4.5
(617)
2,912
등산객
134
하이킹
정확한 경로를 찾는 것이 때로는 어렵지만 베르제메에서 하이킹을 하면 다양한 경치를 마음껏 감상할 수 있답니다. 베르제메에서 가장 멋진 하이킹과 워킹 중에서 마음에 드는 활동을 시작해보세요.
마지막 업데이트: 4월 2, 2026
4.5
(11)
50
등산객
10.4km
03:11
360m
360m
4.5
(8)
37
등산객
6.20km
01:41
80m
80m
초급용 하이킹. 모든 체력 수준에 적합. 실력과 관계없이 누구나 쉽게 갈 수 있는 길.
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5.0
(4)
34
등산객
5.01km
01:32
170m
170m
초급용 하이킹. 모든 체력 수준에 적합. 실력과 관계없이 누구나 쉽게 갈 수 있는 길.
5.0
(1)
20
등산객
11.1km
03:07
230m
230m
보통 하이킹. 좋은 체력 필요. 실력과 관계없이 누구나 쉽게 갈 수 있는 길.
4.8
(4)
16
등산객
13.6km
04:08
470m
470m
보통 하이킹. 좋은 체력 필요. 실력과 관계없이 누구나 쉽게 갈 수 있는 길.
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Road at the edge of the cliff. Remarkable view.
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Saint-Pons was one of the oldest and most important strongholds of the Barony of Aps. Located at the foot of the Coiron, the village was fortified from the 14th century. One can still imagine, depending on the shape of the town, the location of the defensive wall. It is possible to park on the street to go hiking.
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The chapel, nestled against a neck, was rebuilt at the end of the 19th century to fight against Phylloxera. The volcanic plateau of Coiron is an ancient massif since the lavas have been dated between 6 and 8 million years approximately. Strombolian cones have been seriously damaged by erosion. Some have been completely destroyed and we can only observe today the lower part of the chimney, in the form of large lava pellets, the necks or veins sometimes a kilometer long, the dykes.
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The Coiron plateau presents a typical landscape of natural meadows in bocage, maintained by breeders producing meat of recognized quality.
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The volcanic activity of Coiron has developed at the level of two types of buildings: Strombolian volcanoes and explosion craters called maars. The volcanic plateau of Coiron is an ancient massif since the lavas have been dated between 6 and 8 million years approximately. Strombolian cones have been seriously damaged by erosion. Some have been completely destroyed and today we can only observe the lower part of the chimney, in the form of large lava pellets, the necks (Sceautres, Roche Chérie...), or veins sometimes a kilometer long , the dykes. The basalt flows have a particular structure due to their cooling: the lower part is cut into prisms or organs.
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The start is in the wrong place (currently private land). It is better to continue for 100 meters on the Route de Villeneuve and park the car on the right in the residential area. here the route streets.
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This basaltic plateau was actually home to two castles, one on the eastern slope and the other on the western slope. The eastern castle has disappeared, leaving the tower of the western castle balanced on the edge of the rocky plateau.
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This basaltic plateau actually housed two castles, one on the eastern slope and the other on the western slope. The eastern castle has disappeared, leaving the tower of the western castle balanced on the edge of the rocky plateau.
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