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42-560: It is located between the Vosges and the Jura mountains . Mining began in Ronchamp in the mid-18th century and had developed into a full industry by the late 19th century, employing 1500 people. The museum looks back at the miners' work, the techniques and tools they used, and their social life. A collection of miners' lamps is also on display. The chapel of Notre Dame du Haut, designed by Le Corbusier ,

84-638: A Triassic rose sandstone) are embedded sometimes up to more than 500 m (1,600 ft) in thickness. 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. The Vosges are very similar to the corresponding range of the Black Forest across the Rhine since both lie within the same degrees of latitude, have similar geological formations and are characterized by forests on their lower slopes, above which are open pastures and rounded summits of

126-547: A forested region. Forests were cleared for agriculture, livestock and early industrial factories (such as charcoal works and glassworks ) and the water mills used water power . Concentrations of settlement and immigration took place and not only in areas where minerals were found. In the mining area of the Lièpvrette  [ fr ] valley, for example, there was an influx of Saxon miners and mining specialists. From time to time, wars, plagues and religious conflicts saw

168-612: A geological point of view, a graben at the beginning of the Paleogene period caused the formation of Alsace and the uplift of the bedrock plates of the Vosges, in eastern France , and those in the Black Forest , in Germany . 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

210-512: A rather uniform altitude. Both areas exhibit steeper slopes towards the Rhine and a more gradual descent on the other side. Both the Vosges and the Black Forest were formed by isostatic uplift in response to the opening of the Rhine Graben , a major extensional basin. When such basins form, the thinning of the crust causes uplift immediately adjacent to the basin, decreasing with distance from

252-612: Is located in Ronchamp. It is a shrine for the Catholic Church at Ronchamp and was built for a reformist Church looking to continue its relevancy. Warning against decadence, reformers within the Church looked to renew its spirit by embracing modern art and architecture as representative concepts. Marie-Alain Couturier , who would also sponsor Le Corbusier for the La Tourette commission, steered

294-747: Is the highest peak at 1,424 m (4,672 ft), followed by the Storkenkopf (1,366 m, 4,482 ft), and the Hohneck (1,364 m, 4,475 ft). Geographically , the Vosges Mountains are wholly in France , far above the Col de Saverne separating them from the Palatinate Forest in Germany . The latter area logically continues the same Vosges geologic structure but traditionally receives this different name for historical and political reasons. From 1871 to 1918

336-557: The Celts . After the Roman era, Alemanni also settled in the east, and Franks in the northwest. Contrary to widespread belief, the main ridge of the Vosges coincided with the historical Roman-Germanic language boundary only in the southern Vosges. 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

378-537: The First World War : Upper Rhine Plain The Upper Rhine Plain , Rhine Rift Valley or Upper Rhine Graben ( German : Oberrheinische Tiefebene , Oberrheinisches Tiefland or Oberrheingraben , French : Vallée du Rhin ) is a major rift , about 350-kilometre-long (220 mi) and on average 50-kilometre-wide (31 mi), between Basel in the south and the cities of Frankfurt / Wiesbaden in

420-689: The Kastelberg to 1,350 m (4,429 ft); and the Ballon d'Alsace to 1,247 m (4,091 ft). The Col de Saales, between the Higher and Central Vosges, reaches nearly 579 m (1,900 ft), both lower and narrower than the Higher Vosges, with Mont Donon at 1,008 m (3,307 ft) being the highest point of this Nordic section. The highest mountains and peaks of the Vosges (with Alsatian or German names in brackets) are: Two nature parks lie within

462-601: The Parc naturel régional des Ballons des Vosges (established in 1989). Meteorologically , as a consequence of the Foehn effect the difference between the eastern and western mean slopes of the range is very marked. 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

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504-656: The Val d'Argent ; "Valley of Silver"), parts of the canton of Villé valley  [ fr ] ( Vallée de Villé ) and parts of the Bruche valley ( Vallée de la Bruche ). 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

546-565: The foreland basin to the north of the Alps. The result was substantial crustal thinning, forming a major extensional graben and causing isolated volcanic activity. The stretch factor is estimated to be ~2. To both the east and west of the Rhine Plain, two major hill ranges have formed that run the length of the basin. To the west, in France, these hills are known as the Vosges mountain range and in

588-721: The Rhine Graben. The highest point of this small, isolated volcanic centre is the Totenkopf (557 metres). Volcanic activity was most prevalent in the Miocene epoch, some 15 million years ago. Today, the Kaiserstuhl volcano is extinct. In 1356, the Basel earthquake occurred in the Rhine Plain. It was perhaps the most destructive earthquake ever in northwest Europe , destroying the city of Basel and flattening buildings as far as 200 km away. It

630-494: The Rhine valley, the Black Forest and the distant, snow-covered Swiss mountains. The massif known in Latin as Vosago mons or Vosego silva , sometimes Vogesus mons , was extended to the vast woods covering the region. Later, German speakers referred to the same region as Vogesen or Wasgenwald . Over the centuries, settlement population density grew gradually, as was typical for

672-400: The Vosges Mountains. The highlands of the arrondissement of Remiremont receive as annual rainfall or snowfall more than 2,000 mm (79 in) of precipitation yearly, whereas some dry countryside near Colmar receives less than 500 mm (20 in) of water in the event of insufficient storms. The temperature is much lower in the west front of the mountains than in the low plains behind

714-464: The Vosges marked for the most part the border between Germany and France, due to the Franco-Prussian War . The elongated massif is divided south to north into three sections: In addition, the term "Central Vosges" is used to designate the various lines of summits, especially those above 1,000 m (3,300 ft) in elevation. The French department of Vosges is named after the range. From

756-524: The Vosges were the scene of the Battle of Trippstadt . From 1871 to 1918, they formed the main border line between France and the German Empire . The demarcation line stretched from the Ballon d'Alsace in the south to Mont Donon in the north with the lands east of it being incorporated into Germany as part of Alsace-Lorraine . The Vosges saw extensive fighting during the world wars. During World War I, there

798-759: The Vosges: the Ballons des Vosges Nature Park and the Northern Vosges Regional Nature Park . The Northern Vosges Nature Park and the Palatinate Forest Nature Park on the German side of the border form the cross-border UNESCO -designated Palatinate Forest-North Vosges Biosphere Reserve . 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

840-580: The adequacy of the seismic evaluation and design of the Fessenheim Nuclear Power Plant , built in the Rhine Plain close to the faults. Located below the plain, the Upper Rhine aquifer – one of the largest in Europe – holds an estimated 45,000 km (11,000 cu mi) of fresh water and supplies some 3 million people in France and Germany, supplying 75% of their drinking water and 50% of

882-587: The basin. Thus, the highest range of peaks rises immediately adjacent to the basin and increasingly lower mountains rise further from the basin. 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);

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924-404: The crust and provide suitable dilational conduits for magmatic and volcanic activity to occur. This resulted in the emplacement of mafic dykes , which follow the general structural trend of the extensional faults. In addition, isolated volcanoes such as the Kaiserstuhl were formed. The Kaiserstuhl (literally "Emperor's Chair") is a cluster of volcanic hills to the northwest of Freiburg, within

966-507: The depopulation of territories – in their wake it was not uncommon for people to be relocated there from other areas. On the lower heights and buttresses of the main chain on the Alsatian side are numerous castles, generally in ruins, testifying to the importance of this crucial crossroads of Europe, violently contested for centuries. At several points on the main ridge, especially at Sainte Odile above Ribeauvillé (German: Rappoltsweiler), are

1008-487: The east, in Germany, the hills comprise the Black Forest . These ranges exhume the same types of rocks in their cores, including deep crustal gneiss . Both ranges correspond to uplifts of more than 2,500 metres, much of which has since been eroded. This uplift has occurred because of the isostatic response associated with the formation of an extensional basin. As a consequence, the highest mountains exist immediately adjacent to

1050-564: The fight against the German occupation . Le Corbusier also sensed a sacral relationship of the hill with its surroundings, the Jura mountains in the distance and the hill itself, dominating the landscape. The nature of the site would result in an architectural ensemble that has many similitudes with the Acropolis , starting from the ascent at the bottom of the hill to architectural and landscape events along

1092-623: The larger Tertiary formations. Erosive glacial action was the primary catalyst for development of the highland massif feature. The Vosges in their southern and central parts are called the Hautes Vosges . These consist of a large Carboniferous mountain eroded just before the Permian Period with gneiss , granites , porphyritic masses or other volcanic intrusions. The north, south and west parts are less eroded by glaciers, and here Vosges Triassic and Permian red sandstone remains are found in large beds. The grès vosgien (a French name for

1134-604: The last two from the Vosges Mountains. The rivers Moselle , Meurthe and Sarre and their numerous affluents all rise on the Lorraine side. 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 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

1176-466: The margin of the basin, and become increasingly low outwards. The boundaries between the hill ranges and the Rhine Graben are defined by major, normal fault zones. The northern section of the Rhine Plain is equally framed by somewhat lower mountain ranges, the Palatinate Forest on the western and the Odenwald on the eastern side. The extension induced by the formation of the Alps was sufficient to thin

1218-544: The massif, especially in summer. 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. 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

1260-511: The mountainside under heavy fire from the Germans. Two previous rescues failed. The 442nd suffered 800 casualties, rescued the Texans, and took the mountain. On 20 January 1992 Air Inter Flight 148 crashed into the Vosges Mountains while circling to land at Strasbourg International Airport, killing 87 people. In pre-Roman times, the Vosges was empty of settlements or was colonized and dominated by

1302-697: The north on the German side of the border, they form a single geomorphological unit and low mountain range of around 8,000 km (3,100 sq mi) in area. It runs in a north-northeast direction from the Burgundian Gate (the Belfort – Ronchamp – Lure line) to the Börrstadt Basin (the Winnweiler – Börrstadt – Göllheim line), and forms the western boundary of the Upper Rhine Plain . The Grand Ballon

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1344-717: The north. Its southern section straddles the France–Germany border . It forms part of the European Cenozoic Rift System , which extends across Central Europe . The Upper Rhine Graben formed during the Oligocene , as a response to the evolution of the Alps to the south. It remains active to the present day. Today, the Rhine Rift Valley forms a downfaulted trough through which the river Rhine flows. The Upper Rhine Plain

1386-611: The northwest and runs between Donon and Mutzigfelsen heading for Sarrebourg ( Saarburg ). 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 Romance-speaking areas are traditionally part of the Lorrain language region in the west and the Frainc-Comtou region in

1428-522: The relationship of the building with its surroundings. Vosges Mountains The Vosges ( / v oʊ ʒ / VOHZH , French: [voʒ] ; German : Vogesen [voˈɡeːzn̩] ; Franconian and Alemannic German : Vogese ) are a range of medium mountains in Eastern France , near its border with Germany . Together with the Palatine Forest to

1470-620: 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). 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 . During the French Revolutionary Wars , on 13 July 1794,

1512-443: The south. For a long time the distribution of languages and dialects basically correlated with the pattern of settlement movements. However, the switch from German to French as the lingua franca which took place between the 17th and the 20th century across the whole of Alsace was not accompanied by any further significant movements of population. General texts: List of majors periodicals concerning Lorraine and South Lorraine: On

1554-546: The unorthodox project to completion in 1954. This work, like several others in Le Corbusier’s late oeuvre, departs from his principles of standardization and the machine aesthetic outlined in Vers une architecture . In this project, the structural design of the roof was inspired by the engineering of airfoils . It also resembles a nun's coif . The chapel is clearly a site-specific response. By Le Corbusier’s own admission, it

1596-418: The way, before finally terminating at the sanctum sanctorum itself, the chapel. The building itself is a comparatively small structure enclosed by thick walls, with the upturned roof supported on columns embedded within the walls. In the interior, the spaces left between the wall and roof, as well as asymmetric light from the wall openings serve to further reinforce the sacral nature of the space and buttress

1638-617: Was formed during the Early Cenozoic era, during the Late Eocene epoch. At this time, the Alpine Orogeny , the major mountain building event that was to produce the Alps , was in its early stages. The Alps were formed because the continents of Europe and Africa collided. It is thought that because the collision was irregular , the initial contact between the two continents resulted in the formation of dilational (extensional) structures in

1680-449: Was severe and almost continuous fighting in the mountains. During World War II in October 1944, there was a fierce battle between German forces and the U.S. 442nd Regiment, a segregated unit composed of second-generation Japanese Americans (Nisei), during which the 442nd charged straight up the mountain to rescue the 1st Battalion of the 36th Infantry, formerly the Texas Guard—also known as the "Lost Battalion"—who were cut off and stranded on

1722-418: Was the most significant historic seismological event to have occurred in Central Europe. Its epicenter was between Waldkirch and St. Peter in Breisgau-Hochschwarzwald . However, it remains disputed whether the fault that ruptured to cause this earthquake was part of the Rhine Valley extensional system, or simply one of the many thrust faults that make up the Alps to the south. Doubts have been raised over

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1764-401: Was the site that provided an irresistible genius loci for the response, with the horizon visible on all four sides of the hill and its historical legacy for centuries as a place of worship. This historical legacy weaved in different layers into the terrain — from the Romans and sun-worshippers before them, to a cult of the Virgin in the Middle Ages, right through to the modern church and

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