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beds that tend towards being impervious. As weathering progresses, the structure becomes unstable as a result of the undercutting of the sandstone base. Towards the end of the last glaciation period this undercutting, in combination with extensive
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Today numerous boulders on the slopes of the
Ferschweiler Plateau bear witness to the major rock displacements of this period. The Devil's Gorge is a rock fissure between about 1 and 5 metres wide and is a direct consequence of the rock collapse.
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With its bizarre landscape, steep rock faces, narrow gorges and fissures, the Devil's Gorge is a popular attraction for tourists and the start point for other walks in the vicinity.
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The cause of this event was probably a combination of the geological and climatic circumstances. The heavily fissured, more or less porous, rock strata of the so-called
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288:Natural monuments in Rhineland-Palatinate
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134:is located on the eastern edge of the
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213:Typical rock formations in the gorge
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278:Valleys of Rhineland-Palatinate
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63:"Devil's Gorge" Eifel
140:South Eifel Nature Park
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