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Belgium

Flanders

South Limburg

Maaseik

Meeuwen-Gruitrode

Oudsberg Sand Dune

Discover
Places to see

Belgium

Flanders

South Limburg

Maaseik

Meeuwen-Gruitrode

Oudsberg Sand Dune

Oudsberg Sand Dune

Recommended by 331 hikers out of 334

This Highlight is in a protected area

Please check local regulations for: Vlaams Natuurreservaat Oudsberg

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    Best Hikes to Oudsberg Sand Dune

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    1. Oudsberg Dune – Oudsberg Sand Dune loop from Opoeteren

    8.05km

    02:06

    50m

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

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    Intermediate

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

    Intermediate

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

    Intermediate

    Tips

    September 27, 2021

    Now you are in the middle of the dune belt: 3,000 hectares of pure gold! An overwhelming mix of untouched forests, colorful heaths, beautiful moors, fields and meadows.



    In the dune belt you will find rich fauna and flora with enormous biological diversity. The area is home to some rare species: birds such as the red-backed shrike or the nightjar, insects such as the brook damsel, the wood cricket or the red wood ant. You can also spot amphibians like the Finnish salamander or even snakes like the smooth snake. Birds of prey such as buzzards, hawks and meadow harriers also make their home here.

    Translated by Google •

      October 12, 2023

      The pearl of the Dune Belt is the Oudsberg: the highest and largest open drift dune in Flanders. It rises 85 m above sea level. The Oudsberg is surrounded by beautiful heathlands, stately forests and butterfly-rich heathland grasslands. Since 1998 it has been recognized as a Flemish nature reserve.

      (duinenbanden.be)

      Translated by Google •

        February 11, 2024

        The Oudsberg nature reserve belongs to a dune belt that used to stretch from Hechtel to Maaseik. 15,000 years ago, after the last ice ages, the Kempen Plateau experienced enormous sand drifts. Deep, empty depressions formed, in which fens arose. High sand deposits rose above the landscape like dune ridges. As the climate warmed, birch and oak forests developed.

        In the Middle Ages, the soil southwest of De Oudsberg became impoverished due to intensive extraction. As a result, only heather could survive. Local overgrazing of sheep again caused sand drift, which shaped the current dune landscape. More at natuurenbos.be/natuurgebied/oudsberg

        Translated by Google •

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          Elevation 120 m

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          Monday 22 September

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          Location: Meeuwen-Gruitrode, Maaseik, South Limburg, Flanders, Belgium

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