Routes

Planner

Features

Updates

App

Login or Signup

Get the App

Login or Signup

Discover
Places to see

Lakes

Belgium
Wallonia

Wallonie

Liège
Verviers
Eupen

Brackvenn Moor Lakes

Highlight • Lake

Brackvenn Moor Lakes

Recommended by 1470 hikers out of 1506

This Highlight is in a protected area

Please check local regulations for: Parc naturel des Hautes-Fagnes – Eifel

Save

Share

  • More

  • Save

    Share

  • More

  • Take Me There

    Routes here

    Best Hikes to Brackvenn Moor Lakes

    4.8

    (760)

    2,724

    hikers

    1. Boardwalks Through Brackvenn – Brackvenn Moor Lake loop from Küchelscheid

    12.1km

    03:08

    80m

    80m

    Intermediate hike. Good fitness required. Easily-accessible paths. Suitable for all skill levels.

    Navigate

    Send to Phone

    Intermediate

    Easy hike. Great for any fitness level. Easily-accessible paths. Suitable for all skill levels.

    Easy

    Intermediate hike. Good fitness required. Easily-accessible paths. Suitable for all skill levels.

    Intermediate

    Tips

    October 22, 2022

    What is often called a lake in the Fens is often e.g. Palsas.
    The palsen or pingos in the High Fens were formed around 10,000 to 11,000 years ago at the end of the last ice age. When the ground froze deep down during the cold winters of the Ice Age, the wet ground expanded and frost mounds developed. Over the years these mounds grew and the soil material that was on top slid down the sides of the mounds and over time formed a ring-shaped wall around the mound of frost. With the end of the ice age, the ice melted, the frost mound sagged and the wall was preserved. The water in the middle is called bog scour or bog eye.
    Source: euregio-im-bild.de/fotos/palsen-im-brackvenn-bei-m-tzenich.html

    Translated by Google •

      October 22, 2022

      Anyone who sees the beauty of the raised and low moors will never be able to let it go.
      The colors of the landscape, indeed the entire appearance of the High Fens, change dramatically every season. Even in winter - a breathtakingly beautiful landscape.

      Translated by Google •

        November 30, 2022

        The peat that can be found everywhere in the bog and fen areas is the result of a process of incomplete decomposition. Usually, dead plants are gradually decomposed by small animals (such as earthworms), bacteria and fungi. This process applies to well-drained soils. On impervious acidic soils that do not contain many bacteria and in humid climates, plants such as peat moss are only partially decomposed. Their superimposition forms the peat layer. This peat layer can be up to 7 m in certain places here in the Brackvenn. 1 mm layer of peat takes 1 year to form. With a peat layer of 7 m, for example, we are talking about a period of 7,000 years.

        Translated by Google •

          Sign up for a free komoot account to get 61 more insider tips and takes.

          Sign up for free

          Details

          Informations

          Elevation 670 m

          Weather

          Powered by AerisWeather

          Today

          Monday 27 October

          6°C

          5°C

          100 %

          If you start your activity now...

          Max wind speed: 27.0 km/h

          Most visited during

          January

          February

          March

          April

          May

          June

          July

          August

          September

          October

          November

          December

          Loading

          Location: Eupen, Verviers, Liège, Wallonie, Wallonia, Belgium

          Other Popular Places to Check Out

          Boardwalks Through the Hohes Venn

          Explore
          RoutesRoute plannerFeaturesHikesMTB TrailsRoad cycling routesBikepacking
          Download the app
          Follow Us on Socials

          © komoot GmbH

          Privacy Policy