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Transform Fault - A transform fault is a plate boundary along which the relative motion between the two plates is parallel to the strike of the fault and is geometrically the arc of a small circle about the pole of rotation between two plates.
Characteristics - Transform boundaries are places where plates slide sideways past each other. At transform boundaries lithosphere is neither created nor destroyed. Many transform boundaries are found on the sea floor, where they connect segments of diverging mid-ocean ridges. California's San Andreas fault is a transform boundary.
Geological Events - Earthquake is likely to happen in a transform fault in Geological event when happened. The grinding action between the plates at a transform plate boundary results in shallow earthquakes, large lateral displacement of rock, and a broad zone of crustal deformation.
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