In fact, they often lack any recognizable topographic features on land. In addition, they don’t create or destroy crust so they’re more deceptive to see on land. The Piqiang Fault is a left-lateral fault.When you look at the Earth’s surface, transform boundaries are rarer than divergent and convergent plate boundaries. The unit of rock layers that moves toward the viewer relative to the red fault line is on the left. This method always works, no matter from which direction you are looking at the boundary!įigure 2.6.8. If it is on the left side, it is left-lateral.
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