Normal faults usually form where tectonic plate motions cause tension.
The hanging wall moves down relative to the footwall.
The hanging wall moves downward relative to the footwall.
Another type of fault is the thrust fault where ground on one side of the fault moves up and over adjacent ground.
A normal fault occurs when the crust is extended.
The hanging wall moves up relative to the footwall.
An upthrown block between two normal faults dipping away from each other is a horst.
Normal dip slip faults are produced by vertical compression as earth s crust lengthens.
The hanging wall moves down relative to the footwall.
Normal fault s are common.
Low angle normal faults with regional tectonic significance may be designated detachment faults.
What is the age of the rocks on the surface of the footwall side of the fault relative to those on the hanging wall.
In a normal fault the hanging wall moves downward relative to the footwall.
Along a normal fault the hanging wall moves down relative to the footwall.
When the hanging wall moves up in relative to the footwall it is called a fault.
The hanging wall moves down relative to the footwall.
The crust experiences extension.
A hanging wall is the overhanging rock unit on the slant that separates the two slabs while the footwall is below the slant what is the modern theory for orogenesis mountain building.
The footwall moves down relative to the hanging wall.
The hanging wall slides down relative to the footwall.
These usually occur when tectonic forces cause tension that pulls rocks apart.
After the occurrence of a normal dip slip fault in flat lying sedimentary rocks the fault scarp produced is eliminated by erosion.
Alternatively such a fault can be called an extensional fault.
They bound many of the mountain ranges of the world and many of the rift valleys found along spreading margins.
When the hanging wall moves down in relative to the footwall it is called a fault.
In a normal dip slip fault which of the following statements describes the movement of the hanging wall relative to the footwall.