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Germany
North Rhine-Westphalia

Düsseldorf District

Mettmann
Wülfrath

Tillmannsdorfer Saddle in Wülfrath-Dornap

Discover
Places to see

Natural Monuments

Germany
North Rhine-Westphalia

Düsseldorf District

Mettmann
Wülfrath

Tillmannsdorfer Saddle in Wülfrath-Dornap

Highlight • Natural Monument

Tillmannsdorfer Saddle in Wülfrath-Dornap

Recommended by 127 cyclists out of 140

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    Top cycling routes to Tillmannsdorfer Saddle in Wülfrath-Dornap

    4.9

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    1. Glückauf Trail – Schulenberg Tunnel loop from Wuppertal Zoologischer Garten

    102km

    06:19

    900m

    900m

    Hard bike ride. Very good fitness required. Mostly paved surfaces. Suitable for all skill levels.

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    Hard

    Hard bike ride. Very good fitness required. Mostly paved surfaces. Suitable for all skill levels.

    Hard

    Hard bike ride. Very good fitness required. Mostly paved surfaces. Suitable for all skill levels.

    Hard

    Tips

    July 19, 2018

    Due to the Variscan orogeny about 300 million years ago, this subsoil folded in waves, forming saddles and humps of stratified rock. The weathering paved most of the saddles again, in some places such as on the Tillmannsdorfer saddle this folding has been preserved to the present day.

    Translated by Google •

      June 1, 2021

      Tillmanndorfer Fold is a geological outcrop, which, like a window, allows an insight into the geological structure and tectonics of the Düsselhügelland.
      In the Carboniferous (hard coal age), marine sediments were deposited here as lime sludge in a shallow sea, beginning around 330 million years ago. They mainly consisted of calcareous skeletal remains of dead sea creatures. Over the course of many millions of years, these deposits solidified to form a layered rock, coal lime.
      The Devonian followed the Carboniferous. During this time, beginning about 290 million years ago, the originally horizontal layers were unfolded by enormous forces in the earth's interior (plate tectonics). The Variskische Gebirge (Rhenish Slate Mountains) emerged with saddles and hollows. While weathering leveled most of the bulges (saddles) again in the following millions of years, in some places like here with the Tillmannsdorfer fold (also called Tillmansdorfer saddle) the saddle and fold were preserved. The older geological layers are in the core of the saddle, they become younger towards the outside.
      (Source kuladig.de/Objektansicht/KLD-245870)

      Translated by Google •

        May 26, 2019

        A nice climb to the Düsselhöhe.

        Translated by Google •

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          Elevation 200 m

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          Monday 8 December

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          10°C

          14 %

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          Max wind speed: 15.0 km/h

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          Location: Wülfrath, Mettmann, Düsseldorf District, North Rhine-Westphalia, Germany

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