Reverse faults, in contrast, form in regions where the crust is being compressed. These compressional forces cause the hanging wall to move upward relative to the footwall.

Reverse faults, also called thrust faults, slide one block of crust on top of another. These faults are commonly found in collisions zones, where tectonic plates push up mountain ranges such as ...

Reverse faults are the opposite: plates push together, and the resting side is shoved up and over. There are other types and subtypes of faults represented around the world, ...

The second is a reverse fault, where plates pushing against each other build compressional stress. This forces one plate to rise overtop of the other and the area is shortened.

Thrust, or reverse, faults are features in the Earth’s crust that occur when a massive slab of rock moves up and over a lower block of rock, which moves deeper into the Earth, Aron explained.

The earthquake resulted from a geological phenomenon called a “reverse fault”. This occurs when tectonic plates collide, causing the Earth’s crust to thicken.