In a n fault the hanging wall block moves up with the respect to the footwall block.
Hanging wall block and footwall block.
In thrust faulting.
Arrows indicating relative movement of fault blocks f.
Hanging wall and footwall the two sides of a non vertical fault are known as the hanging wall and footwall.
Strike of the fault plane d.
What type of fault is illustrated.
Normal fault as well.
Student name date lab section 9.
When working a tabular ore body the miner stood with the footwall under his feet and with the hanging wall above him.
In diagram 111 below label the following.
Hanging wall block b.
Strike of the fault plane d.
Grabens are formed by what type of faulting.
The hanging wall block and footwall block are labeled in the following diagram.
In a normal fault the hanging wall block moves down relative to the footwall block.
Hanging wall block and footwall block remain in the same position vertically.
The hanging wall occurs above the fault plane and the footwall occurs below it.
The hanging wall block above an inclined fault plane moves downward relative to the lower footwall block.
Hangin wall moves down relative to the footwall.
Although the angle of inclination of a specific fault plane tends to be relatively uniform it may differ considerably along its length from place to place.
In a reverse fault the hanging wall block moves up relative to the footwall block.
When rocks slip past each other in faulting the upper or overlying block along the fault plane is called the hanging wall or headwall.
The crust is shortened and thickened.
Hanging wall block and footwall block.
Dipping fault the blocks are classified as vertical horizontal dipping dip slip strike slip oblique slip.
Normal faults are caused by tensional stress.
Hanging wall definition the underside of the wall rock overlying a vein or bed of ore.
This terminology comes from mining.