convergent plate motion
Normal is always on the ocean border and reverse is always not in an ocean border
dip-slip faults
Reverse and thrust faults are both under compressive stress.
Normal faults, reverse faults, and last but not least transform faults.
Thrust faults and reverse faults are essentially the same, the only difference being the angle: thrust faults have a shallow angle of 45 degrees or less from horizontal. Reverse (thrust) faults and folds usually indicate rock being compressed. In many cases folds develop along reverse faults as one fault block is dragged along another, with an anticline forming in the hanging wall.
Landforms created at reverse faults include mountain ranges and volcanoes. Reverse faults occur at convergent boundaries and the type of convergent boundary determines the landform created.
Faults are created when tectonic plates are stretching or compressing. There are two types of faults which are normal and reverse faults.
no
reverse fault
Rocks moving apart can cause normal faults to form, as opposed to reverse and strike-slip faults.
reverse faults move from compression when the hanging wall moves up
compression
Normal is always on the ocean border and reverse is always not in an ocean border
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.
dip-slip faults
The two types of faults that can result in mountains are reverse faults and normal faults.
Reverse failts are caused by compression. Normal faults however are formed by tension.