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79-754: Wollersheim lies on the northern edge of the Eifel mountains. The fertile lands of the Zülpich Börde border the village. Around Wollersheim is a geological and botanical feature: the muschelkalk kuppen , which are home to numerous rare species of limestone pastures. Southwest of the village rises the Neffelbach stream. Wollersheim is bounded by the villages of Embken , Langendorf (municipality of Zülpich ), Eppenich (municipality of Zülpich), Vlatten (municipality of Heimbach ) and Berg-Thuir . An immense number of archaeological finds point to an early settlement of

158-530: A referendum except those in the administrative district of Palatinate won the necessary majority; however, almost 20 years passed before the referendums finally took place. On 19 January 1975, none of the regions concerned returned a majority for being transferred to another state. This put an end to decades of discussion. Only the AKK conflict , a dispute over the districts of Mainz-Amöneburg , Mainz-Kastel , and Mainz-Kostheim , has continued to exercise politicians up to

237-662: A SW-NE direction far beyond the Rhine valley. Since that folding, the Eifel has largely remained part of the mainland. During the Permian , after the end of the uplifting, the Variscan mountains were heavily eroded, leaving only a relatively flat, truncated upland. For a short time, and only partially, this was later flooded by the sea. Depositions from the Triassic and Jurassic periods have survived in

316-456: A chain from northwest to southeast. The youngest maars are only slightly older than 11,000  years. In the eastern Eifel, volcanism began about 500,000 years ago in the area of today's Laacher See; it extended to the Neuwied Basin to the south, and crossed the Rhine to the east. The quantity of basalt lavas, pumice tuffs and ash tuffs produced by the volcanoes was far greater here than in

395-486: A distinctly stimulating climate; the high elevations being considered as highly stimulating. The Eifel is a clean air area with very low air-chemical pollution. On hot sunny days, there is sometimes an increased concentration of ground-level ozone. Here are a couple of weather station examples for settlements in the Eifel. At the time of the Roman Empire the whole mountain range between the rivers Rhine, Meuse and Moselle

474-445: A recent cultivar , is the leading red grape cultivated on 7,626 hectares (18,840 acres), which is more than a third. Blauer Portugieser (4,446 hectares (10,990 acres)) and Spätburgunder (3,867 hectares (9,560 acres)) show also appreciable cultivated shares. In addition, Pinot blanc , Pinot gris , Chardonnay as white varieties and Regent and St. Laurent as red varieties have been increasing their share, as

553-528: Is a common occasion. The deep Valleys of Rhine and Moselle with an oceanic climate (Köppen climate classification: Cfb ). Summers are hot and moist, while winters are cool. Freezing temperatures are rare and snow usually melts within hours. The mild climate allows palm trees , fig trees , stone pines , oleander shrubs, olive trees , almond trees and other exotic plants to be grown in this area. The forests in this region are home to common pests such as Melolontha Hippocastrani , that cause damage to

632-491: Is a western state of Germany . It covers 19,846 km (7,663 sq mi) and has about 4.05 million residents. It is the ninth largest and sixth most populous of the sixteen states. Mainz is the capital and largest city. Other cities are Ludwigshafen am Rhein , Koblenz , Trier , Kaiserslautern , Worms , and Neuwied . It is bordered by North Rhine-Westphalia , Saarland , Baden-Württemberg and Hesse and by France, Luxembourg and Belgium . Rhineland-Palatinate

711-419: Is an average of 70 days of full snow cover because the frequency of snow at higher elevations is relatively high (for comparison: Bitburg 35  days, Maifeld 30  days), but the level of snowfall varies from year to year. Snow heights vary on average between 15 cm and 60 cm. The humid Atlantic climate can cause extreme variations though: on 2 March 1987 there was 227 centimetres of snow in

790-803: Is derived from Saint Willibrord . As early as 1184 a ladies house ( Frauenhof ) is mentioned for the Cologne foundation of St. Maria im Kapitol . In 1388 the French king, Charles VI and the Duke of Jülich signed the Treaty of Wollersheim ( Wollersheimer Frieden ) here. On 1 January 1972 Wollersheim was incorporated into the new borough of Nideggen. According to the decision of the Oberverwaltungsgericht dated 4 August 1972 Wollersheim remained in Nideggen, and temporarily lost

869-575: Is now regarded as the standard work on the geology of the Eifel. The Eifel and its western continuation into Belgium, the Ardennes , are the remains of a Variscan truncated upland , much of it 400 million years old, that is part of the Rhenish Massif ( Rheinisches Schiefergebirge ). In the area of the Stavelot-Venn Saddle ( Hohes Venn ) are the oldest layers of rock, which originate from

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948-690: Is the most forested state along with Hesse. The state's major rivers are the Rhine, including the UNESCO World Heritage Site Middle Rhine , and the Moselle . Several crater lakes of volcanic origin are in the Eifel , the largest of which is the Laacher See . Climatically, Rhineland-Palatinate can be divided into two areas: The Rhenish Massif with a typically humid continental climate (Dfb). Summers here are usually warm with much precipitation and winters tend to be dry and cold. Snowfall

1027-564: Is the renowned Schloss Wachenheim Group. This company is headquartered in Trier, with operations in several locations in Rhineland-Palatinate and three sites in France (Compagnie Française des Grands Vins (CFGV)). Other renowned sparkling wine producers such as Kupferberg , Deinhard , and Henkell also had their roots in the region, but now belong to companies outside the state as

1106-655: Is west/southwest. A relatively dry and milder climate prevails in the wind and rain shadow of the High Eifel. Cold air from Siberia in the higher elevations of the Eifel has less of an impact on weather conditions, as the proximity of the Atlantic Ocean to the Eifel brings milder sea air to the Eifel even in winter. Looking at the long-term averages, even the Snow Eifel only has snow cover for nine consecutive days in winter, as there are no longer lasting cold spells. However, there

1185-677: The Archdiocese of Cologne . Around Wollersheim a lot of Eifel barley is grown for the brewing industry. From 1791 to 1987 the Cramer Brewery brewed beer in Wollersheim itself. Eifel The Eifel ( German: [ˈaɪfl̩] ; Luxembourgish : Äifel , pronounced [ˈæːɪfəl] ) is a low mountain range in western Germany , eastern Belgium and northern Luxembourg . It occupies parts of southwestern North Rhine-Westphalia , northwestern Rhineland-Palatinate and

1264-551: The Cambrian and are around 550 million years old. The Eifel is one of the few volcanically active areas of Germany, as is evinced by numerous discharges of carbonic acid , for example into the Laacher See . The last eruptions, which gave rise to the most recent maars , occurred about 11,000  years ago. The basement in the Eifel, as in the other regions of the Rhenish Massif , consists mainly of Devonian slates , sandstones and limestones , laid down in an ocean south of

1343-782: The German Wildlife Route and the South Eifel Holiday Route. Due to its moist and mild Atlantic climate, the Eifel is bisected by numerous streams and small rivers. Impoundment of these streams, especially in the North Eifel has led to the creation of very large reservoir , such as the Rursee , which is the second largest in Germany by volume, and the Urftsee . A feature of the Eifel are its natural lakes of volcanic origin. The largest,

1422-558: The Handbook of the Natural Region Divisions of Germany , divided into three major unit (i.e. two-digit) groups and these were subdivided into (three-digit) major natural units. These divisions were subsequently refined in the individual map sheets Trier/Mettendorf , Cochem (both 1974) and Cologne/Aachen (1978) as follows; for the most detailed natural region divisions in Rhineland-Palatinate, fact files were produced by

1501-598: The Laacher See , is a collapsed, water-filled caldera , whilst the many maars are water-filled volcanic eruption bowls. The largest maar lake is the Pulvermaar . The Meerfelder Maar has an even bigger basin, but three-quarters of it has silted up. The many rivers and streams of the Eifel drain into the North Sea via the great rivers outside of the Eifel: the Rhine (and its tributary,

1580-675: The Matronae Veteranehae . Wollersheim Heath was reputedly the scene of the Battle of Zülpich in AD 496 between the Franks under Clovis I and the Alemanni , although many historians now doubt this. The settlement named by Gregory of Tours as Tulbiac may have been somewhere to the south because there were simply not Alemanni this far north. Wollersheim was first recorded in 1231 as Wolrisheim . The name

1659-517: The Moselle ) and the Meuse (with its tributaries, the Rur and Ourthe ). The rivers and streams within the mountain range, together with their larger tributaries, are as follows: Rhine tributaries: Meuse tributaries: Reservoirs Volcanic lakes Despite the interesting geology of the Eifel region, only three comprehensive geological accounts have been produced. In 1822, Johann Steiniger published

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1738-586: The Old Red Continent and folded and overthrust in the Variscan orogeny. Only on the northern edge of the Eifel, in the High Fens and its environs, do older rocks from the Cambrian and Ordovician outcrop. Rocks of the Carboniferous do not occur in the Eifel itself, but lie along its northern boundary in the region of Aachen . The Devonian rocks were deposited in an oceanic basin , in which erosion debris

1817-747: The Pennsylvania Dutch , Maryland Palatines , Ohio Rhinelanders , and Missouri Rhinelanders . The state of Rhineland-Palatinate was founded shortly after the Second World War , on 30 August 1946. It was formed mainly from the southern part of the Prussian Rhine Province (the Regierungsbezirke of Koblenz and Trier ), from Rhenish Hesse , from the western part of Nassau and the Bavarian Rhenish Palatinate minus

1896-562: The Saar Protectorate until the latter was returned to German control in 1957. Rhineland-Palatinate's natural and cultural heritage includes the extensive Palatinate winegrowing region, picturesque landscapes, and many castles and palaces . Rhineland-Palatinate is currently the only federal state in Germany where nuclear weapons are stored extraterritorially under the responsibility and supervision of US forces . Several German-American ethnicities originated from this state, such as

1975-526: The Saarland from joining Rhineland-Palatinate. Mainz was named as the state capital in the regulation; the "Mixed Commission" ( Gemischte Kommission ), named as the highest organ of state charged with the administration of the new state and with the preparation of an advisory state assembly, started its work in Mainz. However war damage and destruction meant that Mainz did not have enough administrative buildings, so

2054-714: The Schwarzer Mann in the Schnee-Eifel , stand out from a long way off as long, forested ridges or clearly isolated mountaintops. The highest mountain in the whole Eifel is the Hohe Acht at 746.9 m. It is the only Eifel summit above 700 m. However, many peaks, mountain ridges and large regions, such as the Zitterwald reach heights of over 600 m. These include two dozen peaks with good all-round views, of which many have an observation tower . From north to south they are:

2133-451: The diphthong and the syllable , -fel . The resulting root form Anfil or Anfali would then mean an "area that is not so level". An - would then be a prefix and -fali , which is related to the Slavic polje ("field"), means "plain" or "heath". W. Kaspers (1938) deduces from the surviving form in pago aquilinse the root form aku-ella, akwella and points to its development into

2212-633: The minister president of the new state by the French military government. Adolf Süsterhenn submitted to the Advisory State Assembly a draft constitution, which was passed after several rounds of negotiation on 25 April 1947 in a final vote, with the absolute majority of the CDU voting for and the SPD and KPD voting against. A point of contention involved the draft constitution providing for separate schools based on Christian denomination. On 18 May 1947, 53% of

2291-514: The "backbone" of the economy in Rhineland-Palatinate. The principal employer is the chemical and plastics processing industry, which is represented by BASF in Ludwigshafen . Boehringer , BioNTech , Joh. A. Benckiser , SGE Deutsche Holding, and Schott Glassworks conclude the top five companies in the state. Rhineland-Palatinate is Germany's leading producer of wine in terms of grape cultivation and wine export. Its capital, Mainz, may be called

2370-456: The Americans to the French. To begin with, the French divided the region provisionally into two "upper presidiums" ( Oberpräsidien ), Rhineland-Hesse-Nassau (for the hitherto Prussian government districts and regions of Koblenz , Trier , and Montabaur ) and Hesse-Palatinate (for the hitherto Bavarian Palatinate and old Hessian-Darmstadt province of Rhenish Hesse ). The formation of the state

2449-683: The Constitutional Court and the State Archives. In addition, the German Federal Archives and Federal Office of Hydrology were established in Koblenz in 1952. A sense of community developed only very gradually in the "land of the retort", which had been established largely without regard to the historical affiliations of its inhabitants. It was given little chance of survival, especially as it had very few large industrial centres. However,

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2528-506: The Earth's surface from the upper regions of the Earth's mantle or, in the majority of cases, gathers in a magma chamber, several tens of kilometres deep, at the base of the Earth's crust , from which magma rises at irregular intervals and causes volcanic eruptions. Volcanism in the Eifel is thought to be partly caused by the Eifel hotspot , a place where hot material from deep in the mantle rises to

2607-477: The Eifel on the Weißer Stein . The mean temperature in the coldest month (January) is -1.5 °C at high elevations, +1.5 to 2 °C in the mountain foreland. There is an average of 110 days of frost, with temperatures below 0 °C in the highlands and an average of 30 to 40 'ice days' when temperatures do not rise above 0 °C. The warmest month (July) only has an average temperature of 14 °C in

2686-564: The High Eifel came to an end about 15 to 20 million years ago, at the same time as that of the Siebengebirge. Volcanism in the western and eastern Eifel is, in contrast to that of the High Eifel, much more recent than that of the Siebengebirge and Westerwald. It began in the West Eifel region of Daun, Hillesheim and Gerolstein about 700,000 years ago and created a chain of ash volcanoes, cinder cones , maars and craters running in

2765-903: The Michelsberg, Häuschen and Teufelsley in the north; the Adert, Hohe Acht and Raßberg in the northeast; the Hochkel, Nerotherkopf, Dietzenley and ruins of the Kasselburg in the central area; the Prümer Kalvarienberg, Hartkopf and Prümer Kopf in the east, the Steineberg and Mäuseberg near Daun, the Hochsimmer and Scheidkopf near Mayen; the Eickelslay and Absberg in the southeast; and the Krautscheid and Hohe Kuppe in

2844-655: The Prussian Rhine Province ), the parts of the Province of Rhenish Hesse ( Rheinhessen ) west of the River Rhine and belonged to the People's State of Hesse ( Volksstaat Hessen ), parts of the Prussian province of Hesse-Nassau ( Montabaur ), and the former Oldenburg region around Birkenfeld ( Principality of Birkenfeld ). On 10 July 1945, the occupation authority on the soil of the present-day Rhineland-Palatinate transferred from

2923-679: The area around Hillesheim and Oberbettingen . In the Upper Cretaceous and during the Tertiary , the Eifel was inundated mainly from the north. Remains of Cretaceous rocks were discovered on the High Fens. Scattered patches of Oligocene deposits can be found there and in the Western Eifel. From the Pliocene onwards, the Rhenish Massif, including the Eifel, experienced an uplift. This led to

3002-430: The area. In 1931/32 in the source region of the Neffelbach, six pottery kilns and several sandstone wells were excavated. Even the name of a pottery owner has survived. On one of the shards of pottery from the 2nd century AD is the name Verecundus . On the nearby Pützberg hill and in the vicinity of Gödersheim Castle , Roman skeleton graves and matronae stones from the Roman era were found which were dedicated to

3081-419: The basis of a significant mining activity for the extraction of building materials since Roman times. Some of the hills are volcanic vents. The peculiar circle-shaped lakes ( maars ) of the volcanic regions formed in volcanic craters. The first volcanic eruptions took place in the early Tertiary centred in the High Eifel and even before the volcanic activity of the Siebengebirge and Westerwald . Volcanism in

3160-522: The capital of the German wine industry, being the home of the German Wine Institute, the German Wine Fund in the Haus des Deutschen Weines (House of German Wine), and the Verband Deutscher Prädikatsweingüter (VDP) Wine Bourse, which brings together the top winemakers of Germany and the wine merchants of the world. Of 13 wine regions producing quality wine in Germany, six ( Rheinhessen , Pfalz , Mosel , Nahe , Mittelrhein , and Ahr ) are located in Rhineland-Palatinate, with 65 to 70% of

3239-497: The center of Jewish life during medieval times. The Takkanot Shum ( Hebrew : תקנות שו"ם ), or Enactments of ShU"M were a set of decrees formulated and agreed upon over a period of decades by their Jewish community leaders. Today, there are approximately 20,000 Jews (0.5% of the population) living in the state. The gross domestic product (GDP) of the state was 147.0 billion euros in 2018, accounting for 4.4% of German economic output. GDP per capita adjusted for purchasing power

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3318-399: The cities of Aachen to the north, Trier to the south and Koblenz to the east. It descends in the northeast along a line from Aachen via Düren to Bonn into the Lower Rhine Bay . In the east and south it is bounded by the valleys of the Rhine and the Moselle . To the west it transitions in Belgium and Luxembourg into the geologically related Ardennes and the Luxembourg Ösling . In

3397-412: The control of the Franks , to the control of the Holy Roman Empire , and saw fighting during the First and Second World Wars. The present state of Rhineland-Palatinate formed part of the French Zone of Occupation (1945–1949) after the Second World War. It comprised the former Bavarian Palatinate, the Regierungsbezirke ("government districts") of Koblenz and Trier (which formed the southern part of

3476-409: The county of Saarpfalz . The Joint German-Luxembourg Sovereign Region ( Gemeinschaftliches deutsch-luxemburgisches Hoheitsgebiet ) is the only unincorporated area of the state of Rhineland-Palatinate. This condominium is formed by the rivers Moselle , Sauer , and Our , where they run along the border between Luxembourg and Rhineland-Palatinate or the Saarland. The region has a vast history, from

3555-490: The edge of the Eifel and formed larger valleys. The Eifel covers an area of 5,300 km and is geographically divided into the North and South Eifel. It is further divided into several natural regional landscapes, some with further subdivisions. Since 2004, part of the North Eifel has been designated as the Eifel National Park . There are also four nature parks in the Eifel (from north to south): Rhineland , High Fens-Eifel , Volcanic Eifel , and South Eifel , although

3634-420: The electorate adopted the Constitution for Rhineland-Palatinate in a referendum . While the Catholic north and west of the new state adopted the constitution by a majority, the majority in Rhenish Hesse and the Palatinate voted against it. On the same date the first elections took place for the state parliament, the Landtag of Rhineland-Palatinate . The inaugural assembly of parliament took place on 4 June 1947 in

3713-464: The establishment of numerous military bases, both Allied and Bundeswehr , helped to some extent to boost the economy. In 1956, under Article 29 of the Basic Law for the Federal Republic of Germany , petitions were made in the regions of Koblenz, Trier, Montabaur, Rhenish Hesse, and Palatinate for their separation from the state and incorporation into the respective states of North Rhine-Westphalia, Hesse, Bavaria, and Baden-Württemberg. All petitions for

3792-412: The first extends only partly into the northern foothills of the Eifel. There are several distinct chains within the Eifel. Since 2004, about 110 km of the Eifel within the German state of North Rhine-Westphalia have been protected as the Eifel National Park nature reserve . Up to 1960, the German part of the Eifel, which belonged to the natural region of the Rhenish Massif , was, according to

3871-424: The first geological map of the area and, in 1853, the Geognostische Beschreibung der Eifel . In 1915 Otto Follmann published a new account, adding to the extent of scientific understanding at that time, the Abriss der Geologie der Eifel ("Abstract of the geology of the Eifel region". In 1986, Wilhelm Meyer finally published the volume, Geologie der Eifel ("Geology of the Eifel"), whose fourth, revised, edition

3950-575: The foliage and soil. The Rhenish Massif forms roughly the northern half of the state, including the regions Eifel, Moselle Valley , Hunsrück , Westerwald , and parts of the Taunus . The Palatinate forms the biggest part of the southern half along with Rhenish Hesse . The Nahe Valley separates both parts. Rhineland-Palatinate is divided into 24 districts ( Landkreise ), 12 independent cities ( Kreisfreie Städte ). Listing with Vehicle registration plates of Germany Listing with Vehicle registration plates of Germany The following table shows

4029-535: The growing conditions improve in Rhineland-Palatinate. The state supports the wine industry by providing a comprehensive consultancy and education program in the service supply centers (German: DLR ) of the land. The Geilweilerhof Institute for Grape Breeding is fully financed by the state. Many well-known new varieties such as Morio-Muskat , Bacchus , Optima , and Regent have been created in these institutes. The worldwide leader in sparkling wine production, producing 224,4 million bottles in 2017/18,

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4108-450: The headquarters of the state government and parliament was provisionally established in Koblenz . On 22 November 1946, the constituent meeting of the Advisory State Assembly ( Beratende Landesversammlung ) took place there, and a draft constitution was drawn up. Previously, local elections had been held. Wilhelm Boden was (after a short term of office as the Oberregierungspräsident of Rhineland-Hesse-Nassau) nominated on 2 December as

4187-447: The higher areas. The level of precipitation decreases significantly from west to east as a result of the rain shadow of the highlands. So the Schneifel receives an average of 1,200 mm of precipitation ( High Fens : 1,400 mm to 1,500 mm), while in Maifeld the average rainfall is only 600 mm. The bioclimatic conditions in the Eifel are favourable. Heat stress and air humidity are rarely present in summer. The Eifel has

4266-456: The large city hall at Koblenz . Wilhelm Boden was elected the first minister-president of Rhineland-Palatinate. Just one month later, Peter Altmeier succeeded him. The constitutional bodies – the Government ( Landesregierung ), the Parliament ( Landtag ) and the Constitutional Court ( Verfassungsgerichtshof ) – established their provisional seat in Koblenz. In the following period, Koblenz and Mainz each emphasized their suitability as

4345-641: The name "Eifel" in the following sequence: aquila  > agfla  > aifla  > eifla  > Eifel . Akuella derives from the pre-German and means "land with summits" or "land with peaks". Rhineland-Palatinate Rhineland-Palatinate ( / ˌ r aɪ n l æ n d p ə ˈ l æ t ɪ n ɪ t , - l ə n d -/ RYNE -land pə- LAT -in-it, -⁠lənd- , US also /- ɪ n eɪ t / -⁠in-ayt ; German: Rheinland-Pfalz [ˈʁaɪnlant ˈpfalts] ; Luxembourgish : Rheinland-Pfalz [ˈʀɑɪnlɑm ˈpfɑlts] ; Palatine German : Rhoilond-Palz )

4424-442: The north it is limited by the Jülich-Zülpicher Börde . Within Germany it lies within the states of Rhineland-Palatinate and North Rhine-Westphalia; in the Benelux the area of Eupen , St. Vith and Luxembourg. Its highest point is the volcanic cone of the Hohe Acht (746.9 m). Originally the Carolingian Eifelgau only covered the smaller region roughly around the sources of the rivers Ahr , Kyll , Urft and Erft . Its name

4503-399: The northern and northwestern foothills of the present Eifel in the eastern half of the Arduenna silva of the Romans. West of the Eifelgau lay the Ardennengau , whose name was derived from Arduenna silva . Following the end of the Frankish Empire the name of the old gaue continued to be used in popular language. Over the centuries an ever-larger region was referred to as the Eifel. Today

4582-427: The option open of annexing further areas west of the Rhine after the Saarland was turned into a protectorate . When the Americans and British, however had led the way with the establishment of German states, the French came under increasing pressure and eventually followed their example by setting up the states of Baden , Württemberg-Hohenzollern, and Rhineland-Palatinate. However the French military government forbade

4661-466: The present day. Rhineland-Palatinate shares international borders with France ( Grand Est ), Luxembourg ( Clervaux , Diekirch , Echternach , Grevenmacher , Remich , and Vianden ), and Belgium ( Wallonia ). Within Germany, its neighbours are Baden-Württemberg , Hesse, North Rhine-Westphalia , and the Saarland . It is the ninth-largest state by area. Rhineland-Palatinate is part of the SaarLorLux euregion. With 42% of its area covered by forests, it

4740-399: The production of wine grapes in Germany having their origin within the state. About 13,000 wine producers generate 80 to 90% of the German wine export. The total estimated production from the six Rhineland-Palatinate regions was nearly 7 million hectoliters in 2018. Traditional grape varieties and a wide range of varieties developed during the last 125 years are characteristic for

4819-448: The region. Classical white varieties are cultivated at 63,683 hectares (157,360 acres). These comprise the famous Rieslings 14,446 hectares (35,700 acres), Müller-Thurgau (8,663 hectares (21,410 acres)), Silvaner (3,701 hectares (9,150 acres)), and Kerner (3,399 hectares (8,400 acres)). The share of red varieties grew constantly during the last decades and amounts to 20,000 hectares (49,000 acres). Dornfelder ,

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4898-437: The so-called Eifel North-South Zone. This is a region of subsidence , which runs from the Trier Bay in the south to the Lower Rhine Bay in the north. Through this zone existed at one time a sea link between north and south Central Europe. The remains of the sediments laid down at this time have survived to a greater extent in the Maubach- Mechernich Triassic Triangle in the north and in the Oberbettingen Triassic Graben in

4977-435: The southern area of the German-speaking Community of Belgium . The Eifel is part of the Rhenish Massif ; within its northern portions lies the Eifel National Park . The Eifelian stage in geological history is named after the region because rocks of that period reach the surface in the Eifel at the Wetteldorf Richtschnitt outcrop. The inhabitants of the Eifel are known as Eiflers or Eifelers . The Eifel lies between

5056-424: The southwest. The mountains and hills of the Eifel include the following (in order of height in metres above sea level ): (near Schwarzer Mann ) For a list of these and other Eifel mountains and hills see the List of mountains and hills of the Eifel . Many of these prominent points are linked by the Eifel-Ardennes Green Route , which crosses the east and south of the region, the German Volcano Route ,

5135-500: The state capital in a public debate. From the beginning, Minister-President Altmeier pressed for Mainz as the capital because he knew that the south of the country, especially the Palatinate, would not accept Koblenz, which was far to the north and formerly Prussian. On 16 May 1950, the Landtag decided to relocate itself and the Landesregierung from Koblenz to Mainz. After the government and parliament moved to Mainz, many state authorities and courts remained in Koblenz, including

5214-421: The state information system of the conservation administration (LANDIS): The BfN groups the 3 (two-digit) major unit groups under the combined group designated D45 . Apart from its valleys, the Eifel is a gently rolling plateau from which elongated mountain ridges and individual mountains rise. The majority of these summits do not attain a great height above the surrounding terrain. Several, however, like

5293-563: The streams and rivers cutting into the gently rolling landscape resulting in the present appearance of the low mountain range with its flat plateaus and deeply incised valleys. Due to numerous recent research projects, climate changes since the last ice age can be traced in detail in the Eifel region. Volcanic activity in the Eifel began 50 millions of years ago and continues into the geological present. It created numerous volcanic structures, lava flows and extensive layers of volcanic ejecta made of tuff and pumice , which have formed

5372-491: The surface, and partly by melt-ascent at deep fractures in the Earth's crust. Research has shown that the volcanism is still active; the Eifel region is rising by 1–2 mm per year and there are escaping gases, for example, carbon dioxide (CO 2 ) in the Laacher See . The Eifel is in the Atlantic climate zone with its relatively high precipitation; winters that are moderately cold and long with periods of snow; and summers that are often humid and cool. The prevailing wind

5451-441: The ten largest cities of Rhineland-Palatinate: In 2018, 40.3% of the population of the state adhered to the Roman Catholic Church and 26.8% to the Protestant Church in Germany ; 32.9% of the population was irreligious or adheres to other religions. Muslims made up 5.0% of the total. The league of ShUM-cities in the later Rhineland-Palatinate comprised the Jewish communities of Mainz, Speyer , and Worms , which became

5530-408: The title of "town" ( Stadt ). The village has two church buildings , the Old Church , whose oldest parts date to the 11th century, and the New Church of 1900 to 1903. In 1958 the Old Church was to be dismantled and moved to the open air museum at Kommern . However the villagers opposed this. The Old Church is one of the oldest sacred buildings in the county of Düren. Wollersheim belongs to

5609-401: The western Eifel. East Eifel volcanism came to an end with a huge eruption, as a result of which the magma chamber emptied and collapsed, creating a caldera . Today's Laacher See formed in the caldera. The ashes from the eruption can be detected today in deposits all over Central Europe and as far as Bornholm as a thin layer. Volcanism is caused by magma , which either rises directly to

5688-596: The western part of the plateau. In the eastern part, in the High Eifel and Volcanic Eifel , individual cinder cones and basalt kuppen , like the Hohe Acht and the Ernstberg , emerged as a result of volcanicity in the Tertiary and Quaternary periods and rise above the undulating countryside. The rivers draining into the Moselle , Rhine and Meuse , such as the Our , Kyll , Ahr , Brohlbach and Rur , have cut deep into

5767-658: The whole German-speaking part of the range between the Rhine, Meuse and Moselle is called the Eifel (including several areas outside of Germany, see the →  Belgian Eifel ), while the French-speaking part in Belgium and France is called the Ardennes . 762 Eifflensis pagus , 772 Eiffelnsis pagus , 804 in pago aquilinse , 838 Eifla , 845 Eiflensis pagus , 855 Eiflinsis pagus , 860–886 Agflinse , 975 Aiflensis pagus , 1051 Eiffila , 1105 Eifla , 1121 Eifla Müller/Schnetz (1937) believe that an -n- has dropped out between

5846-524: Was 33,100 euros or 110% of the EU27 average in the same year. The GDP per employee was 102% of the EU average. Rhineland-Palatinate leads all German states with an export rate around 50%. Important sectors are the winegrowing , chemical , pharmaceutical , and auto parts industries . "Distinctive regional industries" includes gemstones , ceramics and glass, and leather. Small and medium enterprises are considered

5925-669: Was called Arduenna silva ("high forest"). The oldest record of the name "Eifel" does not occur until the Early Middle Ages . Following the collapse of the West Roman Empire , the Frankish Empire emerged in the territories of present-day France and western Germany. This was divided into gaue (Lat.: pagi ). One of them, the Eifelgau , covered the source regions of the rivers Erft , Urft , Kyll and Ahr , i.e. predominantly

6004-545: Was established in 1946 after World War II , from parts of the former states of Prussia (part of its Rhineland and Nassau provinces ), Hesse ( Rhenish Hesse ) and Bavaria (its former outlying Palatinate kreis or district), by the French military administration in Allied-occupied Germany . Rhineland-Palatinate became part of the Federal Republic of Germany in 1949 and shared the country's only border with

6083-521: Was more recently transferred to the entire region. The Eifel belongs to that part of the Rhenish Massif whose rolling plateau is categorised as peneplain highland ( Rumpfhochland ), which was formed by the erosion of the ancient mountains of the Variscan mountain building phase and subsequent further uplifting. Individual mountain chains, up to 700 m, such as the Schneifel and High Fens , run through

6162-535: Was ordained on 30 August 1946, the last state in the Western Zone of Occupation to be established, by Regulation No. 57 of the French military government under General Marie-Pierre Kœnig . It was initially called Rhenish-Palatinate ( Rheinpfälzisches Land or Land Rheinpfalz ); the name Rhineland-Palatinate ( Rheinland-Pfalz ) was first confirmed in the constitution of 18 May 1947. The provisional French government at that time wanted originally to leave

6241-733: Was washed in from the north from the great north continent of Euramerica ( Laurussia or the Old Red Continent ) which was formed by Caledonian mountain building during the Silurian . From the end of the Lower Carboniferous the sea basin was caught up in the Variscan mountain building process, pushed together and uplifted, and thus formed part of the Variscan mountain system that, in the Upper Carboniferous and early Permian , covered large areas of Europe. The Eifel geological structures like main folds and overthrusts can be traced in

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