1) There are different types of folds that can be identified on a geologic map based on the attitude of their axial planes and the direction of dip of the strata. Synclines and anticlines can be distinguished by the direction strata dip and the age of the strata. 2) Folds should be described on a map by specifying the type of strata, the direction of the fold axis, any plunge direction, and whether it is symmetrical or not, plunging or not, and if it is a syncline, anticline, or monocline. 3) When writing a report for a geologic map, it is important to discuss the geomorphology, structure geology, topography