周辺の天然記念物・トップ20

Unfortunately, the bike path here is no longer paved. Still, the scenery is beautiful.

Googleによる翻訳•原文を表示

The cliffs are made of chalk and are impressive to look at.

Googleによる翻訳•原文を表示

Here in Ault begin the chalk cliffs, which stretch all the way to Normandy and repeatedly appear as enormous cliffs.

Googleによる翻訳•原文を表示

You need good shoes.

Googleによる翻訳•原文を表示

the rocks of the Gris-Nez are being loosened by rain and sea.

Googleによる翻訳•原文を表示

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.

Googleによる翻訳•原文を表示

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.

Googleによる翻訳•原文を表示

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.

Googleによる翻訳•原文を表示

Not passable by bike.

Googleによる翻訳•原文を表示

The rocks, with their cracks and small caves in the calcareous wall, provide an important nesting site for numerous bird species such as jackdaws, house martins, fulmars, kestrels, gulls, terns and herring gulls. As part of a renaturation project in 2006, a section of the asphalt road leading to the summit and the parking spaces there were completely removed. Instead, a parking lot about 300 meters inland was significantly expanded.

Googleによる翻訳•原文を表示

The obelisk crowns a 133-meter-high ensemble on a pedestal that can be seen from afar. It is THE landmark to reach to enjoy a 360° panorama from the top of the cliffs of Cap Blanc Nez. When the German army took possession of the Opal Coast in May 1940, this monument was immediately destroyed. The current Dover Patrol dates from the early 1960s. The last restoration took place in 2007. Source: https://www.calaisxxl.com/de/offres/a-voir-a-faire/monument-a-la-dover-patrol/

Googleによる翻訳•原文を表示

The Cap Blanc-Nez War Memorial (Dover Patrol Monument) is a major war memorial erected on the cliffs of Cap Blanc-Nez, near Sangatte. It honours the British naval forces and the Dover Patrol, a key unit of the Royal Navy that secured the Straits of Dover during the First and Second World Wars.

Googleによる翻訳•原文を表示

The Petit Blanc-Nez is a cliff in the Pas-de-Calais region and is part of the Deux-Caps (Two Capes) area, which also includes Cap Gris-Nez. Both are part of the protected area classified as a Grand Site de France and offer breathtaking views of the English Channel and, on a clear day, the English coast.

Googleによる翻訳•原文を表示

Incredibly beautiful paths - partly on wooden planks, partly through fine sand. A small, hidden natural paradise that can be wonderfully explored on a circular hike.

Googleによる翻訳•原文を表示

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.

Googleによる翻訳•原文を表示

Great panorama, but also depressing how fleeting everything is.

Googleによる翻訳•原文を表示

Beautiful chalk cliffs on the coastline

Googleによる翻訳•原文を表示

Very beautiful here, breathtaking rocks

Googleによる翻訳•原文を表示

The Dover Patrol was a Royal Navy command during World War I, whose main task was to prevent German ships, mainly submarines, from crossing the Channel into the Atlantic Ocean. It consisted of several naval ships and aircraft, and performed various tasks, including anti-submarine patrols, escorting ships, laying and clearing naval mines, and bombing German military positions. After the war, memorials were erected in memory of the Dover Patrol in various locations including Dover, Cap Blanc-Nez and New York.

Googleによる翻訳•原文を表示

Cap Blanc-Nez is an impressive cliff located in Escalles, Pas-de-Calais, France, rising to 134 meters above a rocky beach. It is the northernmost cliff in France, consisting of chalk and marl. It offers a strategic vantage point from which on a clear day you can see the cliffs of Dover on the English coast. The area supports a unique grassland and is a popular destination for tourists and hikers. It is part of the Grand Site des Deux Caps, together with Cap Gris-Nez, and attracts 2.5 million visitors annually. It also has historical significance, with remains from the Second World War still visible.

Googleによる翻訳•原文を表示