Hanging Wall Block And Footwall Block

Strike of the fault plane d.

Hanging wall block and footwall block.

In a reverse fault the hanging wall block moves up relative to the footwall block. When working a tabular ore body the miner stood with the footwall under his feet and with the hanging wall above him. Sliding parallel to fault plane dip. In a n fault the hanging wall block moves up with the respect to the footwall block.

Hangin wall moves down relative to the footwall. Hanging wall and footwall the two sides of a non vertical fault are known as the hanging wall and footwall. The crust is shortened and thickened. Normal faults are caused by tensional stress.

Arrows indicating relative movement of fault blocks f. What type of fault is illustrated. What feature in distorted layered sedimentary rocks are evidence of horizontal compression and shortening. In a normal fault the hanging wall block moves down relative to the footwall block.

Hanging wall block b. Student name date lab section 9. This terminology comes from mining. Grabens are formed by what type of faulting.

Hanging wall block and footwall block remain in the same position vertically. In thrust faulting. Dipping fault the blocks are classified as vertical horizontal dipping dip slip strike slip oblique slip. Hanging wall block and footwall block.

The hanging wall block above an inclined fault plane moves downward relative to the lower footwall block. The hanging wall occurs above the fault plane and the footwall occurs below it. In diagram 111 below label the following. The block below is called the footwall.

When rocks slip past each other in faulting the upper or overlying block along the fault plane is called the hanging wall or headwall. Hanging wall definition the underside of the wall rock overlying a vein or bed of ore. Strike of the fault plane d.