The lower half of a fault is typically referred to as the "footwall." This is the block of rock that lies beneath the fault plane and remains stationary during fault movement. In contrast, the upper half is known as the "hanging wall," which moves downward in relation to the footwall during certain types of faulting, such as normal faults. The interaction between these two blocks is crucial in understanding geological processes and earthquake mechanics.
the lower half of Greece
The word used to describe movement on faults is "fault slip." This term refers to the relative displacement of rock masses along a fault line during tectonic activity, such as an earthquake. Fault slip can occur in various forms, including strike-slip, dip-slip, and oblique-slip, depending on the direction of the movement.
The Hayward Fault is a Strike-slip Fault.
The fault that caused the 1995 Kobe earthquake was the Nojima fault.
A reverse fault is formed here
The lower block is known as the footwall.
This block of rock is called a footwall.
This block of rock is called a footwall.
The block of rock below the fault line is called the footwall. This block remains stationary while the other block, called the hanging wall, moves during fault movement.
hanging wall
The footwall
The footwall is the half of the fault that lies below.
The Footwall is half of a fault that lies below .
Altamaha
Altamaha
fault block
a normal fault