Banon, Alpes-de-Haute-Provence
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The village of Banon
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 Banon
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Location within Provence-A.-C.d'A. region
Banon
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| Coordinates: 44°02′20″N 5°37′43″E / 44.0389°N 5.6286°ECoordinates: 44°02′20″N 5°37′43″E / 44.0389°N 5.6286°E | ||
| Country | France | |
| Region | Provence-Alpes-Côte d'Azur | |
| Department | Alpes-de-Haute-Provence | |
| Arrondissement | Forcalquier | |
| Canton | Reillanne | |
| Intercommunality | Pays de Banon | |
| Government | ||
| • Mayor (2014–2020) | Philippe Wagner | |
| Area1 | 39.81 km2 (15.37 sq mi) | |
| Population (2010)2 | 1,070 | |
| • Density | 27/km2 (70/sq mi) | |
| Time zone | CET (UTC+1) | |
| • Summer (DST) | CEST (UTC+2) | |
| INSEE/Postal code | 04018 /04150 | |
| Elevation | 540–1,093 m (1,772–3,586 ft) (avg. 760 m or 2,490 ft) |
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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. |
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1 French Land Register data, which excludes lakes, ponds, glaciers > 1 km² (0.386 sq mi or 247 acres) and river estuaries.
Banon is a commune in the department of Alpes-de-Haute-Provence in the Provence-Alpes-Côte d'Azur region of south-eastern France.
The inhabitants of the commune are known as Banonais or Banonaises.
Banon is located next to the Plateau of Albion some 15 km north-west of Forcalquier, 50 km east of Carpentras, and 760 m above sea level. The village is on a hill overlooking the Coulon valley. Access to the commune is by the D950 road from Revest-du-Bion in the north-west which passes through the village and continues south-east to Limans. The D51 goes south-west from the village to Simiane-la-Rotonde. The D5 goes south-east to Revest-des-Brousses. The D12 goes north from the D950 and loops around to join the D950 again east of the commune. Apart from the village there are the hamlets of L'Adret, L'Adrech, and Le Serre. The commune is farmland on the lower areas to the west and forested on the heights in the east.
Limestone, dating from the Cretaceous period, is the predominant rock in the commune although in the Riaille valley it is Barremian limestone. The limestone is used for construction, especially for wall ties, framing, and lower walls, as well as for fountains. Depressions, oriented SSW-NNE and NNW-SSE are formed of marl and sandstone from the Upper Cretaceous period. Limestones and porous rocks allow water to infiltrate down to a substrate of Neocomian marl. These infiltrations scour the rocks causing the formation of sinkholes or Avens (Pitches) such as the Aven of Belette. The waters circulate at a speed of 77 metres/hour.
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