Normal faults are where the hanging wall drops in relation to the foot wall where as with the reverse fault the hanging wall is pushed higher over the foot wall.
Reverse failts are caused by compression. Normal faults however are formed by tension.
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 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.
Normal
Normal faults occur when the hanging wall moves down relative to the footwall due to extensional forces, while reverse faults occur when the hanging wall moves up relative to the footwall due to compressional forces. Normal faults are associated with divergent plate boundaries, while reverse faults are associated with convergent plate boundaries.
three kinds of faults are normal fault, reverse fault, and strike-slip fault.
Yes, normal and reverse faults are typically at an angle to the Earth's surface. Normal faults have a steep angle and occur in areas of extension, where the hanging wall drops down. Reverse faults have a gentler angle and occur in areas of compression, where the hanging wall moves up.
Faults are created when tectonic plates are stretching or compressing. There are two types of faults which are normal and reverse faults.
Reverse faultNormal faultStrike-slip fault
The three types of faults are Normal faults, Reverse faults, and Strike and Slip fault
Reverse and thrust faults are both under compressive stress.
normal reverse strike-slip