프리빌-에스카보틴 주변 최고의 사이클링 경로
4.3
(981)
6,366
자전거 타는 사람
185
라이딩
프리빌-에스카보틴 최고의 사이클링 경로를 따라 지역을 둘러볼까요? 프리빌-에스카보틴에서 가장 멋진 자전거 라이딩 장소 중에서 가장 마음에 드는 라이딩을 선택해보세요.
마지막 업데이트: 3월 1, 2026
4.6
(7)
42
자전거 타는 사람
33.5km
02:02
120m
120m
보통 자전거 타기. 좋은 체력 필요. 대부분 포장된 지면. 실력과 관계없이 누구나 갈 수 있음.
23
자전거 타는 사람
51.5km
03:17
460m
460m
어려운 자전거 타기. 우수한 체력 필요. 대부분 포장된 지면. 실력과 관계없이 누구나 갈 수 있음.
무료 회원 가입
9
자전거 타는 사람
51.4km
03:32
500m
500m
어려운 자전거 타기. 우수한 체력 필요. 대부분 포장된 지면. 실력과 관계없이 누구나 갈 수 있음.
5.0
(2)
7
자전거 타는 사람
27.3km
01:40
180m
180m
보통 자전거 타기. 좋은 체력 필요. 대부분 포장된 지면. 실력과 관계없이 누구나 갈 수 있음.
2
자전거 타는 사람
16.6km
01:02
130m
130m
초급용 자전거 라이딩. 모든 체력 수준에 적합. 대부분 포장된 지면. 실력과 관계없이 누구나 갈 수 있음.
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The church in Ault is a beautiful building. Its interior is simple yet beautiful.
•3
0
The cliffs are made of chalk and are impressive to look at.
•3
0
Here in Ault begin the chalk cliffs, which stretch all the way to Normandy and repeatedly appear as enormous cliffs.
•4
0
The cliffs around the beach of Ault are composed of chalk from the Upper Cretaceous, more precisely from the Turonian and Coniacian (around 83 million years ago to 90 million years ago). They are strewn with flint nodules which highlight the subhorizontal stratification planes (the formation of flint has already been discussed in Discovery of the geology of the cliffs of Étretat, presentation of an excursion from the beach of Tilleul (Antifer) to the Porte d'Amont (Étretat Nord)). The relative proportion of chalk and flint is around 90-95% chalk to 5-10% flint. Flint horizons are stratigraphic markers. On the cliffs of Ault, the regular flint band called Seven Sisters is recognizable and characterizes the boundary between the Middle Coniacian and the Upper Coniacian (around 87 million years ago). The boundary between the lower and middle Coniacian is marked by the Shoreham 2 marl level, which is more difficult to identify. These lithostratigraphic markings allow in particular the correlation of distant deposits, such as between the Normandy and Picardy coasts, or between the French and English coasts.
•3
0
The cliffs around the beach of Ault are composed of chalk from the Upper Cretaceous, more precisely from the Turonian and Coniacian (around 83 million years ago to 90 million years ago). They are strewn with flint nodules which highlight the subhorizontal stratification planes (the formation of flint has already been discussed in Discovery of the geology of the cliffs of Étretat, presentation of an excursion from the beach of Tilleul (Antifer) to the Porte d'Amont (Étretat Nord)). The relative proportion of chalk and flint is around 90-95% chalk to 5-10% flint. Flint horizons are stratigraphic markers. On the cliffs of Ault, the regular flint band called Seven Sisters is recognizable and characterizes the boundary between the Middle Coniacian and the Upper Coniacian (around 87 million years ago). The boundary between the lower and middle Coniacian is marked by the Shoreham 2 marl level, which is more difficult to identify. These lithostratigraphic markings allow in particular the correlation of distant deposits, such as between the Normandy and Picardy coasts, or between the French and English coasts.
•2
0
Great swimming and surfing beach. Small town with lots going on.
•1
0
Ault is a beautiful place. Beautifully laid out paths above and below the impressive cliffs. The town center is perfect for relaxing. There are a few cafes and bistros for when you get a little hungry. There are benches everywhere where you can sit and enjoy a few minutes of peace and the wonderful views.
•1
0
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