A fault that forms at a divergent boundary
Along a normal fault, the hanging wall moves down relative to the footwall. Normal faults usually form where tectonic plate motions cause tension. Tension is stress that pulls rocks apart. Therefore, normal faults are common at mid-ocean ridges. At mid-ocean ridges, plate separation causes oceanic lithosphere to break into fault blocks.
it goes down slowly
Normal Fault
A normal fault.
This is true of normal faults. 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.
No. A thrust fault is a low-angle reverse fault.
it moves downwards
it goes down slowly
The Owens Valley is NOT a reverse fault. This valley is a normal fault.
Normal Fault
A Reverse fault is happens when tectonic forces cause compression that PUSHES rocks together. Normal fault happens when tectonic forces cause tension that PULLS rocks apart.Normal fault is when the hanging block moves down relative to foot block wall where as the reverse fault is formed when the hanging block wall moves up relative to the foot block walls a result of tension and compression force respectively
A normal fault.
it is a normal fault.
In a normal fault, the fault is at an angle, so one block of rock lies above the fault while the other lies below it. The rock above it is the hanging wall and the rock below it is the footwall. In a normal fault, the hanging wall moves downwards relative to the footwall.
a pulling motion causes a normal fault
three kinds of faults are normal fault, reverse fault, and strike-slip fault.
normal fault reverse fault slip strike fault
normal fault, reverse fault, strike-slip fault,