18의 사벨스보스가지 명소 & 주요 장소

Huis De Beuk is a building in the Savelsbos forest, located in the Dutch municipality of Eijsden-Margraten. The white building is situated northeast of the village of Gronsveld, on a spur of the Wijngaardsberg/Riesenberg, on the edge of the Margraten Plateau. From this location, there is a view of the Meuse Valley to the west. South of Huis De Beuk, the Termaardergrub flows into the Meuse Valley.

A very beautiful forest. If you use the designated paths, you'll enjoy beautiful views of the Meuse Valley from the edge of the forest. The remains of old quarries provide further variety.

great place with beautiful view

Text board [see photo] Limestone quarry Trichterberg Geological Monument Limestone quarry Trichterberg In the past, limestone was mined at this location. This limestone was used as building blocks and at a later time for fertilizing (oenergelen) fields and meadows ` In the upper Cretaceous (80 to 65 million years ago) the whole of South Limburg was flooded by a 'Cretaceous sea'. Many plants and animals that are now extinct lived in this tropical sea. The limestone visible here consists of countless skeletons of small plants and animals that formed the plankton. Many large animals also lived in this Cretaceous sea, such as the ten-meter-long 'Mosasaur'. Flint Flint is a hard rock that can form in pure limestone under very special circumstances. Flint consists of pure silica (SiO2). In the Stone Age, this rock was used for making stone tools. Until the last century, flint was used to make fire using the Tinderbox.

Quarries The Groeve de Hel has two entrances that are separately indicated as Groeve de (Grote) Hel and Groeve de Kleine Hel. The entrance to Groeve de Grote Hel is located southwest and the entrance to Groeve de Kleine Hel is northeast. The two parts of Groeve de Hel are connected via a crawl-hole connection. Groeve de Hel is a medium-sized quarry and has an entrance area with a collapse doline. The stability of the quarries was poor due to over-exploitation of the quarries and the resulting cracks, especially in Groeve de Kleine Hel. The quarries are closed in such a way that bats can fly into the quarries. Wikipedia: The Groeve de Hel or Helgrove is a Limburg marl quarry in the Dutch municipality of Eijsden-Margraten. The underground quarry is located between Gronsveld and Cadier en Keer on the northwest side of the Riesenberg in the northern part of the Savelsbos. The quarry is located on the western edge of the Margraten Plateau in the transition to the Maas Valley. At the site, the plateau plunges steeply for several meters. The quarry is located along one of the two routes from Cadier and Keer to Gronsveld, the other via De Fontein and the Dorregrubbe dry valley on the other side of the Riesenberg. The route along Groeve de Hel runs via the Gruisveldweg, the Hotsboom, the Helweg and the Keerderweg. About 250 meters to the north is the Hotsboom Quarry, about 300 meters to the south are the Riesenberg Quarry and Groeve on top of the Riesenberg and about 300 meters to the southeast is the Varkensgat Quarry. About 300 meters to the south, Huis De Beuk is located at the head of the Riesenberg. Info: https://nl.wikipedia.org/wiki/Groeve_de_Hel

Beautiful climb with a view over the Gronsveld valley

Many hiking trails and routes around here. Nice view

One of the most beautiful in the area!!!