gradpoint: anticlines
The three types of faults are normal, reverse, and strike-slip faults. Normal faults are associated with divergent plate boundaries, reverse faults with convergent plate boundaries, and strike-slip faults with transform plate boundaries.
Normal faults, where the hanging wall drops down relative to the footwall, typically do not generate tsunamis. These faults are more common in areas of active stretching of the Earth's crust and are not usually associated with the sudden vertical displacement of large volumes of water required to trigger a tsunami.
Normal faults are typically associated with extensional regimes where the Earth's crust is being pulled apart. This can occur in settings such as divergent plate boundaries, rift zones, or areas where the crust is being uplifted.
Flambrough Head is a chalk headland with sheer white cliffs. Without looking at a Geological Map of the area I can not tell you if there are any faults running through it (but it is likely) but the Chalk rock will be jointed. I believe there are stacks and caves associated with the headland and these are probably associated with the majour joints (perhaps faults).
Fault-block mountains are associated with normal faults, where blocks of crust are uplifted along one side of the fault while the other side drops down. As the movement along the fault continues, it can lead to the formation of a mountain range with steep slopes on one side and gentler slopes on the other.
Faults
Faults are closely associated with earthquakes and tectonic plate movements. They are fractures in Earth's crust where blocks of rocks move relative to each other, releasing accumulated stress and causing seismic activity.
Earthquakes.
The three types of faults are normal, reverse, and strike-slip faults. Normal faults are associated with divergent plate boundaries, reverse faults with convergent plate boundaries, and strike-slip faults with transform plate boundaries.
Normal fault: Associated with tensional stress, where the hanging wall moves down relative to the footwall. Reverse fault: Associated with compressional stress, where the hanging wall moves up relative to the footwall. Strike-slip fault: Associated with shear stress, where the rocks move horizontally past each other.
Normal faults, where the hanging wall drops down relative to the footwall, typically do not generate tsunamis. These faults are more common in areas of active stretching of the Earth's crust and are not usually associated with the sudden vertical displacement of large volumes of water required to trigger a tsunami.
extensional
A step-down transformer does just what it's designed to do, so there are no 'major' faults associated with it.
Normal faults occur when the hanging wall moves down relative to the footwall due to extensional forces, while reverse faults occur when the hanging wall moves up relative to the footwall due to compressional forces. Normal faults are associated with divergent plate boundaries, while reverse faults are associated with convergent plate boundaries.
Shear Stress.
Normal faults are typically associated with extensional regimes where the Earth's crust is being pulled apart. This can occur in settings such as divergent plate boundaries, rift zones, or areas where the crust is being uplifted.
Flambrough Head is a chalk headland with sheer white cliffs. Without looking at a Geological Map of the area I can not tell you if there are any faults running through it (but it is likely) but the Chalk rock will be jointed. I believe there are stacks and caves associated with the headland and these are probably associated with the majour joints (perhaps faults).