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Roof of the Jarnioux castle, Rhône, France (45°58’ N, 4°38’ E).Buren’s Columns, the Palais-Royal, Paris, France (48°52’ N, 2°20’ E). Loisinord ski slope on a slagheap at Nœux-les-Mines, France (50°28’ N, 2°41’ E).
Village of Ramatuelle, Var, France (43°13’ N, 6°37’ E).Flock of sheep in the bay of the Somme, France (50°13’ N, 1°40’ E).House and lake near Bulat Pestivien, Côtes d’Armor, Brittany, France (48°26’ N, 3°18’ W).
House «Heart» in Sables d’Or les Pins, Fréhel, Côtes-dScrap yard, Saint-Brieuc, Côtes-d’Armor, France (48°31’ N, 2°46’ W). Mussel farming in the Bay of Saint-Brieuc, Côtes d’Armor, France (48°30’ N - 2°46’ W).
Bocage landscape, Côtes d’Armor, France (48°35’ N, 2°19’ W).Marina at Port Camargue, Gard, France (43°31’ N, 4°08’ E).Saint Vidian church in Martres-Tolosane, Haute-Garonne, France (43°12’ N, 1°01’ E).
Saint Sernin basilica, Toulouse, Haute-Garonne, France (43°37’ N, 1°27’ E).Birds Island (L’île aux Oiseaux), Arcachon Bay, Gironde, France (44°41’ N, 1°10’ W).Nature reserve, Aguin bank, Gironde, France (44°39’ N, 1°15’ W).
The Great Dune of Pilat, Gironde, France (44°36’ N – 1°12’ W).  Pig on a farm, Brionne, Eure, France (49°12’ N – 0°43’ E). Hunting in vineyards near Nantes, Loire-Atlantique, France (47°22’ N - 1°11’ W).
Orléans Cathedral, Loiret, France (47°54’ N, 1°54’ E).Village of Loire Valley in fog, Loire-Atlantique, France (47°21’ N, 1°25’ W).The Chausey Islands at low water, Manche, France (48°52’ N, 1°50’ W).
Low tide in the Gulf of Morbihan, Morbihan, France (47°34’ N, 2°49’ W). Sailing ships in the port of Argol, Hœdic Island, Morbihan, France (47°21’ N - 2°52’ W).Gulf of Murtoli, Corsica, France (41°30’ N – 8° 54’ E).
Oyster farming in Island of Oleron, Charente-Maritime, France (45°54’ N, 1°13’ W).Village of Talmont sur Gironde, Charente-Maritime, France (45°32’ N, 0°54’ W).Oyster beds in La Tremblade, Charente-Maritime, France (45°45’ N, 1°02’ W).




Low tide in the Gulf of Morbihan, Morbihan, France (47°34’ N, 2°49’ W).

These exposed mudflats hold in their grip the sailing boats left abandoned by the tide. The tides are the main agent in the Gulf of Morbihan’s geomorphology, constantly reshaping this inland sea, which is 12.4 miles long (20 km) and almost as wide. The cyclical variation in the level of the oceans is due to the gravitational pull of heavenly bodies. Since the moon is the nearest, it is chiefly responsible for moving vast masses of water. But when the moon and sun are in alignment, the phenomenon is greatly accentuated, producing extreme tidal movements. In the Gulf of Morbihan, tidal flows are slowed down by the second-biggest bed of sea wrack in France. This aquatic plant helps to feed the 130,000 or so birds that spend the winter here. This richness has led to the site’s listing under the Ramsar Convention, which covers wetlands of international importance.

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