아마이‬에서 가장 멋진 ‪20‬개의 천연기념물

어렸을 때 동굴 바닥에서부터 올라가면 유적지 꼭대기에 도착했습니다. 도시의 아름다운 파노라마와 함께요.

산책하기에 아주 좋은 곳입니다. Trixhes에서 시작하여 채석장을 따라가는 작은 길을 따라 내려갈 수 있습니다. 아래로 내려가면 Roches 채석장에 도착합니다. 거기서부터 다양한 암석이 있는 두 개의 측면을 통과합니다. 계속 가면 "Houlbouse" 거리에 도착합니다. 그리고 마침내 Chokier에 도착합니다. 아주 멋진 하이킹입니다. 개와 함께, 특히 아이들과 함께 하기에 좋습니다.

자갈 채석장은 사진 애호가나 잘 관리된 길을 걷고 새를 조용히 관찰하고 싶은 산책객에게 매우 풍부한 장소입니다. 하이커와 사진가에게 추천하는 장소입니다. 개를 목줄에 매고 다니는 것과 같이 지침을 존중해 주십시오(일부 사람들이 개를 자유롭게 풀어주어도 해를 끼치지 않을 것이라고 생각하더라도, 포식 본능을 가진 동물이 있어 땅에 둥지를 트는 물총새와 같은 일부 새를 쫓아낼 수 있다는 것을 알아두십시오). 또한 새를 방해하지 않도록 수영하지 마십시오. 지침을 존중하는 모든 분들께 감사드리며, 즐거운 하이킹이나 사진 촬영이 되시기를 바랍니다 🙏.

Excavations are conducted year-round at Moha Castle, making it unique in Belgium. When I visited, two archaeologists were uncovering a wall that runs beneath the visible castle and likely dates back to the 12th century.

The castle is free to visit. At the foot of the rock, there's a visitor center where you can pick up a badge to open the gate. For €4, you can also get a brochure with information about the most important points. The castle is only open to visitors starting in April, but the friendly man at the visitor center let me in on February 27th... as far as you can even call it "inside" at this ruin ;-)

The exact origins of the medieval County of Moha remain unknown. It is likely that the county was formed during the fragmentation of the Carolingian Empire and the Hesbaye region at the end of the 9th century. The first known count, Albert of Moha, is mentioned in a document dated 1026 or 1028. The first defensive stone walls also date from the first half of the 11th century. Having no male heir, Albert of Moha married his daughter to Henry I of Dasbourg around 1050, thus linking the county's destiny to that of this powerful family of Alsatian origin. Initially, it is highly unlikely that the Counts of Dasbourg regularly resided in Moha, entrusting the county's administration to trusted men and a small garrison. However, the situation changed with Hugh II (1130-1180) and his son Albert II (d. 1212), who decided to become more involved in the region's politics. Albert II, in particular, chose to align his interests with those of his nephew, Duke Henry I of Brabant, whose policies he would follow until the end of the 12th century. In 1204, Count Albert III, having lost hope of having a son, chose the Prince-Bishop of Liège as his heir. But the late birth of his daughter Gertrude would jeopardize these agreements. Quickly betrothed to Thibaut of Lorraine, who died in 1219, she then married Thibaut of Champagne, who repudiated her, and subsequently Simon of Linange. At 19, she died childless. On March 19, 1225, the Prince-Bishop of Liège, Hugues de Pierrepont, took possession of Moha. Under the Prince-Bishops, Moha became a prison for political prisoners and a fortification tasked with controlling the city of Huy and blockading merchants. This policy was deeply unpopular and led to reprisals: the people of Huy besieged Moha in 1255. The fortress of Moha was considered impregnable. It was therefore through trickery that the people of Huy, taking advantage of a request for a truce, seized the castle on May 6, 1376. After the attack on the castle, the site's history is largely unknown. Mass is still celebrated twice a year in the castle chapel. During the 18th century, the ruins served as a refuge for a hermit. The castle's stones were gradually plundered, notably to build the surrounding houses. In 1889, the ruins of the castle were purchased by the Belgian state. Source: https://chateaumoha.be/histoire

The "Rocher du Château de Moha" is a limestone outcrop rising from the Mehaigne valley. It was a strategically important site in the Middle Ages, when more castles were built on rocks. This made the site difficult to besiege, and it was well-placed as a control point over the valley. The rock is very recognizable in the landscape. The ruins on the rock are still clearly visible, and the medieval structures are still easily recognizable.

The unique natural phenomenon of the Poudingue d’Ombret: a type of rock formed from deposits of river alluvium, approximately 395 million years old, with large stones surrounded by smaller sediments.