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is a large volcanic mountain range in the German Central Uplands in the state of Hesse, separated from the Rhön Mountains by the Fulda river valley.
Thus it consists of a multitude of overlapping basalt terraces, which descend from the Oberwald, the high central plateau, 600 to 773 metres high, in series of stepped rings to the edges of the mountain region.
As a result of volcanic activity, mainly basaltic lava and pyroclastic deposits were formed.
During the course of this volcanicity, trachyte and phonolite were produced in the early stages, then alkali-olivine basalts were deposited, which alternated with tholeiites.
There is also this geological divide with the Fulda-Haune Tableland, which lies in front of the Knüll to the northeast.
Between them is the Großenlüder-Lauterbacher Graben. By contrast, in the north, the vulcanite does not end until it reaches the adjacent North Vogelsberg Foreland, i.e. Even the Anterior Vogelsberg which lies outside the latter region still has large areas of basaltic rock.