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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.
These volcanic products overlaid a basement of bunter sandstone and tertiary sands, in small areas in the east also rocks of the muschelkalk and keuper.
Erosion following the Miocene wore away the contiguous basalt nappes, which originally reached as far as the area of the Lower Main, back to isolated deposits in the central complex.
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The volcanism of the Vogelsberg was mainly active during the Middle Miocene, according to potassium-argon dating 18.5-10 million years ago, reaching its peak 17-15 million years ago.
These deposits were mined over a long period of time in order to produce raw materials for industry, and the basalt was and still is a highly popular raw material for gravel and natural stone production.
is based, on the one hand, on the relief of the mountain range from its highest point towards the outside and, on the other hand, on its river catchments which radiate outwards: the catchments of the Eder (Schwalm), Lower Fulda (Schlitz and Lüder), Main (Kinzig and Nidda) and Lahn (Ohm).
It is not a former shield volcano, but comprises many individual volcanoes, which are superimposed.
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.
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As a result of volcanic activity, mainly basaltic lava and pyroclastic deposits were formed.