Lines of springs are characteristic of these objects, and the classic theory of their formation is named after Anderson. One type of these objects is divided into "leaky" and "transpressional" types, and in a "reverse" one, the hade is toward the upthrow side. A "reverse" one is almost always a (*) dip-slip type, since in the strike-slip type the walls move horizontally rather than vertically. For
Lines of springs are characteristic of these objects, and the classic theory of their formation is named after Anderson. One type of these objects is divided into "leaky" and "transpressional" types, and in a "reverse" one, the hade is toward the upthrow side. A "reverse" one is almost always a (*) dip-slip type, since in the strike-slip type the walls move horizontally rather than vertically. For 10 points, name these "cracks" in the Earth's crust where one part of the crust moves against another part, a prominent example of which is the San Andreas.
Lines of springs are characteristic of these objects, and the classic theory of their formation is named after Anderson.
faults [or faultlines; prompt on transverse plate boundaries]