In A Fault The Hanging Wall Moves Up Relative To The Footwall

This is true of normal faults.

In a fault the hanging wall moves up relative to the footwall.

In dip slip faults if the hanging wall block moves downward relative to the footwall read more. After the occurrence of a normal dip slip fault in flat lying sedimentary rocks the fault scarp produced is eliminated by erosion. The dip of a reverse fault is relatively steep greater than 45. What is the age of the rocks on the surface of the footwall side of the fault relative to those on the hanging wall.

Describe three types of faults. Reverse faults indicate compressive shortening of the crust. To the dip is called dip slip faulting. When the hanging wall moves down in relative to the footwall it is called a fault.

Fill in the blank 1. These usually occur when tectonic forces cause tension that pulls rocks apart. Strike slip faults are right lateral or left lateral depending on whether the block on the opposite side of the fault from an observer has moved to the right or left. The hanging wall moves down relative to the footwall.

A reverse fault is the opposite of a normal fault the hanging wall moves up relative to the footwall. The terminology of normal and reverse comes from coal mining in england where normal faults are the most common. This is true of normal faults.