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A normal fault.
thrust
Thrust
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.
Seismic waves are released when rock moves along a fault. These waves are the ones that cause earthquakes.
A normal fault is a fault in which the hanging wall has moved downward relative to the footwall.
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.
thrust
In a normal fault, the hanging wall moves down relative to the foot wall.
Reverse Fault
Thrust
Thrust
Thrust
Reverse Fault
A normal fault.
A normal fault
A reverse fault is a fault in which the hanging wall moves up relative to the footwall.