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

To the dip is called dip slip faulting.

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

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. After the occurrence of a normal dip slip fault in flat lying sedimentary rocks the fault scarp produced is eliminated by erosion. When the hanging wall moves up in relative to the footwall it is called a fault. A reverse fault is the opposite of a normal 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. Describe three types of faults. The hanging wall moves down relative to the footwall. In thrust or reverse faults the hanging wall moves up relative to the footwall and in strike slip faults it moves horizontally relative to the footwall.

When the hanging wall moves down in relative to the footwall it is called a fault. Fill in the blank 1. The terminology of normal and reverse comes from coal mining in england where normal faults are the most common. In thrust or reverse faults the hanging wall moves up relative to the footwall and in strike slip faults it moves horizontally relative to the footwall.

Reverse faults indicate compressive shortening of the crust. This is true of normal faults. The dip of a reverse fault is relatively steep greater than 45.