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100-784: The municipality lies in the Eifel and belongs to the Verbandsgemeinde Wittlich-Land . The “Laufeld Culture” ( Hallstatt times , about 700 BC) took its name from a great burying ground that had been found near Laufeld. In 1344, King John of Luxembourg acquired from the Abbey of Echternach the Hof Laufeld (“Laufeld Estate”). Shortly thereafter, this ended up in the ownership of the Counts of Manderscheid . Beginning in 1794, Laufeld lay under French rule. In 1814 it

200-515: 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

300-496: A churchtower argent with conical roof, door and two windows in pale sable and argent a cross flory gules, in a base Or a fess dancetty of the fourth. The three charges all come from Laufeld's history. The churchtower on the dexter (armsbearer's right, viewer's left) side was part of the only parish church in the County of Manderscheid , and was important as a defensive structure as well. Given its importance, it has found its way into

400-544: 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

500-824: 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

600-614: 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

700-618: 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

800-605: A result of the Variscan orogeny . After this event, and over the course of the following 200 million years, this area has been continuously flattened. During the Cretaceous period, the ocean penetrated the continent from the direction of the North Sea up to the mountainous area near Aachen, bringing with it clay, sand, and chalk deposits. While the clay (which was the basis for a major pottery industry in nearby Raeren )

900-419: 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

1000-694: Is divided into seven administrative districts, or boroughs, each with its own district council, district leader, and district authority. The councils are elected locally by those who live within the district, and these districts are further subdivided into smaller sections for statistical purposes, with each sub-district named by a two-digit number. The districts of Aachen, including their constituent statistical districts, are: Regardless of official statistical designations, there are 50 neighbourhoods and communities within Aachen, here arranged by district: The following cities and communities border Aachen, clockwise from

1100-505: 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

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1200-565: Is mostly found in the lower areas of Aachen, the hills of the Aachen Forest and the Lousberg were formed from upper Cretaceous sand and chalk deposits. More recent sedimentation is mainly located in the north and east of Aachen and was formed through tertiary and quaternary river and wind activities. Along the major thrust fault of the Variscan orogeny , there are over 30 thermal springs in Aachen and Burtscheid . Additionally,

1300-553: 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

1400-944: Is the 13th-largest city in North Rhine-Westphalia and the 27th-largest city of Germany, with around 261,000 inhabitants. Aachen is located at the northern foothills of the High Fens and the Eifel Mountains. It sits on the Wurm River , a tributary of the Rur , and together with Mönchengladbach , it is the only larger German city in the drainage basin of the Meuse . It is the westernmost larger city in Germany, lying approximately 61 km (38 mi) west of Cologne and Bonn , directly bordering Belgium in

1500-669: 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

1600-594: 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

1700-674: 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

1800-488: 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,

1900-458: The Eifel and the High Fens and its subsequent prevailing westerly weather patterns, rainfall in Aachen (on average 805 mm/year) is comparatively higher than, for example, in Bonn (with 669 mm/year). Another factor in the local weather forces of Aachen is the occurrence of Foehn winds on the southerly air currents, which results from the city's geographic location on the northern edge of

2000-689: The French Revolution . With approval from the Regierungsbezirk government in Trier on 2 May 1983, Laufeld was granted the right to bear its own arms. Worth seeing in Laufeld is the Doll and Toy Museum ( Puppen- und Spielzeugmuseum ). On display are dolls and playthings from the last 100 years as well as everyday objects from the 1950s. The Laufeld educational nature path teaches about

2100-797: 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

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2200-533: The Meuse , and about 30 km (19 mi) north of the High Fens , which form the northern edge of the Eifel uplands of the Rhenish Massif . The maximum dimensions of the city's territory are 21.6 km ( 13 + 3 ⁄ 8  mi) from north to south, and 17.2 km ( 10 + 3 ⁄ 4  mi) from east to west. The city limits are 87.7 km ( 54 + 1 ⁄ 2  mi) long, of which 23.8 km ( 14 + 3 ⁄ 4  mi) border Belgium and 21.8 km ( 13 + 1 ⁄ 2  mi)

2300-735: The Neolithic era, about 5,000 years ago, attracted to its warm mineral springs . Latin Aquae figures in Aachen's Roman name Aquae granni , which meant "waters of Grannus ", referring to the Celtic god of healing who was worshipped at the springs. This word became Åxhe in Walloon and Aix in French, and subsequently Aix-la-Chapelle to distinguish it from Aix-en-Provence , after Charlemagne had his palatine chapel built there in

2400-511: The Palace . Charlemagne spent most winters in Aachen between 792 and his death in 814. Aachen became the focus of his court and the political centre of his empire. During the Carolingian empire, a Jewish community lived near the royal palace. In Jewish texts, the city of Aachen was called Aish or Ash (אש). In 797, Isaac, a Jewish merchant, accompanied two ambassadors of Charlemagne to

2500-667: The RWTH Aachen (Rheinisch-Westfälische Technische Hochschule), known especially for mechanical engineering, automotive and manufacturing technology as well as for its research and academic hospital Klinikum Aachen , one of the largest medical facilities in Europe. Aachen is located in the middle of the Meuse–Rhine Euroregion , close to the border tripoint of Germany, the Netherlands, and Belgium . The town of Vaals in

2600-597: 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

2700-628: The Treaty of Verdun , the city was within the borders of Middle Francia , until it became part of East Francia after the Treaty of Meerssen (870). It subsequently was part of the Holy Roman Empire and was granted city rights in 1166 by Emperor Frederick Barbarossa , becoming an imperial city . It served as the coronation site where 31 Holy Roman Emperors were crowned Kings of the Germans from 936 to 1531, until Frankfurt am Main became

2800-691: The War of Devolution . The second congress ended with the second treaty in 1748, ending the War of the Austrian Succession . In 1789, there was a constitutional crisis in the Aachen government, and in 1794 Aachen lost its status as a free imperial city . In 1629, the Aachen Jewish community was expelled from the city. In 1667, six Jews were allowed to return. Most of the Aachen Jewish community settled in Burtscheid. As recently as

2900-455: 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

3000-586: The migration period . The last Roman coin finds are from the time of Emperor Gratian (AD 375–383). Rome withdrew its troops from the area, but the town remained populated. By 470, the town came to be ruled by the Ripuarian Franks and subordinated to their capital, Cologne . During the Roman period, Aachen was the site of a flourishing Jewish community. Pepin the Short had a castle residence built in

3100-567: The vicus Aquae Granni was Frankized around the 5th century. This was followed by a period of sedentism under first Merovingian and then Carolingian rule. With the completion of the Carolingian Palace of Aachen at the transition to the 9th century, Aachen was constituted as the main royal residence of the Frankish Empire ruled by Charlemagne . Because of that the city is sometimes called "cradle of Europe". After

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3200-788: The " chef-lieu du département de la Roer " in Napoleon's First French Empire . In 1815, after the Napoleonic Wars , the Kingdom of Prussia took over within the new German Confederation . The city was one of its most socially and politically backward centres until the end of the 19th century. Administered within the Rhine Province , by 1880 the population was 80,000. Starting in 1838, the railway from Cologne to Belgium passed through Aachen. The city suffered extreme overcrowding and deplorable sanitary conditions until 1875, when

3300-527: The Canadian city of Regina, Saskatchewan which is located at a similar latitude but at the heart of the North American landmass, far away from the sea's moderating effects, is classified as being in zone 3a. In the 1991–2020 period, the last freeze (at 2 m above ground) of spring occcured on April 28th and the first fall freeze on October 13th, on average. The Aachen weather station has recorded

3400-600: The Celtic god, and it seems it was the Roman 6th Legion at the start of the 1st century AD that first channelled the hot springs into a spa at Büchel, adding at the end of the same century the Münstertherme spa, two water pipelines, and a probable sanctuary dedicated to Grannus. A kind of forum, surrounded by colonnades, connected the two spa complexes. There was an extensive residential area. The Romans built bathhouses near Burtscheid . A temple precinct called Vernenum

3500-514: 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

3600-520: 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

3700-432: 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

3800-410: 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

3900-423: 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

4000-454: 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

4100-418: 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

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4200-402: The Eifel. Because the city is surrounded by hills, it suffers from inversion-related smog. Some areas of the city have become urban heat islands as a result of poor heat exchange, both because of the area's natural geography and from human activity. The city's numerous cold air corridors, which are slated to remain as free as possible from new construction, therefore play an important role in

4300-525: 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

4400-455: 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

4500-406: The Netherlands lies nearby at about 6 km (4 mi) from Aachen's city centre, while the Dutch city of Heerlen and Eupen , the capital of the German-speaking Community of Belgium , are both located about 20 km (12 mi) from Aachen city centre. Aachen lies near the head of the open valley of the Wurm (which today flows through the city in canalised form), part of the larger basin of

4600-497: The Netherlands. The highest point in Aachen, located in the far southeast of the city, lies at an elevation of 410 m (1,350 ft) above sea level. The lowest point, in the north, and on the border with the Netherlands, is at 125 m (410 ft). As the westernmost city in Germany (and close to the Low Countries), Aachen and the surrounding area belongs to a temperate climate zone ( Cfb ), with humid weather, mild winters, and warm summers. Because of its location north of

4700-526: 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

4800-532: The Roman Curia as such. In 936, Otto I was crowned king of East Francia in the collegiate church built by Charlemagne. During the reign of Otto II , the nobles revolted and the West Franks under Lothair raided Aachen in 978. Aachen was attacked again by Odo of Champagne , who attacked the imperial palace while Conrad II was absent. Odo relinquished it and was killed afterwards. The palace and town of Aachen had fortifying walls built by order of Emperor Frederick Barbarossa between 1172 and 1176. Over

4900-431: 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

5000-419: 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

5100-414: The city is best known is Aachener Printen , a type of gingerbread . The name Aachen is a modern descendant, like southern German Ach(e) , German: Aach , meaning "river" or "stream", from Old High German ahha , meaning "water" or "stream", which directly translates (and etymologically corresponds) to Latin Aquae , referring to the springs. The location has been inhabited by humans since

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5200-449: The city. On Kristallnacht in 1938, the synagogue was destroyed. By the onset of World War II in 1939, many Jews had emigrated or were arrested, and only 782 remained in the city. At the end of the war in 1945, only 62 Jews lived in the city. As of 2003, 1,434 Jews were again living in Aachen. The city of Aachen has developed into a technology hub as a by-product of hosting one of the leading universities of technology in Germany with

5300-415: The city. The first killed 1,525, including 212 children, and bombed six hospitals. During the second, 442 aircraft hit two railway stations, killed 207, and left 15,000 homeless. The raids destroyed Aachen-Eilendorf and Aachen-Burtscheid . The city and its fortified surroundings were besieged from 12 September to 21 October 1944 by the US 1st Infantry Division with the 3rd Armored Division assisting from

5400-418: The court library were also produced locally. During the reign of Louis the Pious (814–840), substantial quantities of ancient texts were produced at Aachen, including legal manuscripts such as the leges scriptorium group, patristic texts including the five manuscripts of the Bamberg Pliny Group . Finally, under Lothair I (840–855), texts of outstanding quality were still being produced. This however marked

5500-434: The court of Harun al-Rashid . He returned to Aachen in July 802, bearing an elephant called Abul-Abbas as a gift for the emperor. After Charlemagne's death, he was buried in the church which he had built; his original tomb has been lost, while his alleged remains are preserved in the Karlsschrein , the shrine where he was reburied after being declared a saint; his saintliness, however, was never officially acknowledged by

5600-440: 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

5700-432: The end of 2009, the foreign-born residents of Aachen made up 13.6 percent of the total population. A significant portion of foreign residents are students at the RWTH Aachen University . Aachen is at the western end of the Benrath line that divides High German to the south from the rest of the West Germanic speech area to the north. Aachen's local dialect is called Öcher Platt and belongs to Ripuarian . The city

5800-402: The end of the period of manuscript production at Aachen. In 1598, following the invasion of Spanish troops from the Netherlands , Rudolf deposed all Protestant office holders in Aachen and went as far as expelling them from the city. From the early 16th century, Aachen started to lose its power and influence. First the coronations of emperors were moved from Aachen to Frankfurt . This

5900-466: The following extreme values: The geology of Aachen is very structurally heterogeneous. The oldest occurring rocks in the area surrounding the city originate from the Devonian period and include carboniferous sandstone , greywacke , claystone and limestone . These formations are part of the Rhenish Massif , north of the High Fens. In the Pennsylvanian subperiod of the Carboniferous geological period, these rock layers were narrowed and folded as

6000-400: The forest ecosystem. Laufeld is a state-recognized recreational municipality ( Erholungsort ). There are two commercial areas with 20 firms and more than 500 jobs. To the east runs the Autobahn A 1 . In Laufeld there is one primary school . Eifel The Eifel ( German: [ˈaɪfl̩] ; Luxembourgish : Äifel , pronounced [ˈæːɪfəl] ) is

6100-447: 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

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6200-448: The late 18th century the Abbess of Burtscheid was still prevented from building a road linking her territory to the neighbouring estates of the duke of Jülich ; the city of Aachen deployed its handful of soldiers to chase away road-diggers. On 9 February 1801, the Peace of Lunéville removed the ownership of Aachen and the entire "left bank" of the Rhine from Germany (the Holy Roman Empire ) and granted it to France. In 1815, control of

6300-402: The late 8th century and then made the city his empire's capital. The city is known by a variety of different names in other languages: Flint quarries on the Lousberg , Schneeberg, and Königshügel, first used during Neolithic times (3000–2500 BC), attest to the long occupation of the site of Aachen, as do recent finds under the modern city's Elisengarten pointing to a former settlement from

6400-459: 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

6500-415: 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

6600-475: The medieval fortifications were abandoned as a limit to building and new, better housing was built in the east of the city, where sanitary drainage was easiest. In December 1880, the Aachen tramway network was opened, and in 1895 it was electrified. In the 19th century and up to the 1930s, the city was important in the production of railway locomotives and carriages, iron, pins, needles , buttons, tobacco, woollen goods, and silk goods. After World War I , Aachen

6700-427: The middle of the 17th century, the city had developed a considerable reputation as a spa, although this was in part because Aachen was then – and remained well into the 19th and early 20th century – a place of high-level prostitution. Traces of this hidden agenda of the city's history are found in the 18th-century guidebooks to Aachen as well as to the other spas. The main indication for visiting patients, ironically,

6800-418: The municipality's arms. The cross with lilylike ends to its arms (“cross flory”) on the sinister (armsbearer's left, viewer's right) side was an heraldic charge borne by the Abbey of Echternach , once the village's landlord in the Middle Ages . The zigzag stripe (“fess dancetty”) in the escutcheon ’s base was the heraldic device borne by the Counts of Manderscheid, who held sway here from the 14th century until

6900-516: 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". Aachen Aachen ( / ˈ ɑː k ən / AH -kən , German: [ˈaːxn̩] ; Aachen dialect : Oche [ˈɔːxə] ; Dutch : Aken [ˈaːkə(n)] ; French: Aix-la-Chapelle ; Latin: Aquae Granni or Aquisgranum )

7000-470: The next 500 years, most kings of Germany who ruled the Holy Roman Empire were crowned in Aachen. The original audience hall built by Charlemagne was torn down and replaced by the current city hall in 1330. During the 13th century, many Jews converted to Christianity, as shown in the records of the Aachen Minster (today's Cathedral). In 1486, the Jews of Aachen offered gifts to Maximilian I during his coronation ceremony. The last king to be crowned here

7100-399: 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

7200-648: The northwest: Herzogenrath , Würselen , Eschweiler , Stolberg and Roetgen (which are all in the district of Aachen ); Raeren , Kelmis and Plombières ( Liège Province in Belgium) as well as Vaals , Gulpen-Wittem , Simpelveld , Heerlen and Kerkrade (all in Limburg Province in the Netherlands). The current mayor of Aachen is Sibylle Keupen , an independent endorsed by Alliance 90/The Greens , since 2020. The most recent mayoral election

7300-477: The preferred place of coronation. One of Germany's leading institutes of higher education in technology, the RWTH Aachen University ( Rheinisch-Westfälisch Technische Hochschule Aachen ), is located in the city. Its university hospital Uniklinikum Aachen is Europe's largest single-building hospital. Aachen's industries include science, engineering and information technology. In 2009, Aachen

7400-518: The royal household for several months. In the year of his coronation as king of the Franks , 768, Charlemagne came to spend Christmas at Aachen for the first time. He remained there in a mansion which he may have extended, although there is no source attesting to any significant building activity at Aachen in his time, apart from the building of the Palatine Chapel (since 1930, cathedral) and

7500-607: The same period. Bronze Age (around 1600 BC) settlement is evidenced by the remains of barrows (burial mounds) found, for example, on the Klausberg. During the Iron Age , the area was settled by Celtic peoples who were perhaps drawn by the marshy Aachen basin's hot sulphur springs where they worshipped Grannus , god of light and healing. The 25-hectare Roman spa resort town of Aquae Granni was, according to legend, founded by Grenus, under Hadrian , around 124 AD. Grenus refers to

7600-663: 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

7700-520: The south. Around 13 October the US 2nd Armored Division, coming from the north, and got as close as Würselen , while the 30th Infantry Division completed the encirclement of Aachen on 16 October 1944. With reinforcements from the US 28th Infantry Division the battle continued involving direct assaults through the heavily defended city, which forced the German garrison to surrender on 21 October 1944. Aachen

7800-462: The southwest, and the Netherlands in the northwest. The city lies in the Meuse–Rhine Euroregion and is the seat of the district of Aachen ( Städteregion Aachen ). The once Celtic settlement was equipped with several thermae in the course of colonization by Roman pioneers settling at the warm Aachen thermal springs around the 1st century. After the withdrawal of the Roman troops,

7900-492: The subsurface of Aachen is traversed by numerous active faults that belong to the Rurgraben fault system, which has been responsible for numerous earthquakes in the past, including the 1756 Düren earthquake and the 1992 Roermond earthquake , which was the strongest earthquake ever recorded in the Netherlands . Aachen has 245,885 inhabitants (as of 31 December 2015), of whom 118,272 are female, and 127,613 are male. At

8000-606: 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

8100-494: The town was passed to the Kingdom of Prussia through an agreement reached by the Congress of Vienna . The third congress took place in 1818, to decide the fate of occupied Napoleonic France. By the middle of the 19th century, industrialisation had swept away most of the city's medieval rules of production and commerce, although the remains of the city's medieval constitution were kept in place until 1801, when Aachen became

8200-620: The town, due to the proximity of the hot springs and also for strategic reasons as it is located between the Rhineland and northern France. Einhard mentions that in 765–766 Pepin spent both Christmas and Easter at Aquis villa ( Et celebravit natalem Domini in Aquis villa et pascha similiter ) ("and [he] celebrated the birth of the Lord [Christmas] in the town Aquis, and similarly Easter"), which must have been sufficiently equipped to support

8300-485: The urban climate of Aachen. The January average is 3.0 °C (37 °F), while the July average is 18.5 °C (65 °F). Precipitation is almost evenly spread throughout the year. The city's oceanic climate provides comparably mild winters: While Aachen falls within the coldest extents covered by USDA plant hardiness zone 8b in the 1991–2020 period, having an average yearly minimum of -9.22 °C (15.4 °F),

8400-459: 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

8500-401: 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

8600-670: 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

8700-476: Was Ferdinand I in 1531. During the Middle Ages , Aachen remained a city of regional importance, due to its proximity to Flanders ; it achieved a modest position in the trade in woollen cloths, favoured by imperial privilege. The city remained a free imperial city , subject to the emperor only, but was politically far too weak to influence the policies of any of its neighbours. The only dominion it had

8800-573: Was syphilis ; only by the end of the 19th century had rheumatism become the most important object of cures at Aachen and Burtscheid. Aachen was chosen as the site of several important congresses and peace treaties: the first congress of Aachen (often referred to as the Congress of Aix-la-Chapelle in English) on 2 May 1668, leading to the First Treaty of Aachen in the same year which ended

8900-584: Was also the site of many important church councils, including the Council of 837 and the Council of 1166 , a council convened by the antipope Paschal III . Aachen was an important site for the production of historical manuscripts. Under Charlemagne's purview, both the Ada Gospels and the Coronation Gospels may have been produced in Aachen. In addition, quantities of the other texts in

9000-824: Was assigned to the Kingdom of Prussia at the Congress of Vienna . Since 1947, it has been part of the then newly founded state of Rhineland-Palatinate . The council is made up of 12 council members, who were elected by majority vote at the municipal election held on 7 June 2009, and the honorary mayor as chairman. The German blazon reads: Über goldenem Schildfuß mit rotem Sparrenbalken gespalten, vorn in Blau ein silberner Kirchturm mit schwarzem Dach, hinten in Silber ein rotes Lilienkreuz. The municipality's arms might in English heraldic language be described thus: Per pale azure

9100-463: Was built near the modern Kornelimünster/Walheim . Today, remains have been found of three bathhouses, including two fountains in the Elisenbrunnen and the Burtscheid bathhouse. Roman civil administration in Aachen eventually broke down as the baths and other public buildings (along with most of the villae rusticae of the surrounding countryside) were destroyed around AD 375 at the start of

9200-633: 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

9300-548: 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

9400-530: Was followed by the religious wars and the great fire of 1656. After the destruction of most of the city in 1656, the rebuilding was mostly in the Baroque style. The decline of Aachen culminated in 1794, when the French, led by General Charles Dumouriez , occupied Aachen. In 1542, the Dutch humanist and physician Francis Fabricius published his study of the health benefits of the hot springs in Aachen. By

9500-595: 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

9600-638: Was largely unscathed. 4,000 inhabitants remained in the city; the rest had followed evacuation orders. Its first Allied-appointed mayor, Franz Oppenhoff , was assassinated by an SS commando unit. On 16 May 1815, the Jewish community of the city offered an homage in its synagogue to the Prussian king, Friedrich Wilhelm III . In 1862, a large synagogue was built, later called the Old Synagogue  [ de ; fr ; id ] . By 1933, 1,345 Jews lived in

9700-750: Was occupied by the Allies until 1930, along with the rest of German territory west of the Rhine. Aachen was one of the locations involved in the Rhenish Republic . On 21 October 1923, an armed mob took over the city hall. Similar actions took place in Mönchengladbach , Duisburg , and Krefeld . This republic lasted about a year. Aachen was heavily damaged during World War II . According to Jörg Friedrich in The Fire (2008), two Allied air raids on 11 April and 24 May 1944 "radically destroyed"

9800-539: Was over Burtscheid , a neighbouring territory ruled by a Benedictine abbess , which was forced to accept that all of its traffic must pass through the "Aachener Reich". As an imperial city, Aachen held certain political privileges that allowed it to remain independent of the troubles of Europe for many years. It remained a direct vassal of the Holy Roman Empire throughout most of the Middle Ages. It

9900-400: Was ranked eighth among cities in Germany for innovation. The regional dialect spoken in the city is a Central Franconian , Ripuarian variant with strong Limburgish influences from the dialects in the neighbouring Netherlands. As a Rhenish city, Aachen is one of the main centres of carnival celebrations in Germany , along with Cologne and Mainz . The culinary specialty for which

10000-580: Was the first German city to be captured by the Western Allies, and its residents welcomed the soldiers as liberators. What remained of the city was destroyed—in some areas completely—during the fighting, mostly by American artillery fire and demolitions carried out by the Waffen-SS defenders. Damaged buildings included medieval churches of and the Rathaus (city hall), although Aachen Cathedral

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