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44-715: The community in the Westerwald between Siegen and Limburg an der Lahn . Seck belongs to the Verbandsgemeinde of Rennerod , a kind of collective municipality. Its seat is in the like-named town . Count Gebhard of the Niederlahngau (832–879) was the first known lord of that holding around Seck in the Middle Westerwald, from which he split the western part to endow his monastery at Gemünden . Count Gebhard's grandson, Rudolf I , Bishop of Würzburg (892–908) consecrated

88-600: A church at Seck to Saint Kilian . Seck had its first documentary mention on 27 May 1059 by King Heinrich IV . In the time that followed, Seck acquired a court. Its great parish reached through Rennerod and Lasterbach all the way to Oberrod . Arnold I of Vaucourt , Archbishop of Trier documented in 1181 that the Seligenstatt Monastery in Seck had been donated to the Archmonastery of Trier ( Erzstift Trier ). In 1215 it

132-537: A humid continental climate (Köppen climate classification: Dfb ). In the lowlands of the Unterwesterwald (Lower Westerwald), summers tend to be warm to hot. Erratic convective downpours are not uncommon, yet mostly brief. Winters are mild and see a lot of precipitation, which mostly falls as rain. Snowfall occurs multiple times a year, but usually melts within hours. Thermophilic fruits like figs and peaches are hardy in this area. The mountainous areas of

176-458: A volcanic upland made of Neogene basalt layers. It covers an area of some 50 km × 70 km (31 mi × 43 mi), and therefore roughly 3,000 km (1,200 sq mi), making the Westerwald one of Germany's biggest mountain ranges by area. In areas of subsidence , it has in its flatter western part (Lower Westerwald) the characteristics of rolling hills. Typical for

220-555: A basalt-rich region. Wäller is another vernacular name for them. One of the 12 best-rated hiking trails in Germany is the Westerwaldsteig. The Westerwaldsteig crosses the Westerwald from east ( Herborn ) to west ( Rhine ). Rhenish Massif The Rhenish Massif , Rhine Massif or Rhenish Uplands ( German : Rheinisches Schiefergebirge , pronounced [ˈʁaɪnɪʃəs ˈʃiːfɐɡəˌbɪʁɡə] : 'Rhenish Slate Uplands')

264-522: A range of handcrafted utility ware, with hand-painted swirling floral motifs. In the eastern Westerwald (the part lying in Hesse) are found interesting limestone deposits from the most varied of geological times. Erdbach limestone from the Lower Carboniferous gave one small time period the name "Erdbachian". Near Breitscheid are found the remnants of an atoll from the subtropical Devonian sea that

308-621: A strip of land on the Rhine's right bank and the so-called Rhine-Westerwald; the Westerwald itself lay outside the Roman-occupied area, for the Romans preferred to maintain a little-settled, most likely pathless wilderness as their border. The Westerwald's permanent settlement and thereby its territorial history began with the Chatti (Hessians) pushing their way into the area after the Romans were driven out in

352-621: Is a geologic massif in western Germany , eastern Belgium , Luxembourg and northeastern France . It is drained centrally, south to north by the river Rhine and a few of its tributaries. West of the indent of the Cologne Bight it has the Eifel and the Belgian and French Ardennes ; east is its greatest German component, the Süder Uplands . The Hunsrück hills form its southwest. The Westerwald

396-676: Is also the inspiration for the South Korean military song, "Our Nation Forever". In recent years it has become somewhat controversial in Germany due to its origins during the National Socialist era, with the German military ceasing performances of it in 2017. The standard German term for a Westerwald dweller is Westerwälder ( IPA: [ˈvɛstɐvɛldɐ] ; plural: same), but they are also popularly known as Basaltköpp (“Basalt Heads”), as they are said to be thickheaded, and they live in

440-684: Is an eastern strip. The Lahn - Dill area is a small central zone and the Taunus Mountains form the rest, the south-east. The massif hosts the Middle Rhine Valley ( Rhine Gorge ), a UNESCO World Heritage site linked to the lowest parts of the Moselle ( German : Mosel , Luxembourgish : Musel ). Geologically the Rhenish Massif consists of metamorphic rocks , mostly slates (hence its German name), deformed and metamorphosed during

484-538: Is centred on Höhr-Grenzhausen . Exports, particularly to Italy, are also important (more than one million metric tons each year). In the mid 16th century, potters from Raeren in Belgium migrated into the Westerwald, bringing with them some of their moulds . This type of pottery was taken to the New World and was found in the early Chesapeake settlements. Today one finds not only highly crafted moulded vases and mugs but also

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528-572: Is the Fuchskaute in the High Westerwald, meaning "fox hollow". Many peaks and crests exceed the 600-metre level. Sorted by elevation above sea level, these are some of the Westerwald's highest elevations: The following are the Westerwald's rivers and streams: Weiher is a German word meaning "pond". Through prehistoric finds it can be determined that the Celts settled in the Westerwald and were using

572-455: Is the Fuchskaute in the High Westerwald. Tourist attractions include the Dornburg  [ de ] (394 metres), site of some Celtic ruins from La Tène times (5th to 1st century BC), found in the community of the same name , and Limburg an der Lahn , a town with a medieval centre. The geologically old, heavily eroded range of the Westerwald is in its northern parts overlaid by

616-687: Is the railway station at Montabaur on the Cologne-Frankfurt high-speed rail line . Westerwald The Westerwald ( German pronunciation: [ˈvɛstɐvalt] ; literally 'Western forest') is a low mountain range on the right bank of the river Rhine in the German federal states of Rhineland-Palatinate , Hesse and North Rhine-Westphalia . It is a part of the Rhenish Massif ( Rheinisches Schiefergebirge or Rhenish Slate Mountains). Its highest elevation, at 657 m above sea level,

660-467: The Autobahnen A ;3 ( Cologne – Frankfurt ), A 45 ( Dortmund – Aschaffenburg ) and A 48 . The most notable railway is the Cologne-Frankfurt high-speed rail line with minor stops at Montabaur and Limburg an der Lahn. The High Westerwald is served by Siegerland Airport for private use and special touristic charters, south of Burbach . Geologically , the Westerwald is part of

704-632: The Hercynian orogeny (around 300 million years ago). Most of the massif is part of the Rhenohercynian zone of this orogeny, that also encompasses the Harz further east and Devonian rocks of Cornwall (southwestern England ). Most rocks in the Rhenish Massif were originally sediments, mostly deposited during the Devonian and Carboniferous in a back-arc basin called the Rhenohercynian basin . In some places in

748-585: The Oberwesterwald (Upper Westerwald) and Hoher Westerwald (High Westerwald) feature a much colder climate and are more prone to extreme weather, such as extreme wind gusts during extratropical cyclones . Summer days are pleasantly warm and rarely become hot due to a cool breeze, while winters are cold and rich in snow. The area is home to a number of ski areas . District seats in the Westerwald are: Altenkirchen (Altenkirchen district), Montabaur (Westerwaldkreis) and Neuwied (Neuwied district). Furthermore,

792-805: The Schlösschen (little residential castle) at Seck, still known locally as the Alte Burg (“Old Castle”). Along with the Principality of Nassau-Hadamar, Seck passed to the Grand Duchy of Berg in 1806 and later to the Duchy of Nassau . Administratively, Seck went to the Amt of Rennerod. In 1866, Duke Adolf of Nassau lost his land to Prussia . The administrative offices were dissolved, “ Stein ” self-administration introduced, and Landkreise (rural districts) formed. Seck ended up in

836-538: The Vulkaneifel , the Westerwald and the Vogelsberg . The volcanic rocks have been linked to a mantle plume that, due to its low density and buoyancy, uplifted the entire region during the last few hundred thousand years, as measured from the present elevation of old river terraces. The mountain and hill ranges within the Rhenish Massif - some with maximum height in metres above sea level (NN) ) are given below: West of

880-496: The "Neues Westerwaldlied" ("New Westerwald Song") by songwriter Ulrik Remy, "Ich bin aus 'm Westerwald" ("I am from the Westerwald") and "Das schönste Mädchen vom Westerwald" ("The Loveliest Girl from the Westerwald") by Karl-Eberhard Hain and Jürgen Hardeck, made well known by De Höhner , Die Schröders and other groups. The "Westerwaldlied" is also sung by the Chilean Armed Forces and is known as "Himno de la Sección". It

924-466: The 3rd century. Placename endings such as –ar, –mar and –aha ("Haigraha" = Haiger ) stemming from the Migration Period ( "Völkerwanderung" ) can still be found now. These lie around the forest's outer edges in basins and dales whose soils and climate were favourable to early settlers, and include, for instance, Hadamar , Lahr and Wetzlar . From the 4th to the 6th century, the settlements from

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968-614: The Ardennes, even older rocks of Cambrian to Silurian age crop out as massifs overlain by Devonian slates. These older rocks form smaller massifs of their own ( Stavelot , Rocroi , Givonne and Serpont ). In the eastern Rhenish Massif some very limited outcrops in the Sauerland show rocks of Ordovician and lower Siliurian age. Further Ordovician rock exposures are part of the southern Taunus . The second rock type are Tertiary and Quaternary igneous rocks , which most prominently occur in

1012-572: The Dill, also belong to the Westerwald, whereas the mountains reaching up to 680 m (2,230 ft) near the Haiger Saddle ( Haiger Sattel ) and east of Siegen are counted as part of the Rothaargebirge . The Westerwald is divided by elevation into these three regions: The climate of the region vastly qualifies as oceanic (Köppen climate classification: Cfb ), while higher altitudes experience

1056-612: The Electorate of Trier were all prominent landlords. Political relations were simplified until the 16th century. Among the four greater powers' spheres of influence (Mainz, Cologne, Trier, Hesse), the House of Nassau managed to expand and strengthen its hold on its territory on the Dill between Siegen and Nassau . After the Napoleonic upheavals, Nassau had to share broad swathes of the Westerwald with

1100-864: The Lahn-Dill-Kreis, the Mayen-Koblenz district, the Rhein-Lahn-Kreis and the Limburg-Weilburg district each have shares of the Westerwald. If Sieg is taken as the Westerwald's northernmost limit, then the Rhein-Sieg district likewise belongs here, at least in parts (for example the Siebengebirge and the communities of Eitorf and Windeck ). The Westerwald and its outer edges are crossed by stretches of Bundesstraßen 8 , 42, 49 , 54 , 62 , 255, 256, 277, 413 and 414, over which there are connections to

1144-638: The Oberwesterwaldkreis, whose seat was in Marienberg , and then in 1855 in the newly formed Kreis Westerburg, which itself was merged in 1932 into a new Oberwesterwaldkreis with its seat in Westerburg . In 1974, Seck became part of the Verbandsgemeinde of Rennerod, but as an autonomous Ortsgemeinde . The two Westerwald districts (Oberwesterwaldkreis and Unterwesterwaldkreis) were dissolved and merged into

1188-547: The Rhenish Massif, and likewise represents a heavily eroded remnant of a great Variscan mountain system which in the Mesozoic characterized a great deal of Europe. The Devonian bedrock is covered by volcanic masses from the Tertiary , particularly basalt and tuffs . Economically important, besides slate, limestone and clay quarrying , were, and still are, iron and its processing industry between Rheintal (Unkel, Linz) and

1232-579: The Trier and Cologne mission, this area underwent Christianization. Trier advanced up the Lahn, Cologne to the Rhine and Sieg. Trier-Lorrainian and Lower Rhine influences were nevertheless brought into the Westerwald. Among the witnesses to the art of building at that time is the monastery church at Limburg- Dietkirchen , in its oldest parts. After many changes in ownership between the Ottonian and Salian noble families, it

1276-627: The Upper Westerwald, bypassing the High Westerwald, seeing it as nothing more than a trackless wooded wilderness, after which they eventually came up against the Rhine in the 2nd century. Even in the time when the Celts found themselves having to avoid the Germanic invaders by moving to the west, the Romans were also pushing in from the Rhine's left bank to the southwest. However, the Romans only managed to seize

1320-673: The Westerwald is bordered by the following river valleys: the Rhine between Koblenz and Linz , the Sieg as far as Betzdorf, the Heller , the Dill and from its mouth near Wetzlar , the Lahn up to Lahnstein . Geomorphologically , the Westerwald belongs to the Rhenish Massif, which forms the greater part of that range's eastern half on the Rhine's right bank. Likewise, the Gladenbach Uplands , lying east of

1364-481: The Westerwald's north and southwest edges even gave two Lower Devonian layers, with their colourful slates, their names. The upper mountain layers are formed of volcanic strata made of basalt containing tuffs. In a few areas, slate and clay have long been quarried, the latter notably in the so-called Kannenbäckerland , but also in a few other places where the clay is worked into the salt- glazed grey Westerwald Pottery with cobalt blue decoration. The pottery industry

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1408-640: The Westerwaldkreis with its seat in Montabaur . The council is made up of 16 council members who were elected in a municipal election on 13 June 2004. They all belong to a Wählergemeinschaft (“voters’ community”) Right near the community runs Bundesstraße 54, leading from Limburg an der Lahn to Siegen . The nearest Autobahn interchange is Limburg-Nord on the A ;3 ( Cologne – Frankfurt ), some 20 km away. The nearest InterCityExpress stop

1452-903: The districts of Altenkirchen , Lahn-Dill , Limburg-Weilburg , Neuwied , Rhein-Lahn , Rhein-Sieg , Westerwaldkreis and partly in Siegen-Wittgenstein . It is found south of the Rothaargebirge , southwest of the Lahn-Dill-Bergland (another low mountain range), north of the Taunus and east of the Middle Rhine and stretches more or less southwards from Siegen and Burbach , southwestwards from Haiger , northwestwards from Weilburg , northwards from Limburg an der Lahn , northeastwards from Koblenz , eastwards from Linz am Rhein , southeastwards from Wissen and southwards from Betzdorf . In its centre lie Bad Marienberg and Hachenburg . Clockwise,

1496-576: The economy of the Upper Westerwald, some 40% of which is actually wooded, are traditional slate mining, clay quarrying , diabase and basalt mining, pottery and the iron ore industry, and among other things mining in the Siegerländer Erzrevier (roughly "Siegerland Ore Grounds"). Despite its relatively slight elevation, the Westerwald has for a low mountain range a typical agreeable climate. Economically and culturally, it belongs among Germany's best known mountain ranges. The name "Westerwald"

1540-532: The heart of the Herrschaft zum (also vom or auf dem ) Westerwald ("Lordship over the Westerwald"). This comprised the three court districts of Marienberg , Emmerichenhain and Neukirch . The Lordship later fell under the governance of the Lordship or County of Beilstein. The Westerwald lies mostly southwest of the three-state common point shared by Rhineland-Palatinate, Hesse and North Rhine-Westphalia in

1584-624: The iron ore deposits in the so-called Hallstatt times ( Iron Age , roughly 750 to 500 BC). In all likelihood they came into the area from the Hunsrück . From La Tène times come the Celtic ringwall-girded defensive and sheltering castles which may be found on, among other peaks, the Malberg. Already by La Tène times, Germanic peoples were thrusting in from the east and from the Sieg valley. They came about 380 BC into

1628-427: The lower Wied, pumice gravel in the Neuwied Basin, various mineral springs and, once, brown coal mining. The whole Westerwald region lay under a tropically warm arm of the sea in the Palaeozoic (600 to 270 million years ago). This sea deposited layers of sediments many kilometres thick into the Variscan geosyncline , which were heavily folded in the orogeny that followed. The towns of Siegen and Koblenz on

1672-501: The newly minted power Prussia . A sovereign Duchy of Nassau existed until it was annexed by Prussia in 1866. Nowadays, the Westerwald is shared among three German federal states: Hesse, North Rhine-Westphalia and Rhineland-Palatinate. The Westerwald is also internationally known in songs, above all in folksongs , and particularly the "Westerwaldlied" ("Westerwald Song"), as well as "Westerwald-Marsch" ("Westerwald March"), "Westerwald, du bist so schön" ("Westerwald, you are so lovely"),

1716-564: The time of the taking of the land arose in formerly pathless areas, taking endings such as –ingen and –heim , like Bellingen and Bladernheim ; these lie on the broad, raised plains in the Upper Westerwald. The Franks built their old settlements on the edge of the Westerwald in the central areas of their districts, to build up slowly and permanently strongholds in the interior. There arose places with names ending in –rode, –scheid, –hahn, –berg, –tal and –seifen . Once clearing settlements had been established and logging for iron ore smelting

1760-418: Was first mentioned in 1048 in a document from the Electorate of Trier and described at that time the woodlands ( Wald is German for "forest" or "woods") around the three churches in Bad Marienberg , Rennerod and Emmerichenhain, west of the royal court at Herborn . Only since the mid 19th century has the name come into common usage for the whole range. The High Westerwald has since the Middle Ages formed

1804-408: Was here 380,000,000 years ago. Parts of this limestone formation are worked in open-pit mining ; near Enspel , a " fossil conservation area" has been instituted, in which institutes from several colleges conduct research and excursions. A few karst caves are of interest to spelaeology and bring about the temporary disappearance and reappearance of the Erdbach. The Westerwald's highest mountain

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1848-400: Was in the end the Counts of Sayn, Diez and Wied who managed to take hold of extensive landholdings. Particular importance was achieved by the Counts of Laurenburg, who later called themselves the Counts of Nassau . In the east, the Landgraves of Hesse put it about that they could beat the Archbishopric of Mainz on the battlefield. Moreover, the Counts of Wied, the Counts of Sayn-Wittgenstein and

1892-430: Was the Maria Laach Abbey's daughter monastery. In the mid 15th century, an end was put to monastery life. In 1468, excise from the Seck yearly market was raised. The Lords of Westerburg and Runkel held sway over the parish of Seck. Often, it was the object of disputes between these two houses and their sidelines. Prince Moritz Heinrich of Nassau-Hadamar had the Secker Weiher (pond) built in 1672, and shortly thereafter also

1936-403: Was under way, the widespread destruction of the forest began. Between the 6th and 9th centuries came settlement expansion from the old settlements towards the edges, a process still witnessed in placename endings such as –hausen, –hofen, –kirch, –burg or –tal . The last settlement period in the Westerwald began in the 10th century and ended about 1300. Through Carolingian policy and therefore

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