Footwall Hanging Wall Reverse Fault

The hanging wall slides down relative to the footwall.

Footwall hanging wall reverse fault.

But that is when the foot wall moves down the hanging wall moves up. But that is when the foot wall moves down the hanging wall moves up. Reverse faults indicate compressive shortening of the crust. A fault plane is a relatively flat surface where rocks break due to displacement.

In a reverse fault the hanging wall right slides over the footwall left due to compressional forces. They bound many of the mountain ranges of the world and many of the rift valleys found along spreading margins. Mike dunning dorling kindersle getty images. If you imagine undoing the motion of a reverse fault you will undo the compression and thus lengthen the horizontal distance between two points on either side of the fault.

They are common at convergent boundaries. Reverse faults occur in areas undergoing compression squishing. Normal dip slip faults are produced by vertical compression as earth s crust lengthens. The hanging wall moves down relative to the foot wall.

The dip of a reverse fault is relatively steep greater than 45. The hanging wall moves up relative to the foot wall. Formed by compressional stress rocks are pushed towards each other thrust fault. Special type of reverse fault that is nearly horizontal angle has less than 45 degrees strike slip fault.

Other articles where normal fault is discussed. Normal faults are common. If the hanging wall rises relative to the footwall you have a reverse fault. The forces creating reverse faults are compressional pushing the sides together.

Reverse faults form when the hanging wall moves up. Tensional faults are produced through tension extension or pulling apart of the crust causing the hanging wall to move down relative to the footwall. Footwall definition the top of the rock stratum underlying a vein or bed of ore. A reverse fault is the opposite of a normal fault the hanging wall moves up relative to the footwall.