Banon () is a commune in the department of Alpes-de-Haute-Provence in the Provence-Alpes-Côte d'Azur region of south-eastern France.
Geography
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.Google Maps
Geology 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.
Relief
Summits The Croue de Bane or Grou de Banc (1092 m) The Crête de Gamby (Gamby peak) (883 m)
Hydrography
The Ravin du Calavon rises just east of the village and flows south, becoming the Calavon river (also known as the Coulon), which eventually joins the Durance south-east of Cabannes. The Riaille river flows south through the western side of the commune and the village before joining the Calavon south of the commune. The Largue flows from the north down the eastern side of the commune and continues south to join the Durance east of Manosque.
Environment The commune has 2,271 hectares of woods and forests.
Climate Banon is located in Alpes-de-Haute-Provence and enjoys an interior Mediterranean climate with summers hot and dry but the winters are cool and marked by frequent frosts. The annual average temperature is 12.8 °C with an average maximum of 22.4 °C and an average minimum of 0 °C. The highest maximum and minimum temperatures are 30 °C in July and 0 °C in December and January. Average sunshine hours are 2,755 hours per year with a peak of 343 hours in July. Another important characteristic of the Mediterranean climate is the rainfall which totals 426 millimetres over the year, unevenly distributed with a little more than 21 millimetres in July and more than 54 millimetres in October. The mistral blows sometimes although the town is sheltered by the Lure mountain. It may be more exposed to the Levant or the Sirocco which rarely occur.
The nearest weather station to Banon is in Saint-Christol in Vaucluse, a little farther away than Forcalquier.Météo-France, Network of stations in the South-East , Climatic, consulted on 11 March 2013
Natural and technological risks None of the 200 communes in the department are in a no seismic risk zone. Banon is in zone 1a (very low risk but not negligible) according to the deterministic classification of 1991 based on the historical earthquakes, and zone 3 (moderate risk) according to the EC8 probabilistic classification of 2011. Banon is also exposed to three other natural hazards: forest fire, flood, landslide.
Banon is not exposed to any risk of technological origin identified by the Prefecture.
There is no risk prevention plan for foreseeable natural risks (PPR) for the commune and there is no DICRIM.
Transport network Several bus lines connect Banon to other communes in the region. The places served are: Apt, Forcalquier, Digne-les-Bains, Avignon, and Manosque. There is also a bus service on market days (Tuesdays) to neighbouring communes.
The nearest airport and railway station are at Avignon.
Toponymy
The area appears for the first time in texts from the 11th century (castrum Banonni). According to Charles Rostaing the name is formed from the oronymic root Ban meaning "horn" or "point". According to this author the name predates the Gauls. This explanation is also shared by Fénié and Claude Martel, for whom this explanation also applies to Grou de Bane. According to Ernest Nègre, Banon comes from a Germanic proper name Bano.Ernest Nègre, General Toponymy of France, Librairie Droz, 1990, 708 pages, p. 828,
Banon in Vivaro-Alpine dialect and in Provençal dialect is said and written Banon in the classical norm and Banoun in the Mistralian norm.
Three main factors explain the toponymy of the commune: the relief between the Albion plateau and the Lure mountain, its location in the Occitan linguistic area, and the people of the area. The terrain is very present: the Pié d'Enroux is formed from a local evolution of the Latin podium meaning "height". The pey in Peymian has the same origin, the name of this hill meaning "the mountain of the middle". The name of the Puy de Salve is formed from the most current evolution in France of podium and there is also the Crête de Gamby (Gamby Ridge). The Coueste Chaude (to the west of the village) is on the slope of a mountain, Occitan derived from the French côte. Other names are formed from the words adret (sunny side of a mountain) and ubac (shady side): thus there are the Adret and the Ubac of Grou de Ban, the hamlet of Adrech at the foot of the Grou, and the Ubac farm at the foot of the Pié d'Enroux. The Combe de Vaux is a pleonastic doublet to designate a valley.
The work of hydraulic erosion on limestone has created avens (sinkholes) including at least one with a specific name: the Aven de Goutin. Amplified by deforestation, the same erosion moves large quantities of stones from the mountain slopes and deposits them on the plains, sometimes covering arable land: this is the origin of the name of Gravières south of the village.
The relatively high flat arable areas are called plains even though they are on a mountain: this name is used in Plaines (at the northern border of the commune) and in the hamlet of Plaines (in ruins) on the southern boundary (as well as these there is the toponym le Nord des Plaines). Le Plan is also a small plain.
Water is also present in the toponymy: there is the water source called Font des Petits and a marshy area called La Palud. A valley is named Aiguebelle meaning "beautiful water". The reference to water is rare in the toponymy of this dry region.
The term grange (barn) in this area refers to an isolated farm: this toponym is present in La Grange (at the northern border of the commune), also at La Grange (outside the village), and in Les Granges de Dauban. The hill overlooking the village is called Le Défens: this is an area, owned by the lord or the community, where herds were banned. Le Clos de Gardon is a cultivable area where the material from road ballasting was used to enclose the fields and meadows with a dry stone wall. Les Chastellas was a fortification at high altitude (which has been confirmed by excavations, see below) and La Tuilerie was a tile production workshop prior to the 18th century (before the term tuilière was used).
History
Prehistory and Antiquity The commune had inhabitants in prehistoric times: the discoveries of Paleolithic remains are quite numerous.
There are two oppida at Mures and Chastellard. At Font-Crémat, a Gallo-Roman villa and a necropolis have been discovered. A treasure of 700 denarii from Nero to Geta was discovered in a vase in 1909 as well as many other unrelated discoveries. During the Pax Romana the iron manufacturing workshops became established in the commune territory. Throughout this period the territory of Banon was part of that of the Sogiontiques (Sogionti) whose territory spanned south of the Baronnies of the Durance. The Sogiontiques were federated to the Vocontii and, after the Gallic Wars, they were attached with them to the Roman province of Gallia Narbonensis (now Narbonne). In the 2nd century they were detached from Voconces and formed a distinct civitas with Segustero (Sisteron) as its capital.
Romanisation can be seen in places such as the villas of Fouent-Crema: there were several houses and workshops or a Gallo-Roman hamlet settled on the plains north-east of Banon in the 1st and 2nd centuries AD. At the time of the Roman Crisis of the Third Century the whole area was burned (about 240-275). The people did not desert the commune as the site was occupied again in the 4th century before abandonment at the end of that century at the same time as the Chastelard de Lardiers nearby.Mariacristina Varano, Religious and Political areas in Provençal country in the Middle Ages (9th-13th centuries). The example of Forcalquier and its region, Thesis defended at the University of Aix-Marseille I, 2011, p. 73-74, 76, 150 The area then became a necropolis and the location of the inhabitants for this period has not been determined either in the immediate vicinity or on the heights.
While the south-east of Gaul was Burgundian land, the king of the Ostrogoths, Theodoric the Great, conquered the region between the Durance and the Rhône as well as Isère in 510. The commune depended briefly on Italy until 526. In order to reconcile with the Burgundian king Godomar III, the Ostrogoth Regent Amalasuntha gave him the territory.
Middle Ages While Chastelard was abandoned, there remained a visual (in the landscape) and symbolic (in attitudes) cue in that the border with the neighbouring community of Lardiers was fixed along the side of the oppidum in a process that seemed common.
The village was fortified in the 11th century (it was the castrum banonum in the charters of the time). During the Middle Ages the Church of Our Lady depended on the Abbey of Cruis who received the income attached to this church as well as those of the Chapel of Saint-Hilaire (disappeared) and returned it to Sénanque Abbey.
The fief of Simiane (from the 12th century to the 1789 revolution) was devastated by Raimond de Turenne in 1391. The Banon community was then within the viguerie of Forcalquier.
Modern times
A fair was held at Banon until the 18th century.
There was a windmill in Banon (probably after the 17th century). Its ruins are located near the Clos de Gardon.
French Revolution During the French Revolution the commune had a patriotic society which was founded after the end of 1792. The medieval castle was razed during the Revolution.
Contemporary Era The French coup d'état of 1851 committed by Louis-Napoléon Bonaparte against the French Second Republic provoked an armed uprising in the lower Alps in defence of the Constitution. After the failure of the insurrection severe repression continued against those who defended the Republic: 17 inhabitants of Banon were brought before the Joint Committee and the majority were sentenced to exile in Algeria.Henri Joannet, Jean-Pierre Pinatel, "Arrests-condemnations", 1851-For Memoir, Les Mées: The Friends of Mées, 2001, p. 71.
As with many communes in the department, Banon adopted schools well before the Jules Ferry laws. The scattered settlements led to doubling of the facilities with, in 1863, two schools installed in the main town and the village of Largue at the east and west extremities of the commune. These schools provided primary education for boys and girls: the Falloux Laws (1851) required the opening of a girls' school in communes with more than 800 inhabitants. The commune benefited from grants from the second Duruy Law (1877) to rebuild the Largue village school and to build a new one at Granges de Dauban.