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Hegau either refers to a region of the Duchy of Swabia or to only that part of said region which is presently located in the country of Germany. It is known for its extinct, partly eroded volcanoes, most of which are crowned with ruins of medieval fortresses.
Today, Hegau refers only to that part of the former Gau which is located within the German state of Baden-Württemberg. This region, also called the Hegauer Kegelbergland (lit.'Hegau conical hill landscape'), is a Young Driftmorainic landscape marked by the remains of several extinct volcanoes, the Hegau volcanoes, which are located mostly to the west and east of the line from Singen (Hohentwiel) in the south to Geisingen in the north. The Hegau volcanoes are national geotopes of Germany.
Origin of the landscape
The Hegau region, situated at about 400m (1,300ft)a.s.l., is surmounted by nearly a dozen conical hills, which are between 643m (2,110ft) and 867m (2,844ft) high and which correspond to the remains of the pipes of past volcanoes. The area was volcanically active during the Mioceneepoch.[2][3] Much later, during the Riss glaciation (Pleistocene epoch), about 150 ka ago, the Hegau region was covered by large glaciers, which over time eroded the softer rocks around the harder basaltic rocks of the former volcanic pipes (an example of an inverted relief). After the melting of the ice age glaciers, the landscape received its typical, modern-day appearance.
In conjunction with the past volcanisms, several maars formed in the area, which later filled with water to form lakes. The sediments of these maar lakes preserve exceptional fossils, for example of the early horse Hippotherium primigenium or of the giant salamander Andrias scheuchzeri.
During the Middle Ages, fortresses were built on top of several Hegau volcanoes.
The arguably best-known of the Hegau volcanoes is the Hohentwiel, on top of which lie the ruins of a fortress of the same name. The Hohentwiel is located next to the industrial city of Singen. It is the southernmost of the Hegau volcanoes. To the north of it, there are nine other extinct volcanoes (see list below).
↑ Johannes Baier & Armin Scherzinger (2021): Das Vulkanfeld im Hegau. Aufschluss, 72(2): 58–69.
↑ Johannes Baier & Armin Scherzinger (2024): Geohistorische Bemerkungen zum Vulkanfeld im Hegau. Jh. Ges. Naturkde. Württemberg, 180, 277–301.
↑ Johannes Baier (2025): Die Säulenklüftung beim Hohenstoffeln (Hegau). In: Aufschluss 76(2): 92-99.
↑ Johannes Baier, Armin Scherzinger (2024): Der Phonolithdom Hohentwiel im Hegau. Aufschluss, Jg. 75, H. 4, S. 253–262.
↑ Armin Scherzinger, Johanne Baier, Günter Schweigert, & Roland Berka (2024): Zur Entstehung der Höwenegg-Vulkangruppe und der Höwenegg-Schichten im Hegau. Jh. Ges. Naturkde. Württemberg, 180, S. 501–528.
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