가장 멋진 솜 자연유산 20곳

Site managed by the Conservatoire d'Espaces Naturels des Hauts de France (Hauts-de-France Regional Nature Reserve). A wide, stabilized gravel path, open to the public, is maintained and marked with signposts. Since 2012, an audio guide has allowed you to explore the nature reserve with a "virtual guide." QR codes placed along the path allow you to play the audio clips using your smartphone. This audio guide is available in three languages (French, English, and Dutch). https://www.cen-hautsdefrance.org/rnn-l-etang-saint-ladre

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Nice corner

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Nice view of the ponds and the villa "Les étangs".

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A gravel path. A bit monotonous and technically challenging to ride on a bike. Wide tires are essential, and suspension is helpful. The view is fantastic. The cliffs of Ault are in front of you, the sea is to your right, and the nature reserve (salt marshes) is to your left, with many seabirds, horses, and other wildlife.

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The Cratère de Lochnagar, an impressive war memorial, was created by a huge mine blown up by the British Royal Engineers on 1 July 1916, as part of the Battle of the Somme. The explosion marked the beginning of the battle and left a crater 90 metres in diameter and 25 metres deep. Interestingly, the crater was named after Lochnagar Street, the trench from which the tunnel was dug. The crater is now a preserved site of remembrance and a religious service is held there every year on 1 July in memory of those who died.

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

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

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The bay of summer, on our trip it was low tide.

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You need good shoes.

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Hike with the difficulty of the dunes but very nice and beautiful.

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😁

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.

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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.

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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.

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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.

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Great panorama, but also depressing how fleeting everything is.

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Beautiful chalk cliffs on the coastline

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Just off the road to Bapaume, is the site of the grand mine. At 7am on the 1st July 1916 the biggest explosion in history cause this hole o e of several that marked the start of the Battle of the Somme. Well worth a visit.

Very moving place of memory. Never forget 💮.

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Very beautiful here, breathtaking rocks

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