Contour maps use contour lines to connect points of equal elevation and represent the topography of a land area. Contour lines become closer together in steep slopes and farther apart in gradual slopes. They form a V pattern along valleys. Index contours are used to label elevations at regular intervals. The distance between contours is called the contour interval. Contour maps can show hills, depressions, and other geological features through patterns of concentric closed contours. They are generated from elevation points measured in the field.