Contrary to popular belief, California will not suddenly "fall into the ocean." It will just continue moving at about 2 inches per year until, 15 million years from now, Los Angeles will be located right next to San Francisco. The southwestern portion of California is moving northwestward towards Alaska. The left-hand panels within each figure illustrate the evolution of slip rate in m/s, while the right-hand panels show the evolution of instantaneous slip direction in degrees. The 1,000 km-long Bolokenu-Aqikekuduk fault (Dzhungarian fault, BAF) is one of the major right-lateral strike-slip faults that cut across the Tian Shan Range. While strike-slip faults occur across the world, the most famous is the San Andreas fault. A series of snapshots of the three Andersonian dynamic rupture models are shown in Figures 3 (normal fault), 4 (reverse fault), and 5 (strike-slip fault). That means someone standing near the fault trace and looking across it would see the far side move to the right or to the left, respectively. a) right lateral b) left lateral c) reverse d) normal Based on what you already know about the movement of the Pacific and North American plates, what type of. Strike-slip faults are either right-lateral or left-lateral. The forces creating these faults are lateral or horizontal, carrying the sides past each other. In these faults, the fault plane is usually vertical so there is no hanging wall or footwall. That is, the slip occurs along the strike, not up or down the dip. Strike-slip faults have walls that move sideways, not up or down. jack0m/DigitalVision Vectors/Getty Images Strike-slip faults occur as plates scrape by each other.
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