The answer would be upward
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.
Reverse Fault
Reverse Fault
Yes, when the hanging wall moves up relative to the footwall along a fault, it is known as a reverse fault. Reverse faults are caused by compressional forces in the Earth's crust, leading to the hanging wall moving up and over the footwall.
This type of fault is known as a reverse fault. Reverse faults are caused by compressional forces in the Earth's crust, which result in the hanging wall moving up relative to the footwall. This type of fault is common in areas where tectonic plates are colliding.
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.
Reverse Fault
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.
A reverse fault is a fault in which the hanging wall moves up relative to the footwall.
Reverse Fault
Yes, when the hanging wall moves up relative to the footwall along a fault, it is known as a reverse fault. Reverse faults are caused by compressional forces in the Earth's crust, leading to the hanging wall moving up and over the footwall.
thrust
This type of fault is known as a reverse fault. Reverse faults are caused by compressional forces in the Earth's crust, which result in the hanging wall moving up relative to the footwall. This type of fault is common in areas where tectonic plates are colliding.
No, a thrust fault is a type of reverse fault, where the hanging wall moves up and over the footwall. In contrast, a normal fault is a type of fault where the hanging wall moves down relative to the footwall.
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 called a reverse fault. It occurs when compressional forces cause the hanging wall to move up relative to the footwall along a steeply inclined fault plane. Reverse faults are commonly found in areas where tectonic plates are colliding or converging.
The key characteristic that distinguishes a normal fault from a reverse fault is the movement of the hanging wall relative to the footwall. In a normal fault, the hanging wall moves downward relative to the footwall, typically due to extensional forces, which pull the Earth's crust apart. Conversely, in a reverse fault, the hanging wall moves upward relative to the footwall, driven by compressional forces that push the crust together. Additionally, the angle of the fault plane can also provide clues, with normal faults usually having a lower angle and reverse faults typically being steeper.