Misplaced Pages

#128871

91-778: To the west, as well as to the north and south-west of Mayen, is the country landscape of the Eifel . To the east, the landscape flattens out, running towards the Koblenz-Neuwied Basin, which is divided into the northern section of the Pellenz and the southern section of the Maifeld . This area is geographically considered to be part of the Eifel. Mayen is often called ‘The Gateway to the Eifel’. The small river Nette runs through

182-545: A border with North Rhine-Westphalia: North Rhine-Westphalia has a population of approximately 18.1 million inhabitants (more than the entire former East Germany , and slightly more than the Netherlands ) and is centred around the polycentric Rhine-Ruhr metropolitan region , which includes the industrial Ruhr region with the largest city of Dortmund and the Rhenish cities of Bonn , Cologne and Düsseldorf . 30 of

273-515: 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

364-792: A deep of 293 m below sea level. At the same time, this is the deepest human-made dip in Germany. The most important rivers flowing at least partially through North Rhine-Westphalia include: the Rhine , the Ruhr , the Ems , the Lippe , and the Weser . The Rhine is by far the most important river in North Rhine-Westphalia: it enters the state as Middle Rhine near Bad Honnef, where still being part of

455-492: 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

546-562: A framework of a federal parliamentary representative democratic republic. The two main parties are, as on the federal level, the centre-right Christian Democratic Union and the centre-left Social Democratic Party . From 1966 to 2005, North Rhine-Westphalia was continuously governed by the Social Democrats or SPD-led governments. The state's legislative body is the Landtag ("state parliament house"). It may pass laws within

637-544: A general election to elect at least 181 members of the Landtag. Only parties who win at least 5% of the votes cast may be represented in parliament. The Landtag, the parliamentary parties and groups consisting of at least 7 members of parliament have the right to table legal proposals to the Landtag for deliberation. The law that is passed by the Landtag is delivered to the Minister-President, who, together with

728-824: 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 , 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

819-627: A relatively small part of Westphalia, consisting instead mostly of Hessian and Eastphalian regions. After the Congress of Vienna , the Kingdom of Prussia received a large amount of territory in the Westphalian region and created the province of Westphalia in 1815. The northernmost portions of the former kingdom, including the town of Osnabrück , had become part of the states of Hanover and Oldenburg . The flag of North Rhine-Westphalia

910-618: 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 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

1001-617: 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 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

SECTION 10

#1732771969129

1092-419: 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

1183-643: Is below the national average in GRDP per capita . The state of North Rhine-Westphalia was established by the British military administration 's "Operation Marriage" on 23 August 1946 by merging the province of Westphalia and the northern parts of the Rhine Province , both being political divisions of the former state of Prussia within the German Reich . On 21 January 1947, the former state of Lippe

1274-568: Is divided almost equally between Catholicism and Protestantism. After the defeat of the Prussian Army at the Battle of Jena-Auerstedt , the Treaty of Tilsit in 1807 made the Westphalian territories part of the Kingdom of Westphalia from 1807 to 1813. It was founded by Napoleon and was a French vassal state . This state only shared the name with the historical region; it contained only

1365-505: 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 the first extends only partly into the northern foothills of the Eifel. There are several distinct chains within

1456-510: Is green-white-red with the combined coats of arms of the Rhineland (white line before green background, symbolizing the river Rhine), Westfalen (the white horse) and Lippe (the red rose). After the establishment of North Rhine-Westphalia in 1946, the tricolor was first introduced in 1948, but was not formally adopted until 1953. The plain variant of the tricolor is considered the civil flag and state ensign, while government authorities use

1547-593: Is hosted in Cologne . It is the largest video game convention in Europe. North Rhine-Westphalia has always been Germany's powerhouse with the largest economy among the German states by GDP figures . In the 1950s and 1960s, Westphalia was known as Land von Kohle und Stahl ( Land of Coal and Steel ). In the post-World War II recovery, the Ruhr was one of the most important industrial regions in Europe, and contributed to

1638-553: 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 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

1729-474: Is now Rhineland-Westphalia and neighbouring Belgium and the Netherlands . In spite of its dismembered condition and the sufferings it underwent at the hands of its French neighbours in various periods of warfare, the Rhenish territory prospered greatly and stood in the foremost rank of German culture and progress. Aachen was the place of coronation of the German emperors, and the ecclesiastical principalities of

1820-410: Is the most populous state in Germany. Apart from the city-states ( Berlin , Hamburg and Bremen ), it is also the most densely populated state in Germany. Covering an area of 34,084 km (13,160 sq mi), it is the fourth-largest German state by size. North Rhine-Westphalia features 30 of the 81 German municipalities with over 100,000 inhabitants, including Cologne (over 1 million),

1911-518: Is the NRW-Nordpunkt near Rahden in the northeast of the state. The Nordpunkt has located the only 100 km to the south of the North Sea coast. The deepest natural dip is arranged in the district Zyfflich in the city of Kranenburg with 9.2 m above sea level in the northwest of the state. Though, the deepest point overground results from mining. The open-pit Hambach reaches at Niederzier

SECTION 20

#1732771969129

2002-677: Is the location of The Bundeswehr (German Armed Forces) has a forces school at the Mayen Barracks, where troops are trained for psychological aspects of leadership of operations, as well as dealing with the media. This school is unique in Germany. Michigan State University , based in Michigan (USA), has a summer program in Mayen. Mayen is twinned with: Eifel The Eifel ( German: [ˈaɪfl̩] ; Luxembourgish : Äifel , pronounced [ˈæːɪfəl] )

2093-669: 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: the Michelsberg, Häuschen and Teufelsley in the north; the Adert, Hohe Acht and Raßberg in the northeast; the Hochkel, Nerotherkopf, Dietzenley and ruins of

2184-594: 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 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

2275-674: 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

2366-488: 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 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,

2457-500: The 80 largest cities in Germany are located within North Rhine-Westphalia. The state's capital is Düsseldorf; the state's largest city is Cologne. In 2022, there were 164,496 births and 234,176 deaths. The following table shows the ten largest cities of North Rhine-Westphalia: The following table shows the population of the state since 1930. The values until 1960 are the average of the yearly population, from 1965

2548-673: The Cugerni were later settled on the west side of the Rhine in the Roman province of Germania Inferior . Julius Caesar conquered the tribes on the left bank, and Augustus established numerous fortified posts on the Rhine, but the Romans never succeeded in gaining a firm footing on the right bank, where the Sugambri neighboured several other tribes including the Tencteri and Usipetes . North of

2639-797: 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 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

2730-647: The Kommunalreform in 1970, four villages next to Mayen were incorporated. The four villages now belong officially to the town and became Boroughs of Mayen. The Boroughs are still village-like and hold most of the Agriculture of Mayen. The Boroughs are The population of Alzheim and Hausen is increasing in the last years, due to the development of new residential areas. Basalt mining , slate mining , cardboard industry , machine - production , aluminium - and artificial material processing . Mayen

2821-637: The Mittelrhein wine region . It changes into the Lower Rhine near Bad Godesberg and leaves North Rhine-Westphalia near Emmerich at a width of 730 metres. Almost immediately after entering the Netherlands, the Rhine splits into many branches. The Pader , which flows entirely within the city of Paderborn , is considered Germany's shortest river. For many, North Rhine-Westphalia is synonymous with industrial areas and urban agglomerations. However,

Mayen - Misplaced Pages Continue

2912-943: The North German Plain . A few isolated hill ranges are located within these lowlands, among them the Hohe Mark, the Beckum Hills , the Baumberge and the Stemmer Berge . The terrain rises towards the south and in the east of the state into parts of Germany's Central Uplands . These hill ranges are the Weser Uplands – including the Egge Hills , the Wiehen Hills , the Wesergebirge and

3003-898: The Randstad , the Flemish Diamond and the Frankfurt Rhine-Main Region . North Rhine-Westphalia was established in 1946 after World War II from the Prussian provinces of Westphalia and the northern part of Rhine Province ( North Rhine ), and the Free State of Lippe by the British military administration in Allied-occupied Germany and became a state of the Federal Republic of Germany in 1949. The city of Bonn served as

3094-422: 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 the streams and rivers cutting into the gently rolling landscape resulting in the present appearance of

3185-414: The Teutoburg Forest in the east, the Sauerland , the Bergisches Land , the Siegerland and the Siebengebirge in the south, as well as the left-Rhenish Eifel in the southwest of the state. The Rothaargebirge in the border region with Hesse rises to height of about 800 m above sea level. The highest of these mountains are the Langenberg , at 843.2 m above sea level, the Kahler Asten (840.7 m) and

3276-450: The Thirty Years' War . The concept of nation-state sovereignty resulting from the treaty became known as " Westphalian sovereignty ". As a result of the Protestant Reformation , there is no dominant religion in Westphalia. Catholicism and Lutheranism are on relatively equal footing. Lutheranism is strong in the eastern and northern parts with numerous free churches. Münster and especially Paderborn are thought of as Catholic. Osnabrück

3367-402: 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

3458-493: The state flag ( Landesdienstflagge ) which is defaced with the state's coat of arms . The state ensign can easily be mistaken for a distressed flag of Hungary , as well as the former national flag of Iran (1964–1980). The same flag was used by the Rhenish Republic (1923–1924) as a symbol of independence and freedom. The horse on the coat of arms is a reference to the Saxon Steed , a heraldic motif associated with both Westphalia and Lower Saxony . The horse first featured in

3549-469: The 15th century coat of arms of the Duchy of Westphalia, before being inherited by the Prussian province of Westphalia and finally the modern state of North Rhine-Westphalia. North Rhine-Westphalia encompasses the plains of the Lower Rhine region and parts of the Central Uplands ( die Mittelgebirge ) up to the gorge of Porta Westfalica . The state covers an area of 34,083 km (13,160 sq mi) and shares borders with Belgium ( Wallonia ) in

3640-402: The Clemensberg (839.2 m). The planimetrically determined centre of North Rhine-Westphalia is located in the south of Dortmund- Aplerbeck in the Aplerbecker Mark (51° 28' N, 7° 33' Ö). Its westernmost point is situated near Selfkant close to the Dutch border, the easternmost near Höxter on the Weser . The southernmost point lies near Hellenthal in the Eifel region. The northernmost point

3731-411: 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

Mayen - Misplaced Pages Continue

3822-417: The Eifel drain into the North Sea via the great rivers outside of the Eifel: the Rhine (and its tributary, 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

3913-432: 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 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

4004-410: 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 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

4095-423: 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

4186-454: The Eifel region, only three comprehensive geological accounts have been produced. In 1822, Johann Steiniger published 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

4277-418: 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 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

4368-525: 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 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

4459-421: The Genovevaburg Museum in Mayen). The name Mayen probably comes from the name Megina. Records from as far back as 847 show this as a designation of the town; it was adapted by the Romans from the Celtic word magos, meaning field. In the 8th century the legend of Genoveva of Brabant , names Mayen as the seat of government of Duke Siegfried of the Pfalz. Mayen received its first official recognition in 1041, and

4550-425: The German Wirtschaftswunder . As of the late 1960s, repeated crises led to contractions of these industrial branches. On the other hand, producing sectors, particularly in mechanical engineering and metal and iron working industry, experienced substantial growth. Despite this structural change and an economic growth which was under national average, the 2018 GDP of 705 billion euro (1/4 of the total German GDP) made NRW

4641-455: 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

SECTION 50

#1732771969129

4732-526: 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, 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

4823-425: The Rhine bulked largely in German history. Prussia first set foot on the Rhine in 1609 by the occupation of the Duchy of Cleves and about a century later Upper Guelders and Moers also became Prussian. At the peace of Basel in 1795, the whole of the left bank of the Rhine was resigned to France, and in 1806, the Rhenish princes all joined the Confederation of the Rhine . After the Congress of Vienna, Prussia

4914-449: The Sigambri and the Rhine region were the Bructeri . As the power of the Roman empire declined, many of these tribes came to be seen collectively as Ripuarian Franks and they pushed forward along both banks of the Rhine, and by the end of the fifth century had conquered all the lands that had formerly been under Roman influence. By the eighth century, the Frankish dominion was firmly established in western Germany and northern Gaul, but at

5005-431: The Stavelot-Venn Saddle ( Hohes Venn ) are the oldest layers of rock, which originate from 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

5096-468: The area of Westphalia. Charlemagne is thought to have spent considerable time in Paderborn and nearby parts. His Saxon Wars also partly took place in what is thought of as Westphalia today. Popular legends link his adversary Widukind to places near Detmold , Bielefeld , Lemgo , Osnabrück, and other places in Westphalia. Widukind was buried in Enger , which is also a subject of a legend. Along with Eastphalia and Engern , Westphalia ( Westfalahi )

5187-419: 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

5278-434: The competency of the state, e.g. cultural matters, the education system, matters of internal security, i.e. the police, building supervision, health supervision and the media; as opposed to matters that are reserved to Federal law. North Rhine-Westphalia uses the same electoral system as the Federal level in Germany: " Personalized proportional representation ". Every five years the citizens of North Rhine-Westphalia vote in

5369-422: The districts and municipalities, while the Landschaftsverband has a directly elected assembly. The five government regions of North Rhine-Westphalia each belong to one of the two Landschaftsverbände : The state's area covers a maximum distance of 291 km from north to south, and 266 km from east to west. The total length of the state's borders is 1,645 km. The following countries and states have

5460-440: 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 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

5551-404: The economically strongest state of Germany by GRP figures , as well as one of the most important economical areas in the world. Of Germany's top 100 corporations, 37 are based in North Rhine-Westphalia. On a per capita base, however, North Rhine-Westphalia remains one of the weaker among the Western German states. North Rhine-Westphalia attracts companies from both Germany and abroad. In 2009,

SECTION 60

#1732771969129

5642-400: The federal capital until the reunification of Germany in 1990 and as the seat of government until 1999. Culturally, North Rhine-Westphalia is not a uniform area; there are significant differences, especially in traditional customs, between the Rhineland region on the one hand and the regions of Westphalia and Lippe on the other. Its economy is the largest among German states by GRDP but

5733-447: 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

5824-501: The interior ministry of North Rhine-Westphalia reported that the number of mosques with a Salafist influence had risen from 3 to 9, which indicated both an actual increase and improved reporting. According to German authorities, Salafism is incompatible with the principles codified in the Constitution of the Federal Republic of Germany , in particular: democracy , the rule of law , and political order based on human rights . The politics of North Rhine-Westphalia takes place within

5915-541: The kingdom of Lotharingia . By the time of Otto I (d. 973), both banks of the Rhine had become part of the Holy Roman Empire , and the Rhenish territory was divided between the duchies of Upper Lorraine on the Moselle and Lower Lorraine on the Meuse. The Ottonian dynasty had both Saxon and Frankish ancestry. As the central power of the Holy Roman Emperor weakened, the Rhineland split into numerous small, independent, separate vicissitudes and special chronicles. The old Lotharingian divisions became obsolete, although

6006-432: The largest part of the state is used for agriculture (almost 52%) and forests (25%). The state consists of five government regions ( Regierungsbezirke ), divided into 31 districts ( Kreise ) and 23 urban districts ( kreisfreie Städte ). In total, North Rhine-Westphalia has 396 municipalities (1997), including the urban districts, which are municipalities by themselves. The government regions have an assembly elected by

6097-459: 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

6188-415: 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 the so-called Eifel North-South Zone. This is a region of subsidence , which runs from the Trier Bay in

6279-658: The ministers involved, is required to sign it and announce it in the Law and Ordinance Gazette. These are the minister-presidents of North Rhine-Westphalia : For the current state government, see Wüst cabinet . The state has Aachen Cathedral , the Cologne Cathedral , the Zeche Zollverein in Essen , the Augustusburg Palace in Brühl and the Imperial Abbey of Corvey in Höxter which are all World Heritage Sites . North Rhine-Westphalia hosts film festivals in Cologne , Bonn, Dortmund , Duisburg , Münster , Oberhausen and Lünen . Other large festivals include Rhenish carnivals , Ruhrtriennale . Every year Gamescom

6370-426: 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". North Rhine-Westphalia North Rhine-Westphalia or North-Rhine/Westphalia , commonly shortened to NRW , is a state ( Land ) in Western Germany . With more than 18 million inhabitants, it

6461-417: The name survives for example in Lorraine in France, and throughout the Middle Ages and even into modern times, the nobility of these areas often sought to preserve the idea of a preeminent duke within Lotharingia, something claimed by the Dukes of Limburg , and the Dukes of Brabant . Such struggles as the War of the Limburg Succession therefore continued to create military and political links between what

6552-634: 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

6643-580: The population at year end is used. Source: Statistische Ämter des Bundes Und der Länder As of 2020 , 50% of the population of the state adhered to the Roman Catholic Church , 25% to the Protestant Church in Germany , and 28% of the population is irreligious or adheres to other denominations or religions. North Rhine-Westphalia ranks first in population among German states for both Roman Catholics and Protestants. In 2016,

6734-528: The republican rule of the French. In 1920, the districts of Eupen and Malmedy were transferred to Belgium (see German-speaking Community of Belgium ). Around AD 1, numerous incursions occurred through Westphalia and perhaps even some permanent Roman or Romanized settlements. The Battle of Teutoburg Forest took place near Osnabrück and some of the Germanic tribes who fought at this battle came from

6825-527: The same time, to the north, Westphalia was being taken over by Saxons pushing south. The Merovingian and Carolingian Franks eventually built an empire which controlled first their Ripuarian kin, and then the Saxons. On the division of the Carolingian Empire at the Treaty of Verdun , the part of the province to the east of the river fell to East Francia , while that to the west remained with

6916-663: 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 the area around Hillesheim and Oberbettingen . In the Upper Cretaceous and during

7007-482: The southwest and the Netherlands ( Limburg , Gelderland and Overijssel ) in the west and northwest. It has borders with the German states of Lower Saxony to the north and northeast, Rhineland-Palatinate to the south and Hesse to the southeast. Approximately half of the state is located in the relative low-lying terrain of the Westphalian Lowland and the Rhineland , both extending broadly into

7098-664: The state capital Düsseldorf (630,000), Dortmund and Essen (about 590,000 inhabitants each) and other cities predominantly located in the Rhine-Ruhr metropolitan area , the largest urban area in Germany and the fourth-largest on the European continent . The location of the Rhine-Ruhr at the heart of the European Blue Banana makes it well connected to other major European cities and metropolitan areas like

7189-658: 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

7280-630: The town was destroyed. After the war and following a special referendum which addressed costs of rebuilding, the people voted to rebuild the town. Up until 1973, Mayen was the District Centre of the Mayen District (with number-plate code MY). After 1973, the district administration was moved to Koblenz and the District was renamed Mayen-Koblenz District with the new number-plate code of MYK; Koblenz kept its own code of KO. Because of

7371-600: The town, flowing from the Eifel towards Weißenthurm on the Rhine . Even in Roman times, Mayen (Lat. Megina ) was an important economic centre. From the end of the 3rd century up until the Middle Ages, potteries operated here, and their products were traded and sold across Central Europe. During prehistoric times, nearby quarries were the sources of basalt to make millstones and tuff used to make sarcophagi. These sarcophagi were found buried with significant glass artifacts as grave goods (both classes of items are displayed in

7462-459: The volume, Geologie der Eifel ("Geology of the Eifel"), whose fourth, revised, edition 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

7553-401: 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

7644-670: 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

7735-488: Was awarded the entire Rhineland , which included the Grand Duchy of Berg , the ecclesiastic electorates of Trier and Cologne , the free cities of Aachen and Cologne, and nearly a hundred small lordships and abbeys. The Prussian Rhine province was formed in 1822 and Prussia had the tact to leave the lower Rhenish districts in undisturbed possession of the liberal institutions to which they had become accustomed under

7826-697: 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

7917-603: 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 a SW-NE direction far beyond the Rhine valley. Since that folding, the Eifel has largely remained part of

8008-595: 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 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

8099-571: Was granted Town Status in 1291 by Rudolf I von Habsburg , at the same time as Bernkastel , Welschbillig , Montabaur and Saarburg . Mayen is possibly linked to the town of Maifeld, which lies a short distant to the south-east, since Mayen was called the capital of the Meiengau in the Middle Ages. During the Second World War, in particular during the allied forces air attacks of 12 December 1944 and 2 January 1945, approximately 90% of

8190-582: Was merged with North Rhine-Westphalia. The constitution of North Rhine-Westphalia was then ratified through a referendum . The first written account of the area was by its conqueror, Julius Caesar , the territories west of the Rhine were occupied by the Eburones and east of the Rhine he reported the Ubii (across from Cologne) and the Sugambri to their north. The Ubii and some other Germanic tribes such as

8281-626: Was originally a district of the Duchy of Saxony . In 1180, Westphalia was elevated to the rank of a duchy by Emperor Barbarossa . The Duchy of Westphalia comprised only a small area south of the Lippe River . Parts of Westphalia came under Brandenburg-Prussian control during the 17th and 18th centuries, but most of it remained divided duchies and other feudal areas of power. The Peace of Westphalia of 1648, signed in Münster and Osnabrück, ended

#128871