Heldburger Gangschar

The Heldburger Gangschar is a Cenozoic volcanic system in the Franconian parts of southern Thuringia and northern Bavaria. The term Gangschar refers to the fact that few of the volcanoes are still preserved as surface shape, while their former activity can be detected by “passage” called fissure fillings. These courses are mostly trained in south-south-west direction, their cross-section is often less than one meter. It is named after the small town Heldburg situated in the Bad Colberg-Heldburg municipality. Their surroundings, the Heldburger Land, completely belongs to the northern part of the volcanic zone. The most impressive by far the still preserved volcanic cones represent the 641 m and 679 m high Gleichberge situated nearby Heldburger Land.

Location

The 679 m and 641 m high rocky mountains Gleichberge situated nearby Heldburger Land
The fortress Veste Heldburg at Heldburger Land on the 405 m high rocky mountain of Phonolit
The 449 m high rocky mountain Straufhain, at its peak, the ruins of the medieval castle Straufhain

The Heldburger Gangschar is not a self-contained landscape and is distributed mainly on the main physiographic units Grabfeld, Itz- Baunach Hügelland and Haßberge. South of the river Main but their former activity is also detectable in the respective northern Steigerwald and Fränkische Alb. Your core zone extends from Hildburghausen to Gerolzhofen.

Volcanic cone

The following are the most famous preserved volcanic cones in parentheses their altitude, and their approximate age and their rock:

Older volcanoes such as the volcano of Oberleinleiter in the Fränkische Alb ( 31 million years, Olivinmelilithnephelinith and Olivinnephelinit ) are no longer recognizable as surface shape today. Although it is the latter reaches a height of 505 m, however, is completely sunk into the Jurassic rocks of the Alps.

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References

Coordinates: 50°17′19″N 10°43′43″E / 50.2886°N 10.7286°E