A fold is a bend in layers of rock. Its sloping sides are the limbs; they meet at the hinge, where the layers are most curved, and the line along the hinge is the fold axis. An anticline is a fold whose layers bend upward, its limbs dipping away from the axis; a syncline is a fold whose layers bend downward, its limbs dipping toward the axis.
Examples
Example 20.10 (The Varden folds)
The limbs of the Varden folds dip , so the cover was shortened by , about : a stretch of the region wide today was wide before folding. Measured on section A–B as drawn, the limbs would look about steep, because the vertical scale is stretched 2.5 times: is multiplied by 2.5, and . Read at face value, that would give a shortening of , more than five times too much.