A normal fault
The hanging wall is the block of rock that lies above an inclined fault plane or dip in the Earth's crust. It moves down relative to the footwall during faulting or mining activities.
As the air moves down the leeward side of a mountain, it gets compressed due to higher pressure at lower altitudes. This compression leads to increased temperature and decreased relative humidity, causing the air to warm up and dry out. This process is known as the Foehn effect.
The direction of a transverse wave is perpendicular to the direction of its motion. This means that as the wave moves forward, the particles of the medium oscillate up and down or side to side.
When a pendulum is hanging straight down, it has gravitational potential energy. This energy is due to its position in the Earth's gravitational field.
The medium moves perpendicular to the direction of the wave. In a transverse wave, the particles of the medium move up and down or side to side, while the wave itself moves forward. In a longitudinal wave, the particles move back and forth in the same direction as the wave propagation.
In a normal fault, the hanging wall moves down relative to the footwall, whereas in a reverse fault, the hanging wall moves up relative to the footwall.
the hanging wall moves down relative to the footwall
The two main types of faulting are normal faulting, where the hanging wall moves down relative to the footwall, and reverse faulting, where the hanging wall moves up relative to the footwall.
It is called a Normal Fault.
No, a hanging wall and a footwall are not the same in geology. The hanging wall is the block of rock above a fault line that moves down relative to the footwall, which is the block of rock below the fault line that moves up.
In a normal fault, the hanging wall moves downward relative to the footwall, creating extensional forces. In a reverse fault, the hanging wall moves upward relative to the footwall, generating compressional forces.
In a normal fault, the hanging wall moves down relative to the footwall. This results in the footwall being pushed up and becoming uplifted relative to the hanging wall.
That geological structure is called a normal fault, where the hanging wall moves down relative to the footwall. If the hanging wall slides up and over the footwall, it is known as a reverse 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.
The result is a normal fault, where the hanging wall moves down relative to the footwall due to extensional forces pulling the rock layers apart.
thrust
In a normal fault, the hanging wall moves down relative to the footwall due to tensional forces pulling the plates apart. This type of fault is associated with divergent plate boundaries or areas where the Earth's crust is being pulled apart.