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</html>";s:4:"text";s:10887:"At several points on the main ridge, especially at Sainte Odile above Ribeauvillé (German: Rappoltsweiler), are the remains of a wall of unmortared stone with tenons of wood, about 1.8 to 2.2 m (6 to 7 ft) thick and 1.3 to 1.7 m (4 to 6 ft) high, called the Mur Païen (Pagan Wall). From 1871 to 1918, they formed the main border line between France and the German Empire. Let yourself be inspired! It was used for defence in the Middle Ages and archaeologists are divided as to whether it was built by the Romans, or before their arrival.[7]. All great mountain systems of the earth are of this type. The Rhine Graben is a major extensional basin. Every season offers different pleasures: revitalizing escapades and intense moments, full of emotion. Fold Mountains . In the High Moselle and Meurthe basins, moraines, boulders and polished rocks testify to the former existence of glaciers which once covered the top of the Vosges. The grès vosgien (a French name for a Triassic rose sandstone) are embedded sometimes up to more than 500 m (1,600 ft) in thickness. Both the fold and the block mountains are included in this type. Old Romance (Altromanisch) is spoken east of the main ridge: in the valley of the Weiss around Lapoutroie, the valley of Lièpvrette (nowadays also called the Val d'Argent; "Valley of Silver"), parts of the canton of Villé valley (Vallée de Villé) and parts of the Bruche valley (Vallée de la Bruche). Share your best experiences in Alsace with #visitalsace. Concentrations of settlement and immigration took place and not only in areas where minerals were found. "La guerre aérienne dans les Vosges. In the Vosges Mountains, a fantastic playground, you can make lots of discoveries. Both areas exhibit steeper slopes towards the Rhine River and a more gradual descent on the other side. Forests were cleared for agriculture, livestock and early industrial factories (such as charcoal works and glassworks) and the water mills used water power. At these legendary farm inns, you can taste genuine local flavours. The massif known in Latin as Vosago mons or Vosego silva, sometimes Vogesus mons, was extended to the vast woods covering the region. In the Vosges Mountains, a fantastic playground, you can make lots of discoveries. The mountain lakes caused by the original glacial phenomena are surrounded by pines, beeches and maples, and green meadows provide pasture for large herds of cattle, with views of the Rhine valley, the Black Forest and the distant, snow-covered Swiss mountains. Pick your activity ©Thomas DEVARD-MASSIF DES VOSGES . The First World War featured severe and almost continuous fighting in the mountains. [citation needed]. The latter area logically continues the same Vosges geologic structure but traditionally receives this different name for historical and political reasons. The main air streams come generally from the west and southwest, so the Alsatian central plains just under the Hautes-Vosges receive much less water than the south-west front of the Vosges Mountains. Vosges, massif extending west of the Rhine River Valley in the Haut-Rhin, Bas-Rhin, and Vosges départements of eastern France.Of ancient rocks, the dome-shaped mountains rise to their greatest heights north of Belfort Gap and then spread westward for more than 40 miles (64 km) toward the Moselle Valley and northward for more than 70 miles (114 km) parallel to the Rhine. An infinite variety of experiences will thrill seekers of fresh air, adventure and a change of scenery. In pre-Roman times, the Vosges was empty of settlements or was colonized and dominated by the Celts. Full of iconic itineraries and sources of inspiration, these mountains will take you on a wonderful adventure. Together with the Palatine Forest to the north on the German side of the border, they form a single geomorphological unit and low mountain range of around 8,000 km2 (3,100 sq mi) in area. The French department of Vosges is named after the range. [8] During the Second World War, in autumn 1944, they were the site of brief but sharp fighting between Franco-American and German forces. #1. The Vosges have been declared as a UNESCO Biosphere Reserve since 1989. The Vosges forms a low-mountain range that covers an area of around 3,100 square miles. If rock-climbing has not satisfied your search for thrills and breathtaking views of the Vosges mountains, you can also admire lakes and mountains from the air during a paragliding flight. After the Roman era, Alemanni also settled in the east, and Franks in the northwest. The highest points are in the Hautes Vosges: the Grand Ballon, in ancient times called Ballon de Guebwiller or Ballon de Murbach, rises to 1,424 m (4,672 ft); the Storckenkopf to 1,366 m (4,482 ft); the Hohneck to 1,364 m (4,475 ft); the Kastelberg to 1,350 m (4,429 ft); and the Ballon d'Alsace to 1,247 m (4,091 ft). The Vosges (/voʊʒ/ VOHZH,[1][2][3] French: [voʒ] (listen); German: Vogesen [voˈɡeːzn̩] (listen);[4] Alemannic German: Vogese) are a range of low mountains in eastern France, near its border with Germany. Over the centuries, settlement population density gradually, as was typical for a forested region. From time to time, wars, plagues and religious conflicts saw the depopulation of territories – in their wake it was not uncommon for people to be relocated there from other areas. When the two plates move towards … fold mountains, block mountains and volcanic mountains. The Germanic areas of the Vosges mountains are part of the Alemannic dialect region and cultural area and, in the north, also part of the Frankish dialect region and cultural area. The Lower Vosges in the north are dislocated plates of various sandstones, ranging from 300 to 600 m (1,000 to 2,000 ft) high. Where an area of sea separates two plates, sediments settle on the sea floor in depressions called geosynclines. The only rivers in Alsace are the Ill coming from south Alsace (or Sundgau), and the Bruche d'Andlau and the Bruche which have as tributaries other, shorter but sometimes powerful streams coming like the last two from the Vosges Mountains. The latter area logically continues the same Vosges geologic structure but traditionally receives this different name for historical and political reasons. From a scientific view, the Vosges Mountains are not mountains as such, but rather the western edge of the unfinished Alsatian graben, stretching continuously as part of the larger Tertiary formations. This range lies close to the border with Germany, and continues on into the fringes of the Palatine Forest of Germany. On the eastern slope economic vineyards reach to a height of 400 m (1,300 ft); on the other hand, in the mountains, it is a land of pasture and forest. Fold mountains are formed due to the folding of the crustal rocks by the compressive forces which in turn are generated by endogenetic forces. By contrast, those parts of the northern Vosges and the whole of the Wasgau, which lie north of the Breusch valley, fall within the Germanic-speaking area because, from Schirmeck the historical linguistic boundary turns to the northwest and runs between Donon and Mutzigfelsen heading for Sarrebourg (Saarburg). In the late 20th century a wide area of the massif was included in two protected areas, the Parc naturel régional des Vosges du Nord (established in 1976) and the Parc naturel régional des Ballons des Vosges (established in 1989). During the French Revolutionary Wars, on 13 July 1794, the Vosges were the scene of the Battle of Trippstadt. Local free flight schools offer a variety of starting options, including discovery flights, two-seater runs and introductory courses. With two Regional Nature Parks, you’re sure to encounter exceptional fauna and flora. A bridge between the past and the future are a bridge between eastern. You ’ re sure to encounter exceptional fauna and flora 1871 to 1918, formed. Biosphere Reserve since 1989 in Germany near the French-German border were found examples of rift.! Covers an area of sea separates two plates, sediments settle on the side! War featured severe and almost continuous fighting in the south have been as. 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Zerion Mini Shell 1.0