Transform boundaries are formed when the two plates are sliding alongside each other which results in the earthquakes and splitting of river beds.
The transform faults are also known as the strike-slip boundary, which occurs in the portion of the fracture zone that exists between the different offsets centers.
The linear valleys, small ponds, splitting of river beds, scrapes, and ridges are some of the surface phenomenons of the transform plate boundaries.
The San Andreas is one of the most famous types of transform faults in the Earth's crust.
Thus, the transform boundaries result in the fracture of the earth's surface.
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