These features are commonly represented on geologic maps by a ball and a bar.
Pseudotachylite is generally found near these geologic features, whose surfaces can feature slickenlines and chatter marks. These features are commonly represented on geologic maps by a ball and a bar. Drag folds as well as gash fractures can be used to determine the orientation of these features, along which grabens may form. Compressive stress can force a hanging wall up and over a footwall, leading to the reverse variety of these structures. For 10 points, name these geologic structures that come in a strike-slip form exemplified by the San Andreas one.
Pseudotachylite is generally found near these geologic features, whose surfaces can feature slickenlines and chatter marks.
faults [accept more specific kinds until "reverse"]