ガーフェレの天然記念物・トップ20

Historically, the Keuzemeersen are a deposit area of the old Leie that meandered in a former flat valley. The Keuzemeersen are therefore located in a bend of the Leie as well as further downstream on the left bank of the Leie, where the typical meadow landscape has been preserved: small meadow plots with pollard willows, a riverbank and a fine-meshed network of ditches with associated fauna and flora. An adjustable weir regulates the water level of the central meadows. The Keuzemeersen are located near a place that is historically described as Keuze. These meadows are part of a whole of connected areas that contain the word "meers" as a name, including the Latemse Meersen, the Beelaertmeersen, the Blaarmeersen and the Bourgoyen-Ossemeersen.

Beautiful place at the Bron with the chapel of Saint Christiana

クリスティアナの泉は、現在でも水やレモネードが作られている場所で、本格的な地元の特産品であり、ビジネスでもあります。http://www.christiana.be/ 「岩」の壁に沿って、その上に倉庫と家が建てられた泉があり、そこから毎日泉水が汲み上げられ、ろ過され、ボトル詰めされています。

The Aelmoeseneiebos (or Aalmoezenijebos) is a nature reserve on the territory of the municipalities of Melle (Gontrode) and Oosterzele (Landskouter). The forest is 28.5 hectares in size and is owned by the University of Ghent. The forest area is now managed by the university Lab for Forest & Nature. The railway line Ghent-Geraardsbergen divides the forest in two. The Aelmoeseneiebos is an old forest area that already appeared on the Ferraris map in 1775. The forest was owned by the Saint Bavo's Abbey of Ghent for centuries. During the French period (1794-1815) it was transferred to the public poor relief of the city of Ghent. In 1967-1968 the Belgian State bought the forest so that the University of Ghent could use it as a test forest. The most important tree species are summer oak and beech, with ash and maple in the stream valleys. The Aelmoeseneiebos is known for its spring flora such as wood anemone, slender primrose, yellow dead-nettle and small periwinkle. During the First World War, the forest was largely cut down but replanted in 1920. Adjacent to the western part of the Aelmoeseneiebos, 10 hectares of plots of land belonging to Natuurpunt, Oosterzele department, are located in the valley of the Gondebeek. With the 'Rodeland landscape project' [1], the aim is to connect the Aelmoeseneiebos with the Makegemse forests through afforestation in the valleys of the Gondebeek, Kerkesbeek and Driesbeek[2][3]. In 2021, 5 amphibian tunnels were constructed in the Gondebeek valley[4]. Inventories and research in the Aelmoeseneiebos found 1329 different species: including 64 tree and shrub species and 599 species of invertebrates. The Aelmoeseneiebos is protected in Europe as part of the Natura 2000 area (habitat directive area) 'Forests of the south-east of the Zandleemstreek' (BE2300044). The forest is freely accessible on the footpaths.

This nature reserve is a remnant of an extensive forest area that gradually had to make way for agriculture in the 18th century. The surrounding land and the forest were owned for centuries by the Aalmoezenij, the poor relief of the Ghent Saint Bavo's Abbey. The production of wood was the main function at that time. The forest was purchased by the Belgian state in 1967-1968 so that the University of Ghent could use it as a test forest. In the early years, it was mainly used for studies on the growth and management of forests with a view to wood production. It also had a recreational and educational function. Railway line 122 Melle-Geraardsbergen divides the forest in two. In the western part (where we walked) an arboretum was created in 1973. With the 'Rodeland landscape project', the aim is to connect the Aelmoeseneiebos with the Makegemse forests through further afforestation of a number of stream valleys.

Beautiful, peaceful nature walk. A small part of the route was quite overgrown with nettles, but nothing insurmountable.

Lots of field paths, close to the stream, a few 'mills' and quite a bit of mud... so waterproof shoes are recommended!

What is exceptional for Flanders is that the Zwalm bridges a height difference of 60 m at a distance of barely 19 km. This means it has a lot of energy. It also has a basin of 155 km², which ensures a decent flow. This decline and this assured flow were used in the past by water mills. (Wikipedia)