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91-737: Together with the northern part of the adjacent Vosges Mountains in France it forms the UNESCO -designated Palatinate Forest-North Vosges Biosphere Reserve . The Palatinate Forest, together with the Vosges south of the French border, from which it has no morphological separation, is part of a single central upland region of about 8,000 km in area, that runs from the Börrstadt Basin (a line from Winnweiler via Börrstadt and Göllheim ) to

182-564: A Palatine geographer and local historian. Prior to 1850, there was no overall name for the Palatine's bunter sandstone mountains Historical territorial factors, rather than geographical ones, governed perceptions at the time. By contrast, the Celts and Romans viewed the entire mountain range west of the Rhine as a single unit, making no distinction between different parts of the region that, today,

273-648: 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

364-553: 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

455-550: A long time, to refer to the entire range on the west bank of the Rhine, at the beginning of the 20th century, it gradually became restricted to the Alsatian part of the sandstone mountains, whilst the term Pfälzerwald ("Palatinate Forest") became increasingly used to refer to the Palatine part. This led to the Palatinate Forest and Vosges being defined as separate and distinct landscapes. However, in recent decades, in

546-628: A plateau bounded by deeply incised valleys. This plateau also runs towards the west at a height of about 500 m before descending gradually to 400 m. It is bisected by the Schwarzbach and Moosalb rivers. To the southwest other ridges separate the valleys of the Merzalbe and the headstreams of the Wieslauter . It is therefore possible to walk from Neustadt an der Weinstraße to Leimen or Kaiserslautern-Mölschbach without dropping below

637-577: 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

728-400: A result of further depositions of sand, rock layers of up to 500 metres thickness were formed. This led inter alia , through the addition of iron oxide, to a variable colouration of the rock strata – hence the name "bunter" sandstone ( bunter being German for "coloured") – and, depending on the type and binding of the material, (clay-bound sandstone as opposed to silicified quartz sandstone) to

819-411: A significant decline in population and the total number of settlements fell sharply (leaving abandoned villages ), as a result of wars and economic circumstances. Thus, during the colonization of the mountains, areas were often cleared that, because of the nutrient-poor sandy soils, were unsuitable for farming and had to be abandoned after a short period because of overuse and overexploitation . Also,

910-614: 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

1001-515: Is no Misplaced Pages article. Characteristic of the Lower and Middle Bunter are V-shaped valleys , with narrow floors and steep sides, cutting deeply into the bedrock. They are the typical valley forms in the central Palatinate Forest, whilst in the southern and northern parts, U-shaped valleys with wider floors predominate. In the southwestern part of the Forest are the so-called woog valleys, in which

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1092-667: Is the Palatinate Forest and the Vosges . The range was named after the Celtic forest god Vosegus and is recorded in many Roman manuscripts as "silva vosegus" or "mons vosegus". It was from this linguistic root that, during the Middle Ages, the name Vosges emerged in the French-speaking area and Wasgen or Wasigenwald , later also Wasgau , in the German-speaking region. So while the term Wasgen continued, for

1183-530: Is to develop the nature park and its eponymous biosphere reserve equally and to maintain its uniqueness and beauty as well as its national recreational value. Since 1997, the head office of the association has been in Lambrecht . The Palatinate Forest Nature Park was recognized in 1992 by UNESCO as a biosphere reserve . In 1998 it became the German part of the first cross-border UNESCO biosphere reserve, namely

1274-790: The Burgundian Gate (on the line Belfort – Ronchamp – Lure ) and which forms the western boundary of the Upper Rhine Plain . This landscape forms, in turn, the eastern part of the very extensive eastern scarplands of France, which, on German soil, take in large parts of the Palatinate and the Saarland, with older (e.g. on the Donnersberg ) and younger strata ( muschelkalk , e.g. the Westrich Plateau ). While

1365-472: The Altschlossfelsen , fractures , overhangs and honeycomb weathering can also be observed. By contrast, felsenmeers and blockfields tend to be found more in the central Palatine Forest. The highest points in this low mountain range occur in the central Palatinate Forest, and mainly in the east. Here, in a single, contiguous ridge is a series of peaks exceeding the 600 metre mark, of which

1456-569: 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

1547-581: The First World War : Bunter sandstone The Buntsandstein (German for coloured or colourful sandstone ) or Bunter sandstone is a lithostratigraphic and allostratigraphic unit (a sequence of rock strata ) in the subsurface of large parts of west and central Europe. The Buntsandstein predominantly consists of sandstone layers of the Lower Triassic series and is one of three characteristic Triassic units, together with

1638-710: 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

1729-672: The Moder system to the Upper Rhine. To the south, the narrow Zaberner Steige forms a border between the Palatinate Forest, which continues into France as the North Vosges ( Vosges du Nord or Nordvogesen ) and the "actual" Vosges . Geomorphologically and geologically, this dividing line is less pronounced than is the case on the right bank of the Rhine, where the Odenwald and Black Forest are clearly separated from each other by

1820-920: The Muschelkalk and Keuper that form the Germanic Trias Supergroup . The Buntsandstein is similar in age, facies and lithology with the Bunter of the British Isles . It is normally lying on top of the Permian Zechstein and below the Muschelkalk. In the past the name Buntsandstein was in Europe also used in a chronostratigraphic sense, as a subdivision of the Triassic system. Among reasons to abandon this use

1911-555: The Palatinate Forest-North Vosges Biosphere Reserve . It thus became the 12th of (as at 2009) 15 German biosphere reserves. These are areas that have a special significance for the global conservation of biological diversity and in which the ecological aspects, sustainable economic management, environmental education and environmental research are best linked together. In 2007, the state of Rhineland–Palatinate issued an ordinance by which

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2002-642: 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 the western boundary of

2093-621: 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

2184-525: The Quaternary period (2.8 to 0.01 million years ago) erosion processes once more dominated. In particular, it was the weathering and removal processes that occurred during the various cold and warm periods that determined the final topographical shape of the Palatinate Forest. Characteristic of this is a system of deeply incised valleys, especially in the north and centre, diverse mountain shapes and bizarre rock formations. Gneisses and slates form

2275-698: The Rotliegendes . This results in a clear geomorphological separation of the two landscape areas, which runs approximately along a line from Eisenberg via Göllheim and Börrstadt to Otterberg near Kaiserslautern . The hill country between the Haardt and the Upper Rhine Plain, where Palatine wines are grown, is known as the Weinstrasse . The German Wine Route runs through this zone of hills. The St. Ingbert-Kaiserslauten Depression runs up to

2366-571: The Tyrol and Swabia and the settlement of Huguenot and Mennonite religious refugees from Switzerland, France and the Netherlands. From then to the end of the 18th century, the population expanded as a result of the better design of farms (such as the Frankish house ) and the expansion of villages ( clustered village or Haufendörfer ). This development, however, meant that the resources of

2457-628: 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

2548-680: 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

2639-731: The Vosges ridge. This often goes unrecognized as a result of the French border; hence the French southern part of the natural region is often, wrongly, counted as part of the North Vosges. The important subdivisions of these bunter sandstone mountains were drawn up in the 1950s and 1960s in the Handbook of the Natural Region Divisions of Germany and 1:200,000 map sheets by the German Federal Institute for Regional Studies. Despite that, some deviation in

2730-800: The Weinbiet (554.0 m), and the Eckkopf (516.0 m) near Deidesheim . North of the Isenach only the Rahnfels (516.5 m) breaks through the 500 metre contour. In its continuation to the north its descends from 400 to 300 metres above sea level. South of the Queich the countryside changes due to the somewhat different geological situation (see Landscape character ). Here larger erosion surfaces and rather isolated hillforms (conical hills), which on average reach heights of 450 metres, characterize

2821-517: The 19th century (the Ludwig Railway and Landau–Zweibrücken line ) brought some improvement in the situation, because it became possible to commute to towns outside the Palatinate Forest and seek employment in one of the emerging industries (e.g. BASF at Ludwigshafen ) outside the region. In the 20th century, the general economic structural changes in Germany also affected the region of

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2912-532: The 450 metre contour line. North of the line from Hochspeyerbach to Speyerbach the highest points are the 570.8 m high Drachenfels and the Hoher Stoppelkopf ( Stoppelkopf ; 566.2 m). In the triangle formed by the Isenach to the north and German Wine Route to the east are other hills over 500 metres in height. The most prominent are Neustadt's northern local hill ( Hausberg ),

3003-669: The Dutch subdivision, the upper two formations are part of the Upper Germanic Trias and the others part of the Lower Germanic Trias. Bunter sandstone often forms spectacular rock formations as a result of weathering: including isolated rocks several tens of metres high. Most of them are designated natural monuments , for example, the Devil's Table near Hinterweidenthal . In the Palatinate, near Eppenbrunn , are

3094-447: The Earth's crust occurred (passive rifting ). At the same time the sides of the newly created lowlands were uplifted, in the case of the Palatinate Forest, to a height of about 1000 metres. These processes, which continue today, have had four important implications for the present landscape of the low mountain region: In the later Paleogene (34 to 23.8 million years ago) and Neogene (23.8 to 2.8 million years ago) and also in

3185-466: The Great Kalmit , at 672.6 m, is also the highest point of the entire Palatinate Forest. The ridge begins at the Steigerkopf (also called the Schänzel ) (about 500 m) and heads westwards to the Frankenweide region around the Eschkopf (609.9 m) and Weißenberg (609.9 m). This massif extends from the town of Hochspeyer via Johanniskreuz to Hauenstein . Its central area between Johanniskreuz and Hermersbergerhof rather resembles

3276-429: The Lower and Middle Bunter have produced a scarpland relief, whose cuestas characterize the landscape, especially in the north and east, whilst the southeastern part of the Palatinate Forest is dominated by rather isolated types of hill separated by erosion surfaces. In the bunter sandstone mountains a wide variety of hill shapes may be observed, depending on the various rock strata of which they are composed. Typical of

3367-434: The Palatinate Forest, which was increasingly integrated into the overall economic and transport systems . Secluded forest farming villages became municipalities with a service character through the building of infrastructure (e.g. public transport), and, in many cases, the villagers now no longer worked locally, but in more distant regional centres, such as Ludwigshafen and Kaiserslautern. By contrast local industries in

3458-399: 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

3549-478: The UNESCO guidelines for the design of biosphere reserves would be implemented specifically for the Palatinate Forest Nature Park. This laid down a zoning scheme as its main focus, which envisaged three zones with different objectives and protection functions: The "quiet zones" ( Stillezonen ) also covered in the law are intended to ensure a "recreation in the stillness", but are not part of the UNESCO guidelines for biosphere reserves. The concept originates rather from

3640-400: 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

3731-421: 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

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3822-463: 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

3913-443: The appearance of the countryside. Over the millennia, the weathering and erosion of the sandstone, with its varying degrees of hardness, have produced bizarre rock formations, e. g. rock pinnacles , rock faces, rock walls and rock blocks. In addition, the small-scale weathering of strata of differing hardness has produced caves , natural arches and table rocks ( Devil's Table ). On the almost two-kilometre-long rock terrace of

4004-416: The axis of the future Pyrenees . Deposition took place in an arid, continental environment ( playa facies), so that there was little chemical weathering . Therefore, the Buntsandstein deposits are typical red beds , mainly sandstones and conglomerates with little clay . The late Anisian saw a major rise of the global ( eustatic ) sea level. A tropical sea filled the Germanic Basin then, stopping

4095-424: 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);

4186-440: The bedrock of the Palatinate Forest today, but they are generally covered by younger rock formations, cropping out only in a few places on the eastern edge of the mountains. These rock strata cover the bedrock and consist, in addition to sandstone , of shale and marl . They generally have a softer consistency and therefore form broad valleys and erosion surfaces in the northern Palatinate Forest (the Stumpfwald ) as well as in

4277-457: The beginning of the Palaeogene period of the Cenozoic era (66 to 23.8 million years ago) the formation of the Alps led to considerable tensions in the Earth's crust , which, in their forelands to the north of the Alps, caused a bulge in the mantle and crust. At the apex of the arch so formed, there were considerable tensile stresses, so that the rock layers were stretched and about 35 million years ago, deep cracks and depressions in

4368-443: The boundaries of the Palatinate Forest are comparatively clearly defined to the north and east, the transition to neighbouring landscapes to the west and south is less sharp. To the north, the Palatinate Forest is adjoined by the North Palatine Uplands , including the Donnersberg ( 686.5 m ). This is where the bunter sandstone formations typical of the Palatinate Forest end, being replaced by other types of rock such as those of

4459-445: The cities in the Rhine valley which were then suffering badly from air pollution. The nature park expansion programme envisaged 95 car parks, 13 camp sites, seven observation towers and five open-air pools. In fact, 62 woodland car parks were created in the first seven years as well as 530 benches and as many waste bins. A total of 370 km of walking routes were added or created and 45 signed circular walks laid out. The management of

4550-426: The context of European integration (the Schengen Agreement ), there has been an increasing trend to regard the entire mountain complex as a single geographical entity again. Evidence of this changed attitude can be seen, for example, in the establishment in 1998 of the first cross-border biosphere reserve, the Palatinate Forest-North Vosges Biosphere Reserve by UNESCO . Whilst there are traces of human activities in

4641-453: The core area in the biosphere reserve, with its mixed stands of primeval beech, oak and pine. The Palatinate Forest is primarily characterised by a block of bunter sandstone and its underlying formations of Zechstein . The tectonically formed bedding of these rock types and their subsequent erosion led to the topography of this low mountain range that we see today. In the Permian geological period (about 296–251 million years ago)

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4732-457: 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

4823-399: The deposition of the Buntsandstein and marking the beginning of the deposition of the Muschelkalk. The Buntsandstein belongs to the Changhsingian to Anisian stages , meaning it is between 252 and 246 million years old. In German lithostratigraphy, it is seen as a group, in the Netherlands and North Sea the name has no official status (though that does not keep geologists from using it). In

4914-489: The edges of today's Palatinate Forest, there was increasing population pressure in the Middle Ages (10th to 13th century), especially through the initiatives of the nobility and the church , e.g. through the establishment of monasteries such as the Cistercian abbeys of Otterberg (1144) and Eußerthal (1148), the colonization and development of the mountains. Areas that could be used for agriculture were cleared and settled permanently. This development reached its peak in

5005-418: The establishment of the Palatinate Forest Nature Park and, later the Palatinate Forest-North Vosges Biosphere Reserve . The Palatinate Forest Nature Park was created in 1958 as the third nature park in Germany. In accordance with the requirements of the originator of the nature park concept, Alfred Toepfer , the Palatinate Forest was to be a place of recreation and exercise for the stressed office workers of

5096-446: The expansion of recreational facilities was viewed as complete and attention switched to the care of biotopes and the landscape in the centre. Increasingly there was also a desire to replace the many coniferous monocultures , planted as a result of war, wartime reparations and times of crisis, with species rich site-specific mixed forests . On 20 July 1982 the Palatinate Forest Nature Park Association ( Verein Naturpark Pfälzerwald )

5187-424: The first sandstone formations, some 100 metres thick, were deposited in the area of today's Palatinate Forest; in particular, the rock units of the Rotliegendes and the Zechstein (about 256–251 million years ago) are important. At the beginning of the Germanic Triassic , i.e. from the Lower to the beginning of the Middle Triassic, there was (about 251–243 million years ago) a desert-like climate, so that as

5278-444: The formation of rock layers of different hardness. This resulted in the subgroups of lower, middle and upper bunter sandstone. These bunter sandstone formations were buried by various types of sediments in the adjacent sections of muschelkalk (243–235 million years ago) and keuper (234–200 million years ago), and also during the Jurassic (200–142 million years ago) and Cretaceous (142–66 million years ago). At

5369-420: The further impoverishment of the population. Occupations that the forest itself supported, such as lumberjacks , charcoal burners , rafters , resin burners (pitch boilers) and ash burners, supported only a meagre existence. After large population losses during the Thirty Years' War , the population was initially restored and stabilized in the late 17th century, initially as a result of settler migration from

5460-411: The highest points in the southwest. The category structure of the list is based on the concept for the natural region division of the Palatine Forest . The important summits of the range are annotated with their corresponding landscape subdivision and arranged according to their height in metres (m) above sea level (NHN) . The nearest settlement is given for lesser known hills or those for which there

5551-407: The landscape. The highest points on the German side of the Wasgau are the Rehberg (576.8 m) near Annweiler, the castle hill of the ruins of Wegelnburg (570.9 m) near Nothweiler , followed by the Hohe Derst (560.5 m) west of Bad Bergzabern and the Großer Eyberg (513.0 m) southwest of Dahn . The Hohe List (475.8 m) and Erlenkopf (472.1 m) near Eppenbrunn are

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5642-567: 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

5733-457: The last few decades have caused further structural problems, especially affecting remote communities in sparsely populated areas through population decline, aging and migration. At the same time, the forested highlands has gained increasing importance in the second half of the twentieth century as a place for recreation and leisure activities of special ecological status . This is reflected in various touristic concepts and activities to offer

5824-499: 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

5915-433: The lowland of the Kraichgau . Only the Burgundian Gate beyond the Vosges forms an orographically clear border on the left bank of the Rhine. The Palatinate Forest can be divided into three areas. The Palatinate Forest is a major (3rd level) natural region within the Palatine-Saarland Scarplands (a 2nd order major region) and runs south as far as the Col de Saverne , i.e. far into French territory, where it continues as

6006-401: 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

6097-451: The more habitable regions of what is now the Palatinate, taking place since the Neolithic period (5,500-4,500 BC), and especially in Celtic (800 to 10 BC) and Roman (10 BC to 450 AD) times, the mountains on the west bank of the Rhine were practically uninhabited and covered by dense, ancient forest until the end of the Migration Period (about 600 AD). After the Frankish conquests in the Early Middle Ages (7th to 10th century) took them to

6188-423: The mountains became rarer or were closed, as can be seen in the example of the footwear industry. Since its heyday in the 1950s and 1960s, globalization has seen the relocation of shoe production abroad, resulting in the almost total collapse of the industry, reinforced especially in the 1980s and 1990s by increasing unemployment and induced migration trends. In addition, the far-reaching demographic changes of

6279-409: The mountains were rapidly exhausted and over-population and poverty, in particular in the 19th century, led to increased emigration to the New World . Apart from the modest level of iron extraction and processing, work in the forests and the operation of paper mills , the shoemaking industry in the region Pirmasens was the only real source of income. This meant that the railway in the second half of

6370-412: 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

6461-435: The names used by the handbook has prevailed. The most important subordinate landscapes are listed with the aid of a map; the map only showing the names of well-known landscapes and only the more significant landscape boundaries. The name Pfälzerwald was first used in 1843 – when the Palatinate was part of the Kingdom of Bavaria – by foresters in the centrally-located municipality of Johanniskreuz , who used it to refer to

6552-454: The native population additional work and income opportunities and to assist in counteracting the structural changes described above. Whereas the Palatinate Forest was earlier seen mainly as a source of raw materials and energy supply, today, in addition to its recreation and leisure function, its ecological importance as a "special protected landscape" has come to the forefront. This change in attitude found visible expression, inter alia, through

6643-640: The nature park took over the Palatinate Forest Club (PWV). The 20 open shelters, built for walkers in log house style, were named "Fischer Huts" after the managing director of the Palatinate Forest Club, Ludwig Fischer. In the mid-1960s, the PWV came to the conclusion that the work required could not be done by volunteers and handed the management of the nature park to the Palatinate provincial government. By 1974, 3.7 million euros had been spent on improving recreational opportunities. Around 1975

6734-617: The northern and central Palatinate Forest are prominent hill "blocks" ( Bergklötze ) and elongated trapezium-shaped ridges, frequently with rocky summit areas (e. g. the Kesselberg , 661.8 m) whilst, in the western part of the range, plateau-like hill formations with clearings predominate. In the southeastern Palatinate Forest, by contrast, the sediments of the Rotliegendes and Zechstein (erosion surfaces), and especially resistant Trifels and Rehberg beds (conical hills) influence

6825-578: 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

6916-696: The northwestern Palatinate Forest from west-southwest to east-northeast into which the Forest descends in a clear escarpment, especially into the boggy lowland of the Landstuhl Bruch west of Kaiserslautern. To the west of the Großer Hausberg, the Westrich Plateau separates from the Palatinate Forest at the sharp southern boundary of the Landstuhler Bruch in a comparatively smooth transition. It reaches comparable heights in

7007-666: The official Dutch lithostratigraphy, the Buntsandstein is divided into the Lower and Upper Germanic Trias Groups . The British Bunter Formation is basically a continuation of the same unit. In Germany the Buntsandstein is subdivided into three subgroups with seven formations (from top to base): Upper Buntsandstein Middle Buntsandstein Lower Buntsandstein All of these are reasonably good reservoir rocks for oil and gas. In

7098-491: The old protected area regulation for the Palatinate Forest Nature Park (1984) and therefore overlaps with the other three zones. Core, buffer and transition zones are representatively distributed over the area of the biosphere reserve. As part of this, some 16 core zones were defined, together covering about 2.3 percent of the area. The source region of the Wieslauter (2,296 ha) being the largest of

7189-568: The region during the era of the Salian (10th-12th centuries) and Hohenstaufen (12th and 13th century) emperors, with the construction of Trifels Castle and other castles in the surrounding area that, for a time, made it the centre of power of the empire. This development took place in the Late Middle Ages (13th to 15th centuries) and Early Modern Period (16th to 18th century), because disease (e.g. The Plague ) and famine led to

7280-646: 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,

7371-579: 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

7462-443: 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

7553-605: The southeast. The southern Palatinate sandstone formations of the Zechstein are divided into four strata having a total thickness of about 80 to 100 metres. The rock unit of bunter sandstone is divided into three strata: Weathering and erosion of the different rock strata of the Palatine Forest with their variable hardness have resulted in a low mountain landscape with a dense, deeply incised system of valleys and wide variety of hill shapes. The hard and resistant rocks of

7644-519: The transition area, but as a muschelkalk plateau it has a significantly different relief and is no longer fully forested. It not only stretches around the western edge of the Palatinate Forest, but also further south around the Vosges. From the area of Lemberg in Lorraine, it also forms the watershed between the Moselle and the Upper Rhine; the southern part of the region being drained completely via

7735-401: The use of the forest to obtain firewood and timber did not follow the principles of sustainability . On the one hand, the production of straw ( foliage as bedding for cattle) and wood pasture damaged the soils and forests; on the other hand the manufacture of iron , glass and potash , which needed a lot of wood, led for centuries to the overuse and destruction of the forest and thus to

7826-545: The valley floor is wide and they are therefore especially well suited for the construction of ponds, or woogs , reservoirs and small lakes (see below). 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

7917-480: The woods of the bunter sandstone region of the Palatinate. Its use was extended when, in 1902, the Palatinate Forest Club ( Pfälzerwald-Verein or PWV) was founded, Fritz Claus, one of the pioneers of the PWV, in particular, strove to promote the name. A more precise, scientifically based definition of the Palatinate Forest as an independent natural region was introduced in 1911 by Daniel Häberle,

8008-627: Was covered by inland seas which deposited the Zechstein evaporites . At the end of the Permian a connection with the Paleo-Tethys Ocean to the south was formed in present-day southeast Poland, causing sea water to flow in periodically. This caused the inflow of more clastic material, which was deposited in the form of large alluvial fans . The same process happened in the Triassic for the Basque-Cantabrian Basin , in

8099-441: Was founded as a support organization. The members of the association are those counties and independent towns whose territories are covered by the nature park as well as the Palatinate regional association, various rambling and sports clubs and environmental organizations. Many social organisations are involved in the work of the nature park, ensuring the independence of academic and regional individual interests. The association's goal

8190-563: 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

8281-603: Was the discovery that its base lies actually in the latest Permian. The Buntsandstein was deposited in the Germanic Basin , a large sedimentary basin that was the successor of the smaller Permian Basin and spread across present day Poland , Germany, Denmark , the southern regions of the North Sea and Baltic Sea , the Netherlands and south England. In the late Permian this region had an arid climate and it

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