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Garonne Lateral Canal
The Garonne (, also , ; Occitan, Catalan, Basque, and es, Garona, ; la, Garumna or ) is a river of southwest France and northern Spain. It flows from the central Spanish Pyrenees to the Gironde estuary at the French port of Bordeaux – a length of , of which is in Spain (Val d'Aran); The Ratera-Saboredo cirque has been pointed by many researchers as the origin of the Garonne.Faura i Sans (M.); Sobre hidrología subterránea en los Pirineos Centrales de Aragón y Cataluña. Bol. de la Real Soc. de Hist. Nat, vom. XVI, pgs. 353-354. Madrid, 1916. The third thesis holds that the river rises on the slopes of Pic Aneto at above sea level and flows by way of a sinkhole known as the '' Forau de Aigualluts'' () through the limestone of the Tuca Blanca de Pomèro and a resurgence in the Val dera Artiga above the Aran Valley in the Spanish Pyrenees. This underground route was suggested by the geologist Ramond de Carbonnières in 1787, but there was no confirmation until 1931, when ...
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Bordeaux
Bordeaux ( , ; Gascon oc, Bordèu ; eu, Bordele; it, Bordò; es, Burdeos) is a port city on the river Garonne in the Gironde department, Southwestern France. It is the capital of the Nouvelle-Aquitaine region, as well as the prefecture of the Gironde department. Its inhabitants are called ''"Bordelais"'' (masculine) or ''"Bordelaises"'' (feminine). The term "Bordelais" may also refer to the city and its surrounding region. The city of Bordeaux proper had a population of 260,958 in 2019 within its small municipal territory of , With its 27 suburban municipalities it forms the Bordeaux Metropolis, in charge of metropolitan issues. With a population of 814,049 at the Jan. 2019 census. it is the fifth most populated in France, after Paris, Lyon, Marseille and Lille and ahead of Toulouse. Together with its suburbs and exurbs, except satellite cities of Arcachon and Libourne, the Bordeaux metropolitan area had a population of 1,363,711 that same year (Jan. 2019 census), ma ...
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Latin
Latin (, or , ) is a classical language belonging to the Italic branch of the Indo-European languages. Latin was originally a dialect spoken in the lower Tiber area (then known as Latium) around present-day Rome, but through the power of the Roman Republic it became the dominant language in the Italian region and subsequently throughout the Roman Empire. Even after the fall of Western Rome, Latin remained the common language of international communication, science, scholarship and academia in Europe until well into the 18th century, when other regional vernaculars (including its own descendants, the Romance languages) supplanted it in common academic and political usage, and it eventually became a dead language in the modern linguistic definition. Latin is a highly inflected language, with three distinct genders (masculine, feminine, and neuter), six or seven noun cases (nominative, accusative, genitive, dative, ablative, and vocative), five declensions, four verb conjuga ...
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Louis Ramond De Carbonnières
Louis François Élisabeth Ramond, baron de Carbonnières (4 January 1755 Strasbourg – 14 May 1827), was a French politician, geologist and botanist. He is regarded as one of the first explorers of the high mountains of the Pyrenees who can be described as a '' pyreneist''. Life Louis Ramond was born in Strasbourg, to Pierre-Bernard Ramond (1715–1796), treasurer of war, and Rosalie-Reine Eisentrand (1732–1762). He studied law at the University of Strasbourg in 1775 and became a lawyer in February 1777. In Strasbourg he became friends with another student, Jakob Michael Reinhold Lenz (1751–1792), a writer belonging to the then-fashionable '' Sturm und Drang'' movement. During this period Ramond discovered German Romantic literature, in particular Goethe's '' The Sorrows of Young Werther''; this book inspired him to become a writer and in 1777 he published the ''Werther''-influenced ''Les Dernières aventures du jeune d’Olban'' (''The Last Adventures of Young Olban''). ...
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Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ...
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Forau De Aigualluts
Aigualluts is a karst formation and waterfall in the Province of Huesca, northeastern Spain. It lies along the Ésera River, at 2074 m above sea level on Pico Aneto. Description A walk of just an hour and a half in total duration, essential for anyone who travels to the Benasque Valley for the first time, being probably the most visited place in this valley. The Forau de Aiguallut is a chasm through which the waters from the Aneto glacier disappear to resurface again in the Val d'Aran, in the Garonne river basin, which flows into the Atlantic Sea in the French city of Bordeaux Bordeaux ( , ; Gascon oc, Bordèu ; eu, Bordele; it, Bordò; es, Burdeos) is a port city on the river Garonne in the Gironde department, Southwestern France. It is the capital of the Nouvelle-Aquitaine region, as well as the prefect .... Before its disappearance, the waters coming from the Aneto glacier flow into the great meadow of the Plan d’Aigualluts, where it meanders in small m ...
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Sinkhole
A sinkhole is a depression or hole in the ground caused by some form of collapse of the surface layer. The term is sometimes used to refer to doline, enclosed depressions that are locally also known as ''vrtače'' and shakeholes, and to openings where surface water enters into underground passages known as ''ponor'', swallow hole or swallet. A ''cenote'' is a type of sinkhole that exposes groundwater underneath. A ''sink'' or ''stream sink'' are more general terms for sites that drain surface water, possibly by infiltration into sediment or crumbled rock. Most sinkholes are caused by karst processes – the chemical dissolution of carbonate rocks, collapse or suffosion processes. Sinkholes are usually circular and vary in size from tens to hundreds of meters both in diameter and depth, and vary in form from soil-lined bowls to bedrock-edged chasms. Sinkholes may form gradually or suddenly, and are found worldwide. Formation Natural processes Sinkholes may capture surf ...
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Pont De Rei
The Pont de Rei ( en, King's Bridge, french: Pont du Roi, oc, Eth Pònt de Rei) is a bridge and border crossing over the river Garonne that connects the Aran Valley of Spain with the Haute-Garonne department of France. The road on the French side is N125, ending in the commune of Fos; on the Spanish side the road is N-230, ending in the municipality of Bausen. History In 1515, the ''Plan d'Arem'' agreement was signed at the crossing between Spanish and French nobles and representatives to guarantee free passage and exchange of goods between the valleys on both sides of the border. A festival was held and a monument erected in 2015 to commemorate the 500-year anniversary of the treaty. The border crossing was used by many Spanish refugees fleeing to France during the Spanish Civil War; and in the other direction by Jews fleeing the Nazi occupation of France The Military Administration in France (german: Militärverwaltung in Frankreich; french: Occupation de la France pa ...
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Sea Level
Mean sea level (MSL, often shortened to sea level) is an average surface level of one or more among Earth's coastal bodies of water from which heights such as elevation may be measured. The global MSL is a type of vertical datuma standardised geodetic datumthat is used, for example, as a chart datum in cartography and marine navigation, or, in aviation, as the standard sea level at which atmospheric pressure is measured to calibrate altitude and, consequently, aircraft flight levels. A common and relatively straightforward mean sea-level standard is instead the midpoint between a mean low and mean high tide at a particular location. Sea levels can be affected by many factors and are known to have varied greatly over geological time scales. Current sea level rise is mainly caused by human-induced climate change. When temperatures rise, Glacier, mountain glaciers and the Ice sheet, polar ice caps melt, increasing the amount of water in water bodies. Because most of human settlem ...
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Aneto
Aneto (''pic d'Aneto'' in French language, French, formerly ''pic de Néthou'') is the highest mountain in the Pyrenees and in Aragon, and Spain's third-highest mountain, reaching a height of . It stands in the Spanish province of Huesca (province), Huesca, the northernmost of the three Aragonese provinces, south of the France–Spain border. It forms the southernmost part of the Maladeta massif. Aneto is located in the Posets-Maladeta Natural Park, in the municipality of Benasque, Province of Huesca, Huesca province, autonomous community of Aragon, Spain. It is part of the Maladeta massif and is located in the Benasque valley. It consists of Paleozoic terrain of a granitic nature and Mesozoic materials. Its northern side holds the largest glacier in the Pyrenees, covering in 2005; it is shrinking rapidly due to warming summer temperatures and decreasing winter precipitations over the 20th century – it covered 106.7 ha in 1981, and over 200 ha in the 19th century. ...
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Aran Valley
Aran (; ; ) (previously officially called in Occitan Val d'Aran, Catalan: ''Vall d'Aran'', Spanish: ''Valle de Arán'') is an administrative entity (formerly considered a Comarques of Catalonia, comarca) in Lleida (province), Lleida, Catalonia, Spain, consisting of the Aran Valley, in area, in the Pyrenees mountains, in the northwestern part of the province of Lleida. This valley constitutes the only contiguous part of Catalonia located on the northern side of the Pyrenees. Hence, this valley holds the only Catalan rivers to flow into the Atlantic Ocean (for the same reason, the region is characterized by an Atlantic climate, instead of a Mediterranean one). The Garonne river flows through Aran from its source on the Pla de Beret (Beret Flat) near the Port de la Bonaigua. It is joined by the Joèu river (from the slopes of Aneto, Aneto mountain) which passes underground at the ''Forau de Aigualluts''. It then reappears in the Val dera Artiga de Lin before reaching the Aran valley, ...
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Garonne 5102
The Garonne (, also , ; Occitan, Catalan, Basque, and es, Garona, ; la, Garumna or ) is a river of southwest France and northern Spain. It flows from the central Spanish Pyrenees to the Gironde estuary at the French port of Bordeaux – a length of , of which is in Spain (Val d'Aran); The Ratera-Saboredo cirque has been pointed by many researchers as the origin of the Garonne.Faura i Sans (M.); Sobre hidrología subterránea en los Pirineos Centrales de Aragón y Cataluña. Bol. de la Real Soc. de Hist. Nat, vom. XVI, pgs. 353-354. Madrid, 1916. The third thesis holds that the river rises on the slopes of Pic Aneto at above sea level and flows by way of a sinkhole known as the '' Forau de Aigualluts'' () through the limestone of the Tuca Blanca de Pomèro and a resurgence in the Val dera Artiga above the Aran Valley in the Spanish Pyrenees. This underground route was suggested by the geologist Ramond de Carbonnières in 1787, but there was no confirmation until 1931, whe ...
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Benasque - Aigualluts - Cascada 03
Benasque (; in Benasquese dialect: ''Benás''; an, Benás) () is a town in the comarca of Ribagorza, province of Huesca, (Spain). It is the main town in the Benasque Valley, located in the heart of the Pyrenees and surrounded by the highest peaks in that range. Climate The climate is of a high mountain type, with cool summers, and cold winters and frequent snow. Its average annual temperature is 9.4 degrees Celsius (at 1138 meters above sea level). Language The regional language of Benasque is a Catalan– Aragonese transitional dialect that shares features with Gascon (Occitan). It is usually called ''patués'' ("patois") by its native speakers. Possessing features that are transitional between Aragonese and Catalan, it has sometimes been classified as a variety of Catalan. To promote the local language, the local council has held an annual writing and poetry competition in ''patués'' since 1999. Separate awards are given to young and grown-up authors. Gallery ...
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