The Black Forest consists of a cover of sandstone on top of a core of gneiss and granites. Formerly it shared tectonic evolution with the nearby Vosges Mountains. Later during the Middle Eocene a rifting period affected the area and caused formation of the Rhine graben. During the last glacial period of the W�rm glaciation, the Black Forest was covered by glaciers; several tarns (or lakes) such as the Mummelsee are remains of this period.
Rivers in the Black Forest include the Danube (which originates in the Black Forest as the confluence of the Brigach and Breg rivers), the Enz, the Kinzig, the Murg, the Nagold, the Neckar, the Rench, and the Wiese. The Black Forest is part of the continental divide between the Atlantic Ocean drainage basin (drained by the Rhine) and the Black Sea drainage basin (drained by the Danube).
� Feldberg (1,493 m (4,898 ft))
� Herzogenhorn (1,415 m (4,642 ft))
� Belchen (1,414 m (4,639 ft))
� Spiesshorn (1,349 m (4,426 ft))
� Schauinsland (1,284 m (4,213 ft))
� Kandel (Berg) (1,241 m (4,072 ft))
� Hochblauen (1,165 m (3,822 ft))
� Hornisgrinde (1,164 m (3,819
