
The Eger Graben (much less commonly called the Ohre or Ohře Graben; cs, Oherský rift, german: Egergraben) is a geological structure in the
Czech Republic. It runs southwards, parallel to the
Ore Mountains and its formation is linked with that of the mountain range.
Topography
The
Ohře (equally commonly known in English by its German name ''Eger'', hence the name of the trough) flows through the Eger
Graben
In geology, a graben () is a depressed block of the crust of a planet or moon, bordered by parallel normal faults.
Etymology
''Graben'' is a loan word from German, meaning 'ditch' or 'trench'. The word was first used in the geologic contex ...
and separates the Ore Mountains from the
Slavkov Forest and the
Doupov Mountains. The trench continues to the northeast along the valley of the
Bílina and later, as the
North Bohemian Basin, separates the Ore Mountains from the
Bohemian Central Mountains
Bohemian or Bohemians may refer to:
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, where the River Ohře leaves the graben and flows into the Elbe south of the Bohemian Mountains.
Geology
The Eger Graben is part of the
European Cenozoic Rift System and was created geologically on the same principle as the
Rhine Rift Valley. It was formed by the almost complete erosion of the
Variscan Mountains and sits on a
fault-block caused by the horizontal pressure of the
African continental plate. This block dropped, however, in contrast to the surrounding area. The Ore Mountains are
fault-block mountains
Fault blocks are very large blocks of rock, sometimes hundreds of kilometres in extent, created by tectonic and localized stresses in Earth's crust. Large areas of bedrock are broken up into blocks by faults. Blocks are characterized by rela ...
which rise very gently in Germany, but drop very steeply into the Eger Graben. The trench thus follows the main fault line of the Ore Mountains. Researchers believe that a new volcano is in the process of forming and hope to be able to drill holes in the area to better study what they believe is an awakening volcano.
''Sachsen: Forscher entdecken erwachenden Vulkan nach Erdbeben''
at focus.de. Retrieved 18 December 2021.
References
Sources
P. De`zes*, S.M. Schmid, P.A. Ziegler (2004) ''Evolution of the European Cenozoic Rift System: interaction of the Alpine and Pyrenean orogens with their foreland lithosphere''
Peter A. Ziegler (1990) ''Geological atlas of Western and Central Europe'', Volume 2
{{Authority control
Geography of the Czech Republic
Cenozoic rifts and grabens