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40-574: Muggensturm is sited in the Upper Rhine Plain at the foot of the Black Forest . The Federbach flows through the town and the neighboring 43 ha nature reserve Federbachbruch . The municipality borders Bietigheim , Malsch (district of Karlsruhe ), Oberweier , Kuppenheim , Waldprechtsweier and Bischweier . Muggensturm's area contains the municipality as well as the Ziegelhütte house in

80-584: 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

120-615: A downfaulted trough through which the river Rhine flows. The Upper Rhine Plain 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

160-547: 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

200-854: A range of medium mountains in Eastern France , near its border with Germany . 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 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

240-561: 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

280-767: Is a cluster of volcanic hills to the northwest of Freiburg, within 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

320-596: Is named after the range. From 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

360-677: Is sited near the Bundesstraße 3 and the Rheintalbahn . It is connected to the Karlsruhe Stadtbahn . 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

400-557: 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

440-689: 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

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480-545: The Odenwald on the eastern side. The extension induced by the formation of the Alps was sufficient to thin 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")

520-601: 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

560-465: The Steinhardt and the lost settlements of Eichelbach and Frierlinde. The first mention of Muggensturm can be found in an official document of Pope Celestine III in the year 1193, where it is spelled Mugetstrum . The 2009 local election resulted in the following composition of the municipal council ( Gemeinderat ): The voter participation was 54.1% (+0.2). Numbers in braces refer to the results of

600-656: 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

640-494: 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

680-400: 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

720-524: 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

760-710: 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

800-636: 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);

840-580: The city of Basel and flattening buildings as far as 200 km away. It 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

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880-507: 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

920-472: The formation of an extensional basin. As a consequence, the highest mountains exist immediately adjacent to 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

960-623: 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

1000-604: 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

1040-584: The length of the basin. To the west, in France, these hills are known as the Vosges mountain range and in 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

1080-672: The many thrust faults that make up the Alps to the south. Doubts have been raised over 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

1120-544: 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

1160-511: 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

1200-611: 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

1240-509: The previous local election. Since 1993 Dietmar Späth (born 1963) is the mayor, he was reelected in 2001 and 2009. Muggensturm's twin town is Gradara in the Italian province of Pesaro and Urbino. It was established in 2002. In 2011 an additional inner-German town twinning with Schönwalde-Glien ( Brandenburg ) was founded. In 2005, the Bürgerband ( citizen belt ), a unique community photo album,

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1280-620: 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,

1320-570: The same Vosges geologic structure but traditionally receives this different name for historical and political reasons. From 1871 to 1918 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

1360-642: The south and the cities of Frankfurt / Wiesbaden in 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

1400-443: 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

1440-756: The water used by industry. Since the 1970s it has suffered increasingly serious pollution from nitrates , pesticides , chloride and VOCs . A collaboration of 25 universities and government agencies have been researching seismic hazards, neotectonics, and water management of the Quaternary Graben fill. The research focuses on four themes: 48°57′54″N 8°14′02″E  /  48.9650°N 8.2340°E  / 48.9650; 8.2340 Vosges mountain range The Vosges ( / v oʊ ʒ / VOHZH , French: [voʒ] ; German : Vogesen [voˈɡeːzn̩] ; Franconian and Alemannic German : Vogese ) are

1480-570: The western boundary of the Upper Rhine Plain . The Grand Ballon 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

1520-438: Was irregular , the initial contact between the two continents resulted in the formation of dilational (extensional) structures in 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

1560-526: Was installed in the town hall . It shows around 2'500 Muggensturm citizens photographed by journalist Anton Jany. Every year at the end of July, the Muggensturm Volksfest attracts many visitors. Before 2011, local clubs would decorate waggons with up to 200'000 flowers and participate in a large pageant. Population development: In 2010, Muggensturm won the gold medal in the Entente Florale competition between municipalities. Entente Florale awards distinguished town development achievements. Muggensturm

1600-449: 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

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