a result of shear stress is called a strike-slip fault. In this type of fault, the rocks on either side of the fault move horizontally past one another, typically along a vertical or near-vertical fault plane. Strike-slip faults are often associated with tectonic plate boundaries, such as transform boundaries, where lateral movement occurs. An example of a well-known strike-slip fault is the San Andreas Fault in California.
A reverse fault can create a landform known as a fault scarp, which is a steep slope or cliff that forms when one block of rock is thrust up and over another along the fault line. This can result in noticeable elevation changes in the landscape.
fault block
a normal fault
a reverse fault is formedmountains
The energy released by fault movement forms seismic waves.
Normal fault, i believe is true.
This is described as a normal fault.
A normal fault would form.
The Alpine Fault is a geological right-lateral strike-slip fault. It forms a transform boundary, so yes.
This is described as a normal fault.
fault
This is described as a normal fault.
A strike-slip fault