Large blocks of solidified ice age gravel, stacked wildly on top of each other, characterize the "Devil's Kitchen" in the valley of the eastern Günz. They come from the steep valley flank above, from where they broke off in the post-glacial period. As a rockfall or landslide, they slid down the valley on loose gravel and fine sediments of the tertiary subsoil.

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Elevation 810 m

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Thursday 11 December

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Location: Obergünzburg, Ostallgäu, Allgäu, Swabia, Bavaria, Germany

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