the force is compression
Reverse faults are created by compressional forces, which occur when tectonic plates move toward each other. This compression causes the hanging wall block to be pushed up relative to the footwall block. These types of faults are typically found in regions experiencing significant tectonic stress, such as convergent plate boundaries. The resulting geological features often include mountain ranges and folded rock layers.
a. Transform:transform boundaries or motion creates strike-slip faults.b. Convergent:convergent boundaries or motion creates reverse faults.c. Divergent:divergent motion creates a normal fault.
the best answer is reverse boundary
Faults are created when tectonic plates are stretching or compressing. There are two types of faults which are normal and reverse faults.
The three types of faults are normal, reverse, and strike-slip faults. Normal faults are associated with divergent plate boundaries, reverse faults with convergent plate boundaries, and strike-slip faults with transform plate boundaries.
compression
reverse fault
a. Transform:transform boundaries or motion creates strike-slip faults.b. Convergent:convergent boundaries or motion creates reverse faults.c. Divergent:divergent motion creates a normal fault.
Reverse and thrust faults are both under compressive stress.
reverse faults move from compression when the hanging wall moves up
compression
The three major types of faults are normal faults, reverse faults, and strike-slip faults. Synclines are not faults but rather geological structures that describe the folding of rock layers.
The main direction of the stress on blocks of rock at normal faults, reverse faults and the strike slip faults usually happens at the weak areas.
the best answer is reverse boundary
Reverse failts are caused by compression. Normal faults however are formed by tension.
Faults are created when tectonic plates are stretching or compressing. There are two types of faults which are normal and reverse faults.
The three types of faults are normal, reverse, and strike-slip faults. Normal faults are associated with divergent plate boundaries, reverse faults with convergent plate boundaries, and strike-slip faults with transform plate boundaries.