Périgny, Charente-Maritime

Clavette (French pronunciation: ​[klavɛt]) is a commune in the Charente-Maritime in the department in the Nouvelle-Aquitaine region in southwestern France.

Montroy (French pronunciation: ​[mɔ̃ʁwa]) is a commune in the Charente-Maritime in the department in the Nouvelle-Aquitaine region in southwestern France.

Saint-Rogatien (French pronunciation: ​[sɛ̃ ʁɔɡasjɛ̃]) is a commune in the Charente-Maritime department in the Nouvelle-Aquitaine region in southwestern France.Besides the town, the town includes the area of Casse-Mortier and part of the village Pommerou, shared with the town of Clavette. Its inhabitants are called Rogatiens and Rogatiennes.

Aytré (French pronunciation: ​[ɛtʁe]) is a commune in the Charente-Maritime department, Nouvelle-Aquitaine, southwestern France. Aytré is especially known for its long beach, which is easily accessible from neighbouring La Rochelle, or Les Minimes. The beach is flat and shallow, making it a good bathing spot for children, and an excellent spot for windsurfing. The historian Jean Prasteau (1921–1997) was born in Aytré, as was Jean Desaguliers, a Protestant pastor, and father of John Theophilus Desaguliers.

The Abbey of Saint-Léonard des Chaumes (Latin: Sanctus Leonardus de Calmis) was a Cistercian monastery in Dompierre-sur-Mer in the province of Aunis in the Kingdom of France. It was destroyed in the 18th century.

La Jarne (French pronunciation: ​[la ʒaʁn]) is a commune in the Charente-Maritime department in southwestern France. It is 7 km southeast of the city of La Rochelle.

The Canal de Marans à La Rochelle, also known as Canal de Marans, Canal de Rompsay (French pronunciation: ​[kanal də ʁɔ̃se]) or Canal de La Rochelle depending on the location, is a French canal in the Charente-Maritime department connecting the city of La Rochelle with the town of Marans. It also connects the river of the Sèvre Niortaise to the harbour at La Rochelle. The canal goes through the communes of Dompierre-sur-Mer, Andilly and Sainte-Soulle. It is 24.5 km long, with 4 locks, and has a total level change of 1.7 m. It has a width of 5.2 m. The canal was built in the 19th century in order to foster trade between the two cities. It was part of a great project of a North-South canal connecting the river Loire to the Adour. The project was ordered by imperial decision of Napoleon I on July 17, 1805, with the objective of connecting Niort with La Rochelle. It was started in 1806, but only open in 1875, and only reached La Rochelle in 1888. It was built with the forced labour of prisoners. When it was completed however, the advent of the train (with the establishment of a track between Nantes and La Rochelle) meant that the canal fell into disuse. Navigation on the canal was totally stopped after the Second World War. It is today not navigable. Today the canal allows for picturesque walks between the two cities. It is renowned for its flora and fauna. The waters of the canal discharge into the Maubec reservoir at La Rochelle, just before the tidal bassin, and its waters contribute to scour the harbour and navigable channels.

Puilboreau (French pronunciation: ​[pɥilbɔʁo]) is a commune in the Charente-Maritime department in southwestern France. Its residents are called Puilborains (male) and Puilboraines (female).

Dompierre-sur-Mer (French pronunciation: ​[dɔ̃pjɛʁ syʁ mɛʁ], literally Dompierre on Sea) is a commune in the Charente-Maritime department, southwestern France.

Angoulins (French pronunciation: ​[ɑ̃ɡulɛ̃]) is a commune in the Charente-Maritime department in the Nouvelle-Aquitaine region of southwestern France. The inhabitants of the commune are known as Angoulinois or Angoulinoises.

Salles-sur-Mer (French pronunciation: ​[sal syʁ mɛʁ]) is a commune in the Charente-Maritime department, region of Nouvelle-Aquitaine (formerly Poitou-Charentes), southwestern France.

La Pointe du Chay is a limestone promontory, about 5 kilometres from La Rochelle, France, between the seafront of Aytré and Angoulins. La Pointe du Chay is composed of layers of limestone dating back to the Sequanian stage (upper Oxfordian stage) of the Jurassic period (circa 160 million years ago), when a large part of France was submerged. These rocks were formed by the accumulation of organisms falling on the seabed, where they solidified. This happened at the time dinosaurs were roaming the earth. Many of these layers are especially visible and easily accessible at La Pointe du Chay, in which are encapsulated many small marine fossils. Layers of thick white rocks, formed during period of relatively warm seas, alternate with highly friable layers containing sands and remains of mud, formed during colder periods, and with layers containing various corals, that were formed during warmer, tropical times.