Angoulins | ||
---|---|---|
Seashore at Angoulins
|
||
|
||
Coordinates: 46°06′18″N 1°06′31″W / 46.105°N 1.108611°WCoordinates: 46°06′18″N 1°06′31″W / 46.105°N 1.108611°W | ||
Country | France | |
Region | Nouvelle-Aquitaine | |
Department | Charente-Maritime | |
Arrondissement | La Rochelle | |
Canton | Châtelaillon-Plage | |
Intercommunality | La Rochelle | |
Government | ||
• Mayor (2014-2020) | Daniel Vailleau | |
Area1 | 7.86 km2 (3.03 sq mi) | |
Population (2014)2 | 3,800 | |
• Density | 480/km2 (1,300/sq mi) | |
Time zone | CET (UTC+1) | |
• Summer (DST) | CEST (UTC+2) | |
INSEE/Postal code | 17010 /17690 | |
Elevation | 0–17 m (0–56 ft) (avg. 4 m or 13 ft) |
|
1 French Land Register data, which excludes lakes, ponds, glaciers > 1 km² (0.386 sq mi or 247 acres) and river estuaries. 2Population without double counting: residents of multiple communes (e.g., students and military personnel) only counted once. |
1 French Land Register data, which excludes lakes, ponds, glaciers > 1 km² (0.386 sq mi or 247 acres) and river estuaries.
Angoulins 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
Angoulins is located in the northwest of the department of Charente-Maritime some 8 km south-east of La Rochelle and 5 km north of Châtelaillon-Plage in the former province of Aunis. It is a coastal commune on the Atlantic ocean. Access is by the E602 (D137) highway from La Rochelle continuing south-east with an exit in the commune just east of Angoulins town. There is also the D202 from Salles-sur-Mer in the east turning south and continuing to Chatelaillon-Plage. Access to the town is by the D111E1 from the D202 on the southern border continuing through the town and turning east to the motorway exit.
Angoulins town has a large urban area occupying almost 50% of the commune with farmland to the north, east, and west.
The entire commune is located on Jurassic terrain which completely covers the plain of Aunis. Jurassic Marl and limestone outcrops appear on the surface of the commune and the relief is slightly rolling.
The coastal strip of Angoulins, which corresponds to the last extremity of the plain of Aunis, is relatively varied. It alternates between low sandy and marshy shores and high limestone cliffs.
Low-lying coasts, which were formerly salt marshes, have today been transformed into oyster beds (at the marsh north of Chay Point) and are derived from Quaternary sedimentary deposits of marine origin - from the last Flandrian transgression. The sandy coast is situated in a small cove formed naturally by the phenomena of marine erosion and ocean currents (Angoulins beach, south of the Chay point).