Transform boundaries are seen in earthquakes that are caused by normal faults. Some types of faults are listric or ring faults.
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Normal faults are associated with divergent plate boundaries, where two tectonic plates are moving away from each other. This type of boundary results in tensional stress that leads to the hanging wall moving down relative to the footwall, creating a normal fault.
Earthquakes are typically caused by movement along a fault line, which is a fracture in the Earth's crust where rocks have shifted position relative to each other. The three main types of faults that can cause earthquakes are normal faults, reverse faults, and strike-slip faults.
The landforms that are formed at a transform boundary forms features such as fault lines and oceanic fracture zones. Fault lines are also known as strike slip faults. They produce powerful earthquakes.
Earthquakes can occur at any type of plate boundary, but the most powerful earthquakes tend to occur at convergent boundaries and at transform boundaries.
A transform boundary. This is where tectonic plates slide horizontally past each other in opposite directions. This movement can cause earthquakes along the boundary.
The stress that causes strike-slip faults is produced by a shearing force and so is called shear stress.