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.
This is a reverse fault, also known as a thrust fault. Reverse faults are caused by compressional forces in the Earth's crust, leading to the hanging wall moving up relative to the foot wall. This type of fault is often associated with mountain-building processes.
The position of the hanging wall relative to the foot wall indicates the type of fault and the stress acting on the rock layer. In a normal fault, the hanging wall moves downward relative to the foot wall, suggesting extensional stress that pulls rocks apart. Conversely, in a reverse fault, the hanging wall moves upward, indicating compressional stress that pushes rocks together. These movements reflect the geological forces shaping the Earth's crust.
A reverse fault is in a zone of compressional faulting, rocks in the hanging wall are pushed up relative to rocks in the footwall. A normal fault is in a zone of tensional faulting, rocks in the hanging wall drop down relative to those in a footwall forming a normal fault.
The hanging wall moves up relative to the foot wall. These happen when tectonic forces push rocks together. It is caused by compression.
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 foot wall.
thrust
In geology, the hanging wall refers to the rock layer above a fault plane, while the footwall refers to the rock layer below the fault plane. The hanging wall moves downward relative to the footwall in a normal fault, whereas in a reverse fault, the hanging wall moves up relative to the footwall.
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.
This is a reverse fault, also known as a thrust fault. Reverse faults are caused by compressional forces in the Earth's crust, leading to the hanging wall moving up relative to the foot wall. This type of fault is often associated with mountain-building processes.
The position of the hanging wall relative to the foot wall indicates the type of fault and the stress acting on the rock layer. In a normal fault, the hanging wall moves downward relative to the foot wall, suggesting extensional stress that pulls rocks apart. Conversely, in a reverse fault, the hanging wall moves upward, indicating compressional stress that pushes rocks together. These movements reflect the geological forces shaping the Earth's crust.
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
reverse fault. but that is when the foot wall moves down, the hanging wall moves up. in a strike-slip fault, they slide past each other, the foot wall and hanging wall are not there because it has to be like this to be a reverse or normal fault: hanging wall ----------foot wall ----------- in this diagram, the foot wall has moved down making the hanging wall move up to form a reverse fault. remember this on tests: the hanging wall is always above the fault line: /hanging wall above foot wall below / /
A reverse fault is in a zone of compressional faulting, rocks in the hanging wall are pushed up relative to rocks in the footwall. A normal fault is in a zone of tensional faulting, rocks in the hanging wall drop down relative to those in a footwall forming a normal fault.
No
A block of rock below the plane of a fault is known as the hanging wall. It is the rock mass that is located above the fault plane and typically moves downward relative to the footwall during fault movement.