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Monts D'Arrée
The Monts d'Arrée, or Menezioù Are in Breton, are an ancient mountain range in western Brittany which forms part of the Armorican massif. Historically it marked the border of the regions of Cornouaille and Léon Leon, Léon (French) or León (Spanish) may refer to: Places Europe * León, Spain, capital city of the Province of León * Province of León, Spain * Kingdom of León, an independent state in the Iberian Peninsula from 910 to 1230 and again fro .... The mounts constitute rocks dramatically emerging from the land, running in a north-eastern line across the landscape. Image:Bretagne_Finistere_RocTrevezel_1991_001.jpg, Roc'h Trevezel Image:Bretagne_Finistere_RocTrevezel_1991_002.jpg, Roc'h Trevezel File:Émetteur de Roc'h Trédudon.jpg, Roc'h Tredudon References External links Statistic concerning Breton mountains. {{DEFAULTSORT:Monts D'Arree Mountain ranges of Brittany Brittany region articles needing translation from French Wikipedia ...
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Breton Language
Breton (, ; or in Morbihan) is a Southwestern Brittonic language of the Celtic language family spoken in Brittany, part of modern-day France. It is the only Celtic language still widely in use on the European mainland, albeit as a member of the insular branch instead of the continental grouping. Breton was brought from Great Britain to Armorica (the ancient name for the coastal region that includes the Brittany peninsula) by migrating Britons during the Early Middle Ages, making it an Insular Celtic language. Breton is most closely related to Cornish, another Southwestern Brittonic language. Welsh and the extinct Cumbric, both Western Brittonic languages, are more distantly related. Having declined from more than one million speakers around 1950 to about 200,000 in the first decade of the 21st century, Breton is classified as "severely endangered" by the UNESCO '' Atlas of the World's Languages in Danger''. However, the number of children attending bilingual classes rose 33 ...
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Brittany
Brittany (; french: link=no, Bretagne ; br, Breizh, or ; Gallo language, Gallo: ''Bertaèyn'' ) is a peninsula, Historical region, historical country and cultural area in the west of modern France, covering the western part of what was known as Armorica during the period of Roman occupation. It became an Kingdom of Brittany, independent kingdom and then a Duchy of Brittany, duchy before being Union of Brittany and France, united with the Kingdom of France in 1532 as a provinces of France, province governed as a separate nation under the crown. Brittany has also been referred to as Little Britain (as opposed to Great Britain, with which it shares an etymology). It is bordered by the English Channel to the north, Normandy to the northeast, eastern Pays de la Loire to the southeast, the Bay of Biscay to the south, and the Celtic Sea and the Atlantic Ocean to the west. Its land area is 34,023 km2 . Brittany is the site of some of the world's oldest standing architecture, ho ...
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Armorican Massif
The Armorican Massif (french: Massif armoricain, ) is a geologic massif that covers a large area in the northwest of France, including Brittany, the western part of Normandy and the Pays de la Loire. It is important because it is connected to Dover on the British side of the English Channel and there has been tilting back and forth that has controlled the geography on both sides. Its name comes from the old Armorica, a Gaul area between the rivers Loire and Seine. The massif is composed of metamorphic and magmatic rocks that were metamorphosed and/or deformed during the Hercynian or Variscan orogeny (400 to 280 million years ago) and the earlier Cadomian orogeny (650 to 550 million years ago). The region was uplifted when the Bay of Biscay opened during the Cretaceous period. The Cantabrian Mountains and the Armorican Massif were then rift shoulders of the Bay of Biscay. The competent old rocks of the Armorican Massif have been eroded to a plateaulike peneplain. The highes ...
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Cornouaille
Cornouaille (; br, Kernev, Kerne) is a historical region on the west coast of Brittany in West France. The name is cognate with Cornwall in neighbouring Great Britain. This can be explained by the settlement of Cornouaille by migrant princes from Cornwall who created an independent principality founded by Rivelen Mor Marthou, and the founding of the Bishopric of Cornouaille by ancient saints from Cornwall. Celtic Britons and the settlers in Brittany spoke a common language, which later evolved into Breton, Welsh and Cornish. Etymology The toponym Cornouaille was established in the early Middle Ages in the southwest of the Breton peninsula. Prior to this, following the withdrawal of Rome from Britain, other British migrants from what is now modern Devon had established the region of ''Domnonea'' (in Breton) or ''Domnonée'' (in French) in the north of the peninsula, taken from the Latin ''Dumnonia''. The region was first mentioned in surviving records by a ''Cornouaille'' ...
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Viscounty Of Léon
The Viscounty or County of Léon () was a feudal state in extreme western Brittany in the High Middle Ages. Though nominally a vassal of the sovereign duke of Brittany, Léon was functionally independent of any external controls until the viscounts came under attack by King Henry II of England. It thus became the focus of revolts and wars when Brittany was drawn into the Angevin empire. The history of Léon's early counts is obscure. The original viscounts of Léon were public officials appointed by the counts of Cornouaille, but by the mid-eleventh century they had usurped public authority in their province. Their ability to remain independent of both count and duke was likely due to their remoteness in the extremity of the Armorican peninsula. Unlike their Breton neighbours they did not participate in the Norman conquest of England in 1066.Everard, 16. Count Harvey II, however, did participate on the side of Stephen of Blois in the nineteen years of civil war in England called ...
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Mountain Ranges Of Brittany
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ...
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