vertical direction
The movement of the Hanging wall in the normal fault downward with the gravity whereas in the Reverse fault the hanging wall moved upward against the gravity
Faults are breaks in the crust where the crust has moved. The types of dip-slip faults are normal and reverse faults. In both of these, the movement is along the slope of the fault. Sudden movements along these faults can produce fault scarps. Layers of rock being misaligned is evidence of fault movement. Fault creep is caused by slow movement along the fault.In a normal fault, the plates are moving away from each other. This is due to tension. When the fault moves, the footwall rises relative to the hanging wall. Normal faults occur at divergent boundaries, such as ocean ridges. Normal faults can produce fault-block mountains.In a reverse fault, the plates are moving towards each other. This is due to compression. Here, the footwall falls relative to the hanging wall. A thrust fault is a special type of reverse fault, where the angle is shallow. Reverse faults occur at convergent boundaries, like subduction zones.A strike-slip fault is where the two plates move horizontally past each other. The force between them is called shearing. This type of fault is often called a transform fault, because they occur at transform boundaries.
A place where two tectonic plates meet is a fracture in the Earth.
Fault boundaries are the places where two tectonic plates (sections of the earth's crust) meet. Because of the movement of the plates against one another, fault boundaries are the locations where most earthquakes occur.
a fault
In a normal fault, the crust moves along a downward sloping fault plane, with the hanging wall moving down relative to the footwall. This movement is caused by tensional stresses pulling the crust apart.
The movement of the crust along a thrust fault is usually a reverse movement unlike the movement along a normal fault.
The movement of the crust along a thrust fault is usually a reverse movement unlike the movement along a normal fault.
This is known as a fault. A fault is a fracture in the Earth's crust along which movement has occurred. Movement along faults can result in earthquakes.
A break in the Earth's crust along which there has been some movement is a fault. A fault is considered a planar fracture.
A normal fault is a type of fault in which the hanging wall drops down relative to the footwall due to tensional forces in the Earth's crust. This type of fault is commonly associated with extensional tectonic settings, where the crust is being pulled apart.
In a dip-slip fault, the movement is primarily vertical along the fault plane, either up (reverse fault) or down (normal fault). In a strike-slip fault, the movement is primarily horizontal along the fault plane, with minimal vertical movement. Both types of faults are caused by tectonic stresses in the Earth's crust.
a normal fault, which is caused by tensional forces pulling apart the Earth's crust. This movement results in the hanging wall dropping relative to the footwall, creating a sloping fault plane.
It is known as a 'fault'.
A fault is a fracture in the Earth's crust where movement has occurred. This movement can be horizontal, vertical, or a combination of both. Faults can generate earthquakes when the stress along the fault is released suddenly, resulting in movement along the fault surface.
When movement occurs along a normal fault, the hanging wall moves down relative to the footwall. This type of faulting is caused by extensional stresses in the Earth's crust, where the crust is being pulled apart. Normal faults are common in areas of tectonic plate divergence or in regions experiencing crustal extension.
The hanging wall typically moves upward in a reverse fault or downward in a normal fault, due to the movement along the fault line causing one block to move relative to the other. This movement is a result of the stress and deformation within the Earth's crust.