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78-457: The Bloskülb is a 570-metre-high hill in the central part of the Palatine Forest of Germany . It lies about three kilometres northwest of the village of Iggelbach . It is located entirely within the territory of the municipality of Elmstein . This Rhineland-Palatinate location article is a stub . You can help Misplaced Pages by expanding it . Palatine Forest Together with

156-553: 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,

234-672: A legacy of rhyolites near Dossenheim . At roughly the same time, the Central European plate began to tear apart so that the Upper Rhine Rift developed. Even as the Upper Rhine Rift valley still sinks today by just under a millimetre each year, the Odenwald, relatively to that, was uplifted to the height it has today. Along the faults, the small rivers Gersprenz and Weschnitz have, in part, carved their courses. The Upper Rhine Rift

312-537: 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

390-611: 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

468-400: 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

546-411: 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,

624-484: Is connected with monsters (knight Georg fights against the man-eating lindworm near Frankenstein-castle ) and creatures of nature with magic potency (a water spirit changed into a fox near Niedernhausen, the merwoman in the Meerwiese of Waldürn). Secondly the local legend is connected with the genre of the historic saga: a historic person or an original is portrayed anecdotally (the count of Erbach and Luther, resp.

702-546: Is known as a leisure destination easily accessible from the urban areas of Mannheim and Frankfurt . It is known for its clean thin air and was once known for its health sanitariums. There are many marked hiking paths through the rural areas. Wild blueberries , strawberries and mushrooms are to be found in the forests. The planned extension to the Odenwaldautobahn , that is, the A ;45 ( Dortmund – Aschaffenburg ),

780-507: 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

858-717: Is part of a fracture zone reaching from the Mediterranean Sea to Norway . Right on the edge of the Odenwald, it is roughly 2 500 m deep, but has been filled in to its current height by river and sea sediment, for until about 20 million years ago, the North Sea reached far inland, across the Wetterau Depression into the Rhine Valley. About 2500 BC, there is evidence that the Linear Pottery culture settled along

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936-692: 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

1014-521: 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

1092-750: 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

1170-537: The Raubacher Joggel , landgrave Ludwig VIII: of Hesse-Darmstadt, robber Hölzerlips ). Thirdly a local tale explains an etiological or original myth (aetiological saga). For example, there is explained: Beside these legends there are two famous and well-known Odenwaldsagas: In the Nibelungenlied (see also Nibelung ) the dragon slayer Siegfried , on a hunting trip (instead of a failed campaign) leading from

1248-465: 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

1326-618: The Burgundian city of Worms into the Odenwald, is murdered by Hagen of Tronje . Since no exact spot for this deed has been handed down, countless communities, especially in the Hessian Odenwald are squabbling over the right to call themselves “Siegfried’s Murder Site”, for example a spring near Gras-Ellenbach ( Siegfriedsbrunnen ), Mossautal-Hüttenthal Lindelbrunnen ) or Heppenheim ( Siegfriedbrunnen ). The ruins of Rodenstein (below-mentioned) and Schnellerts near Fränkisch-Crumbach are

1404-677: The Early Triassic layers. Furthermore, in the south near Heidelberg , there is still Zechstein under the Early Triassic deposits. Roughly 50 to 60 million years ago, volcanoes formed along the great geological faults . Still bearing witness to this time are the Otzberg , the Daumberg and the Katzenbuckel, all extinct volcanoes in the Odenwald. Furthermore, volcanism with acidic rocks has left

1482-986: The Hessisches Ried (the northeastern section of the Rhine rift) to the west, the Main and the Bauland (a mostly unwooded area with good soils) to the east, the Hanau-Seligenstadt Basin – a subbasin of the Upper Rhine Rift Valley in the Rhine-Main Lowlands – to the north and the Kraichgau to the south. The part south of the Neckar valley is sometimes called the Kleiner Odenwald ("Little Odenwald"). The northern and western Odenwald belong to southern Hesse, with

1560-651: 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

1638-539: 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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1716-519: 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

1794-675: 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

1872-621: The Triassic , about 200 million years ago, the land sank again, forming the Germanic Basin in which the metre-thick layers of red sandstone could build up . These were later covered over with layers of muschelkalk from a broad inland sea, then followed by sediments from the Late Triassic (or Keuper). The South German Cuesta Land thus formed. When the land in the Odenwald was uplifted again about 180 million years ago, more than 100 m of

1950-556: 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

2028-703: 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

2106-776: 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

2184-505: 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

2262-519: 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 ),

2340-496: 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

2418-728: 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

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2496-429: 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

2574-729: The Odenwald now lay in Roman-ruled Germania Superior . About 159, the Limes was shifted about 30 kilometres (19 miles) eastwards to the Miltenberg – Walldürn – Buchen - Osterburken line. In 260, Roman hegemony fell. The Alamanni were also thrusting into the Odenwald and settling the land between the Main and Neckar, after whom came the Franks . In the 5th century, the Franks, under Clovis I , divided

2652-434: 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

2730-600: 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

2808-443: 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

2886-494: 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

2964-699: 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

3042-443: 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

3120-445: 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

3198-427: 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

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3276-455: 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)

3354-489: 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

3432-418: 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

3510-446: 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 )

3588-424: 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

3666-445: 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

3744-421: 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

3822-411: 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

3900-482: The job of opening the empty woods up by the central Frankish power ( Carolingian ), Lorsch Abbey from the west, Fulda Monastery from the east and Mosbach Monastery from the south. Amorbach Monastery had the greatest importance for ecclesiastical, cultural and economic development in the eastern Odenwald. In the 9th century in the southeastern Odenwald near the now more thickly settled Bauland, settlements were established. The muschelkalk-new red sandstone mineral boundary

3978-434: The land up into districts. In the 7th and 8th centuries came Christianization by Irish - Scottish and Anglo-Saxon monks ( Pirmin , Boniface ). On the muschelkalk lands of today's Bauland, which favoured agriculture , a broad mesh of settlements arose. The parts of the Odenwald farther in from the rivers, though, with their scant New Red Sandstone soils remained uninhabited. Four Benedictine monasteries were assigned

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4056-407: 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

4134-458: 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

4212-433: 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

4290-451: 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

4368-424: 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

4446-409: 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

4524-441: 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

4602-454: 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

4680-516: 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

4758-404: The northern (Gersprenz) and southern (Neckar valley) edges of the Odenwald. About 400 BC, Celts (Gauls) settled throughout southern Germany. Almost all of the Odenwald was covered then with virgin forest , and the outer edges were not settled. Germanic peoples drove the Celts westwards across the Rhine to what is now France . About AD 100, the older Odenwald line of the Neckar-Odenwald Limes

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4836-498: 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

4914-451: 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

4992-432: 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

5070-408: 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

5148-452: 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

5226-435: The sedimentary layering, in parts, was eroded away down to the bedrock , as can still be seen in the western Odenwald. The bedrock here is composed of a number of different rocks, among them gneiss , granite , diorite , gabbro in the Frankenstein pluton , and so on. In the eastern Odenwald, the red sandstone is all that is left of the sedimentary mixture. Farther east in the Bauland, the muschelkalk deposits still overlie

5304-421: The setting of an Odenwald ghost story: during the night the knight Rodenstein (the Rodensteiner ) flies with a berserker-cornet through the air to prophesy the beginning of a war ( Wild Hunt motif). Countless streams rise in the Odenwald, the longest of which are the following: There are a few bodies of standing water in the Odenwald, among which are the following: Odenwald is twinned with: The Odenwald

5382-406: The south stretching into Baden . In the northeast, a small part lies in Lower Franconia in Bavaria. The Odenwald, along with other parts of the Central German Uplands, belongs to the Variscan , which more than 300 million years ago in the Carboniferous period ran through great parts of Europe . The cause of this orogeny was the collision of Africa ’s and Europe's forerunner continents. In

5460-483: 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

5538-408: 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

5616-401: 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

5694-513: 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). Odenwald The Odenwald ( German: [ˈoːdn̩valt] ) is a low mountain range in the German states of Hesse , Bavaria and Baden-Württemberg . The Odenwald is located between the Upper Rhine Plain with the Bergstraße and

5772-518: 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,

5850-555: Was built under Roman Emperor Trajan (98-117). This stretch of the Empire's border ran from Fort Wimpfen in the Valley ( Kastell Wimpfen im Tal ) northwards by way of the Forts of Neckarburken, the lesser forts of Trienz and Robern near Fahrenbach , Fort Oberscheidental, Fort Schloßau, Fort Hesselbach, Fort Würzberg, Fort Eulbach, Fort Hainhaus and Fort Hesselbach to Fort Wörth on the Main . Parts of

5928-407: Was crossed. The following are some theories about the origin of the name Odenwald : Linguists who research phonetic changes and the sound shifts reject theories no. 1 to 3 and prefer 4 or 5; some historians favor no. 2. The numerous Odenwald folk legends are mostly connected with historic geographic sites (castle, town, rock, road and so on) They relate: In some stories the local aspect firstly

6006-441: 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

6084-694: Was never realized. Nevertheless, all these Bundesstraßen run through the Odenwald: Furthermore, the Nibelungenstraße and the Siegfriedstraße run through the Odenwald, partly along the roads listed above. The Odenwald is home to many historic castles and palatial residences. In times past the fortresses on the top of the Odenwald mountains controlled Bergstraße and the Weschnitz-, the Gersprenz-,

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