Haupeschbaach – Halerbaach

The valleys of the Haupeschbaach and the Halerbaach near Beaufort and Haller are incised into the Luxembourg Sandstone and show the typical forms of such valleys. They have been formed […]

The valleys of the Haupeschbaach and the Halerbaach near Beaufort and Haller are incised into the Luxembourg Sandstone and show the typical forms of such valleys. They have been formed […]

The valleys of the Haupeschbaach and the Halerbaach near Beaufort and Haller are incised into the Luxembourg Sandstone and show […]

Mardell – small pond

A mardel (tiny pond) is a small hollow mould, which is at least temporarily filled with water. It is a typical form connected to dissolution of gypsum lenses or limestones […]

A mardel (tiny pond) is a small hollow mould, which is at least temporarily filled with water. It is a typical form connected to dissolution of gypsum lenses or limestones […]

A mardel (tiny pond) is a small hollow mould, which is at least temporarily filled with water. It is a […]

Gefale Leeën – rockfall in dolomite

The landscape in the area of the Gefale Leeën („fallen stones“) is the result of an enormous rockfall in dolomites of the Middle Triassic (“Muschelkalk”) and sliding processes of the […]

The landscape in the area of the Gefale Leeën („fallen stones“) is the result of an enormous rockfall in dolomites of the Middle Triassic (“Muschelkalk”) and sliding processes of the […]

The landscape in the area of the Gefale Leeën („fallen stones“) is the result of an enormous rockfall in dolomites […]

Alkummer – narrow passageway in dolomite

A large part of the dolomite rocks, limited by the joint system, slid and tilted on the marly layer underneath in the direction of the valley and opened up a […]

A large part of the dolomite rocks, limited by the joint system, slid and tilted on the marly layer underneath in the direction of the valley and opened up a […]

A large part of the dolomite rocks, limited by the joint system, slid and tilted on the marly layer underneath […]

Zeiebierg – a butte near Bech

At this location, the Luxembourg Sandstone plateau (li2) drops steeply down. About 100 m deeper, a gently undulating landscape of clayey marls (ku-km) extends to the south. There are still […]

At this location, the Luxembourg Sandstone plateau (li2) drops steeply down. About 100 m deeper, a gently undulating landscape of clayey marls (ku-km) extends to the south. There are still […]

At this location, the Luxembourg Sandstone plateau (li2) drops steeply down. About 100 m deeper, a gently undulating landscape of […]

Hëlt – Dolomite, orchids and wine

The Hëlt near Rosport is built up from the layers of the middle (marl with gypsum layers) and upper “Muschelkalk” (dolomite). The gypsum layers were quarried in open quarries in […]

The Hëlt near Rosport is built up from the layers of the middle (marl with gypsum layers) and upper “Muschelkalk” (dolomite). The gypsum layers were quarried in open quarries in […]

The Hëlt near Rosport is built up from the layers of the middle (marl with gypsum layers) and upper “Muschelkalk” […]

Dauschbuer – fascinating rock

Calcareous tufa springs are rare and special habitats that are home to a variety of specialised creatures and are protected EU-wide protection (FFH Directive). At the source of the spring, […]

Calcareous tufa springs are rare and special habitats that are home to a variety of specialised creatures and are protected EU-wide protection (FFH Directive). At the source of the spring, […]

Calcareous tufa springs are rare and special habitats that are home to a variety of specialised creatures and are protected […]

Noumerleeën – miniature image of the region

The rocky landscape of the Noumerleeën delimits the distribution area of the Luxembourg sandstone in the Natur- & Geopark Mëllerdall. To the northwest, the gently undulating landscapes of the marls […]

The rocky landscape of the Noumerleeën delimits the distribution area of the Luxembourg sandstone in the Natur- & Geopark Mëllerdall. To the northwest, the gently undulating landscapes of the marls […]

The rocky landscape of the Noumerleeën delimits the distribution area of the Luxembourg sandstone in the Natur- & Geopark Mëllerdall. […]

Schéissendëmpel – force of the water

At the Schéissendëmpel with its stone bridge, the water of the Black Ernz stream flows over some large boulders lying in the stream bed. They cannot be carried away by […]

At the Schéissendëmpel with its stone bridge, the water of the Black Ernz stream flows over some large boulders lying in the stream bed. They cannot be carried away by […]

At the Schéissendëmpel with its stone bridge, the water of the Black Ernz stream flows over some large boulders lying […]

Wollefsschlucht – a sandstone gorge

The steep rock cliffs of the up to 40-metre deep “Wolf’s Gorge” consist of Luxembourg sandstone (li2). While the sandstone forms the “Érelchen” plateau, the lower part of the slope […]

The steep rock cliffs of the up to 40-metre deep “Wolf’s Gorge” consist of Luxembourg sandstone (li2). While the sandstone forms the “Érelchen” plateau, the lower part of the slope […]

The steep rock cliffs of the up to 40-metre deep “Wolf’s Gorge” consist of Luxembourg sandstone (li2). While the sandstone […]