0000000000862915

AUTHOR

M. Pirrung

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Tertiary maars of the Hocheifel Volcanic Field, Germany

2008

In the Hocheifel only three maars are known. The Eckfeld Maar, filled with Eocene lacustrine sediments, is located at the southern boundary of the volcanic field, where the Tertiary peneplain has been eroded only slightly. The ages of the Jungferweiher Maar in the southeast and the Dottingen Maar in the northeast of the Tertiary Hocheifel Volcanic Field (THVF) are unknown and their timing within the THVF is uncertain. In contrast to the surrounding area, the central part of the THVF is deeply eroded. Here, six large diatremes (>600 m) were identified in the area of Kelberg with one exception. So far, no relics of crater sediments have been found within the large diatremes. They probably rep…

DiatremePeneplaingeographyCinder conegeography.geographical_feature_categoryVolcanoImpact craterGeochemistryCalderaSeismologyGeologyMaar
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