Nottonville — Wikipédia

Nottonville is a French commune located in the department of Eure-et-Loir in the Center-Val de Loire region.

Situation [ modifier | Modifier and code ]

The town is crossed by the Conie, tributary of the Loir. Two arms meet in Notvil: La Conie Haute which comes from the town of Varize and La Conie Basse who goes through the locality Pontault then by La Chenardière Towards Courbehaye.

Then it takes its course by crossing an extent called The spoy goure , then the Raffaults to the place called Vallors Before going through the commune of Conie-Molitard. Basse conie is a resurgence of the Beauce tablecloth, it once spread out in a swamp towards the woods of La Chenardière . The current bed was dug by hand, between the two wars in order to eradicate mosquitoes and protect seasonal agricultural workers.

Neighboring municipalities [ modifier | Modifier and code ]

Hams and Lieces [ modifier | Modifier and code ]

Remarkable Sequoia, hamlet of wood.

• Wood ;
• Pontault ;
• Réclainville ;
• Rescue.

Hydrography [ modifier | Modifier and code ]

Spoy goure [ modifier | Modifier and code ]

La Goure (or the Gour) of Spoy is located in the town of Nottonville, south of the Spoy Ferme. It is a deep basin of 8 to 10 meters where it seems that the upstream waters of the two valleys of the Conies gather in a sort of reservoir.

The name is taken from the association of that of the Spoy Farm, a gap of the neighboring town of Civry, and “goure”, which can be criticized for “gouffre” ^{[ first ] [Ref. incomplete]} .

If the two Conies Amonts (the Conie du Sud or Conie’s Varia , and the Conie du Nord or Rau la Conie , Resurgences of the Beauce tablecloth) are intermittent, it is only from the spy goure that the conie is sustainable, and then completely deserves the name of the pongue river of the Loir.
We deduce that the goure is also supplied underground by a third local underground source, which ensures the sustainability of downstream flow ^{[ 2 ]} .

Climate [ modifier | Modifier and code ]

The climate that characterizes the municipality was qualified, in 2010, as “degraded oceanic climate of the plains of the center and the North”, according to the typology of the climates of France which then has eight main types of climates in metropolitan France ^{[ 3 ]} . In 2020, the municipality came out of the type “altered ocean climate” in the classification established by Météo-France, which now only has, at first glance, only five main types of climates in mainland France. It is a transitional area between the oceanic climate, the mountain climate and the semi-continental climate. The temperature differences between winter and summer increase with the removal of the sea. The rainfall is lower than in the sea, except near the reliefs ^{[ 4 ]} .

The climatic parameters which made it possible to establish the typology of 2010 have six variables for temperatures and eight for precipitation, whose values ​​correspond to the monthly data on normal 1971-2000 ^{[ Note 1 ]} . The seven main variables characterizing the municipality are presented in the box below.

With climate change, these variables have evolved. A study carried out in 2014 by the Directorate General of Energy and Climate ^{[ 7 ]} supplemented by regional studies ^{[ 8 ]} provides indeed that the average temperature should grow and the average rainfall is lower, with high regional variations. These changes can be noted on the nearest Météo-France weather station, “Pre-Saint-Evroult”, in the town of Pré-Saint-Évroult, commissioned in 1995 ^{[ 9 ]} and which is at 9 km as the crow flies ^{[ ten ] , [ Note 4 ]} , where the average annual temperature is 11.1 °C and the precipitation height of 597.4 mm For the period 1981-2010 ^{[ 11 ]} .
On the nearest historic weather station ^{[ Note 5 ]} , “Châteaudun”, in the town of Jallans, commissioned in 1952 and 11 km ^{[ twelfth ]} , the average annual temperature evolves from 10.6 °C For the period 1971-2000 ^{[ 13 ]} To 11.1 °C For 1981-2010 ^{[ 14 ]} , then 11.5 °C For 1991-2020 ^{[ 15 ]} .

Typology [ modifier | Modifier and code ]

Nottonville is a rural commune, because it is one of the not very little dense municipalities, within the meaning of the municipal density grid of INSEE ^{[ Note 6 ] , [ 16 ] , [ 17 ] , [ 18 ]} .
The municipality is also outside the attraction of cities ^{[ 19 ] , [ 20 ]} .

Land use [ modifier | Modifier and code ]

Map of infrastructure and land use of the municipality in 2018 (CLC).

The land use of the municipality, as it emerges from the European Biophysical Occupation Database of Corine Land Cover (CLC), is marked by the importance of agricultural territories (88.3% in 2018) , a proportion identical to that of 1990 (88.4%). The detailed distribution in 2018 is as follows:
Arable lands (88.3%), forests (6.4%), interior wetlands (5.2%) ^{[ 21 ]} .

The IGN also provides an online tool to compare the evolution over time of the soil occupation of the municipality (or territories to different scales). Several eras are accessible in the form of aerial cards or photos: the Cassini card ( XVIII ^{It is} century), the staff map (1820-1866) and the current period (1950 to today) ^{[ Card 1 ]} .

Major risks [ modifier | Modifier and code ]

The territory of the commune of Nottonville is vulnerable to different natural vagaries: meteorological (storm, thunderstorm, snow, very cold, heat wave or drought), floods, ground movements and earthquake (very low seismicity). It is also exposed to a technological risk, the transport of dangerous materials ^{[ 22 ]} . A site published by the BRGM makes it possible to simply and quickly assess the risks of a property located either by your address or by the number of its plot ^{[ 23 ]} .

Natural risks [ modifier | Modifier and code ]

Certain parts of the municipal territory are likely to be affected by the risk of flooding by overflowing watercourse, in particular conie and conie. The municipality was recognized as a natural disaster under damage caused by floods and mudslides that occurred in 1999 and 2013 ^{[ 24 ] , [ 22 ]} .

Map of the Alea Retraction-Backlin areas of the clay soils of Nottonville.

The movements of land likely to occur in the town are sags and collapses linked to the underground cavities ^{[ 25 ]} . The national inventory of underground cavities makes it possible to locate those located in the town ^{[ 26 ]} .

Removing clay soils is likely to cause significant damage to buildings in the event of alternating periods of drought and rain. 36.6% of the municipal area is in medium or strong hazard (52.8% at the departmental level and 48.5% at the national level). Of the 196 buildings counted in the town in 2019, 149 are in Middle or strong hazard, 76%, to be compared to 70% at the departmental level and 54% at the national level. A mapping of the national territory exhibition to the swelling of the clay soils is available on the BRGM website ^{[ 27 ] , [ Card 2 ]} .

Regarding land movements, the municipality was recognized as a natural disaster under damage caused by field movements in 1999 ^{[ 22 ]} .

Technological risks [ modifier | Modifier and code ]

The risk of transporting dangerous materials in the town is linked to its crossing by significant road or rail infrastructures or the presence of a hydrocarbon transport pipe. An accident occurring on such infrastructure is indeed likely to have serious effects to the frame or to people up to 350 m , depending on the nature of the material transported. Town planning provisions can be recommended accordingly ^{[ 28 ]} .

The name of the locality is attested in the forms Villa Nantonensis And Nantona villa In 1080, Nantonville In 1178, Nothonville In 1736 ^{[ 29 ]} .

You base Latin Nantul bottom , With , name of a person of Gallic origin, and villa , “Rural domain”. According to the form Nantona villa of 1080.

In 1890, the hamlet of Pontault underwent an important fire. The claim destroys the locality and made several victims ^{[ 30 ]} .

List of mayors [ modifier | Modifier and code ]

Environmental policy [ modifier | Modifier and code ]

Demography [ modifier | Modifier and code ]

The evolution of the number of inhabitants is known through the population censuses made in the municipality since 1793. From 2006, the legal populations of the municipalities are published annually by INSEE. The census is now based on an annual information collection, successively concerning all the municipal territories during a period of five years. For municipalities with less than 10,000 inhabitants, a census survey relating to the entire population is carried out every five years, the legal populations of the intermediate years being estimated by interpolation or extrapolation ^{[ thirty first ]} . For the municipality, the first exhaustive census falling within the framework of the new system was carried out in 2005 ^{[ 32 ]} .

In 2020, the town had 283 inhabitants ^{[ Note 7 ]} , decreased by 10.44%compared to 2014 (Eure-et-Loir: −0.53%, France excluding Mayotte: +1.9%).

Histogram of demographic evolution

Education [ modifier | Modifier and code ]

Cultural manifestations and festivities [ modifier | Modifier and code ]

Stores-t- rideaux.com is a French online commerce SME, created in 2011 in Nottonville.

Places and monuments [ modifier | Modifier and code ]

Former wood abbey [ modifier | Modifier and code ]

The old wood abbey, Classified MH (1988) ^{[ 35 ]} , is a priory, the only attested construction, fortified by X ^{It is} century located at the exit of the place called wood towards the place called Vallors . It has a door framed by two towers with loopholes and a trace of Pont-Levis, as well as a massive oak door, recently restored.

It was built by the monks of Marmoutier who established, on the remains of a Carolingian period residence, a priory from the XI ^{It is} Siècle. Le Logis Prioral Date Du XV ^{It is} century and includes an inverted boat frame.

In the courtyard there is a large dovecote, revealing the richness of the domain of monks (the number of authorized nests was dependent on the extent of the domain). The house would have served as a tithe barn.

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• 
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  The Abbey, from Villiers-Saint-Orien.

Brush castle [ modifier | Modifier and code ]

The Château de la Brosse.

The Château de la Brosse, Registered MH (1990) ^{[ 36 ]} , dated XVII ^{It is} century, but burned at XIX ^{It is} century.

The commons, the courtyard and a turret remain the only vintage vestiges of this castle.

Saint-Pierre church [ modifier | Modifier and code ]

The Saint-Pierre church, on the other hand XIV ^{It is} century. It is located in Nottonville even opposite the town hall. Its frame in frame of XVII ^{It is} century was restored following the 1999 storm.

Site Castral of Nottonville [ modifier | Modifier and code ]

A powerfully fortified castle of the Viscount of Chartres, the main element of which was a quadrangular quadranged dungeon-turn of about twenty meters, of which only the foundations remain, to which is attached to an elevation building still in elevation. Logis with single-storey rooms ^{[ 37 ]} .

Megaliths [ modifier | Modifier and code ]

Dolmen du Pallet de Garangua.

• Dolmen collapsed says Gargantua Palet On the road between Pontault and the Château de la Brosse.
• Dolmens and polishers between Wood And Vallors .
• Polish (moved) says of La Pierre Saint Martin in front of the farm of The natterie .

Rouche houses [ modifier | Modifier and code ]

• Many houses in rouche (Local reed), especially along rue des Chaumières in front of the church. Previously, the reedlières were widely exploited. From this past, testifies to the presence in the town of a fabric factory, today in fabric and mechanical.

Personalities linked to the municipality [ modifier | Modifier and code ]

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external links [ modifier | Modifier and code ]

Notes and cards [ modifier | Modifier and code ]

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Cards [ modifier | Modifier and code ]

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