When rocks move in to each other. When two plates are constantly hitting each other, they form a convergent boundary, which forms a reverse fault. The Compression between these plates (or push) makes one slide above the other. If this happens continuously, one will be above the other, resting on it. This creates a hanging and foot wall.
This is called a reverse or thrust fault.
No, a fault-block is not typically created by two reverse faults. Reverse faults involve the upward movement of rock layers, and when two reverse faults occur in close proximity, they can create a complex structure but do not directly form a fault-block. Fault-blocks are more commonly associated with normal faults, where blocks of the Earth's crust are pulled apart, resulting in sections that drop down relative to others. In summary, while reverse faults can influence the landscape, they do not create fault-blocks in the same manner as normal faults do.
A reverse fault moves because it is under compression. The dip of a reverse fault is relatively steep, greater than 45-degrees.
Reverse
a reverse fault
no
A normal fault is the opposite of a reverse fault.
A reverse fault is formed here
A reverse fault
This is called a reverse or thrust fault.
Normal fault, i believe is true.
No, a fault-block is not typically created by two reverse faults. Reverse faults involve the upward movement of rock layers, and when two reverse faults occur in close proximity, they can create a complex structure but do not directly form a fault-block. Fault-blocks are more commonly associated with normal faults, where blocks of the Earth's crust are pulled apart, resulting in sections that drop down relative to others. In summary, while reverse faults can influence the landscape, they do not create fault-blocks in the same manner as normal faults do.
normal reverse strike-slip
Reverse Fault
three kinds of faults are normal fault, reverse fault, and strike-slip fault.
normal fault reverse fault slip strike fault
normal fault, reverse fault, strike-slip fault,