Taubenberg has a peculiar geomorphology. The highest point is in the west of the ridge. From there, the small flows in a valley in the center of the terrain structure to the east and the Mangfall, in which it flows. The valley of the Farnbach divides Taubenberg into a northern and a southern ridge, which are connected to each other in the west. The northern ridge is higher, in its east is the second highest point of the mountain. The southern ridge drops almost equally from west to east. In front of it is the , a broad sloping hollow with fen.