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Wilgartswiesen
Wilgartswiesen is a municipality in Südwestpfalz district, in Rhineland-Palatinate, western Germany. Geography The municipality lies in the southern part of the Palatine Forest, the German part of the Wasgau, in the middle of the Palatine Forest-North Vosges Biosphere Reserve. On the territory of Wilgartswieser the Wellbach stream empties into the Queich, which itself is one of the main drainage systems of the Palatinate region. North of the village run several bunter sandstone The Buntsandstein (German for ''coloured'' or ''colourful sandstone'') or Bunter sandstone is a lithostratigraphic and allostratigraphic unit (a sequence of rock strata) in the subsurface of large parts of west and central Europe. The Buntsands ... rock groups, out of which the castles of Wilgartaburg and Falkenburg have been hewn. The municipal terrain, most of which is part of the Frankenweide, is almost entirely wooded. References Municipalities in Rhineland-Palatinate Palatinate Fo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Falkenburg Castle (Palatinate)
Falkenburg Castle is a castle ruin overlooking the village of Wilgartswiesen in the Palatinate Forest in Rhineland-Palatinate, Germany. Like almost all castles in this region it was built on sandstone. History The Falkenburg was probably built in the 11th century as a successor to the nearby Wilgartaburg and to protect the adjacent villages. In the documents of Archbishop Erkinbald of Mainz, letters dating to 1019 describe a rock outcrop called the Falkenstein considered as the most northerly border belonging to the principality of Kaiserslautern. Werner I of Bolanden is thought to have begun construction of the castle on this rock in 1125; he was a vassal of Duke Frederick II of Swabia. At the Bolanden family monastery in Hane were records of Sigbold of Falkenstein in 1135; he was one of the first to take the name of the castle for himself. Then in 1233 the imperial '' ministerialis'', Phillip IV of Bolanden, was the first to clearly say that he was from Falkenstein in a lega ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Frankenweide
The Frankenweide is a hill region in the German state of Rhineland-Palatinate. It forms the central part of the Palatine Forest in the Palatinate region. Geography The Frankenweide is a single forest that, today, covers an area of a good 200 km². Much of it is a plateau at an elevation of about 380–, which climbs steadily from north to south. Individual hill summits rise prominently from the plateau, which is framed by deeply incised valleys. In the south the Frankenweide is bounded by the valley of the Queich, in the east by the Wellbach stream and its northern projection. There it is adjoined by the imperial forest (''Reichswald'') of Kaiserslautern. In the northwest the Moosalb stream forms the border, and in the southwest, it is bounded by Gräfenstein Land. From north to south the region is divided into Lower Frankenweide (''Untere Frankenweide'') with its municipality of Waldleiningen, Middle Frankenweide (''Mittlere Frankenweide'') and Eschkopf, and Upper Fra ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wilgartaburg
The Wilgartaburg, also called the ''Wiligartaburg, Wilgartsburg'' or ''Wiligartisburg'', is the heritage site of a ruined rock castle located at a height of near the German village of Wilgartswiesen in the state of Rhineland-Palatinate. Location The remains of the former hill castle are located near Wilgartswiesen before the Rinnthal at around 245 metres above sea level on a spur of the Göckelberg hill above the River Queich. This left tributary of the Rhine rises in the Wasgau region which comprises the southern part of the Palatinate Forest in Germany and the northern part of the Vosges in France. History The Wilgartaburg is one of the oldest castles in the Palatinate region, probably dating to the 8th or 9th century. According to an unverified source it was built in the late 10th or early 11th century by an abbot of Hornbach Abbey, initially as a wooden castle. In the Salian era (11th century) it was rebuilt in stone. This was expanded in the 12th century and a fi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wasgau
The Wasgau (german: Wasgau, french: Vasgovie) is a Franco-German hill range in the German state of Rhineland-Palatinate and the French departments of Bas-Rhin and Moselle. It is formed from the southern part of the Palatine Forest and the northern part of the Vosges mountains, and extends from the River Queich in the north over the French border to the Col de Saverne in the south. The highest hill in the entire Wasgau is the Grand Wintersberg (581 m above NHN) near Niederbronn-les-Bains in northern Alsace. Next, at 577 m is the only slightly lower Rehberg near Annweiler in the South Palatinate, which is the highest summit on German soil in the Wasgau. The Wasgau forms the southern part of the Palatine Forest-North Vosges Biosphere Reserve. Geography Location The Wasgau runs from a line between Pirmasens and Landau in the north that, from Wilgartswiesen coincides with the course of the River Queich, to the Col de Saverne and a line between Phalsbourg to Sa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Südwestpfalz
Südwestpfalz is a district (''Kreis'' or more precise ''Landkreis'') in the south of Rhineland-Palatinate, Germany. Neighboring districts are (from west clockwise) Saarpfalz, the district-free city Zweibrücken, the districts Kaiserslautern and Bad Dürkheim, the district-free city Landau (the Taubensuhl/Fassendeich forest part of the city), Südliche Weinstraße, and the French ''département'' Bas-Rhin. The district-free city Pirmasens is surrounded by the district. History The district was created 18 February 1818 as the ''Landkommisariat Pirmasens''. During the communal reforms of 1968-72, several changes were made to the district. In 1969, the neighboring district Bad Bergzabern was dissolved and some part of it was added, while other municipalities were incorporated into the city Pirmasens. In 1972, the district ''Landkreis Zweibrücken'' was dissolved and added into the district ''Landkreis Pirmasens'', which on 1 January 1997 renamed itself to ''Südwestpfalz''. Geogra ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Queich
The Queich is a tributary of the Rhine, which rises in the southern part of the Palatinate Forest, and flows through the Upper Rhine valley to its confluence with the Rhine in Germersheim. It is long and is one of the four major drainage systems of the Palatinate Forest along with the Speyerbach, Lauter and Schwarzbach. The Queich flows through the towns Hauenstein, Annweiler am Trifels, Siebeldingen, Landau, Offenbach an der Queich and Germersheim. Topography Sources The Queichquelle is south of the municipality of Hauenstein at an elevation of almost on the eastern slope of the high mount ''Winterberg''. It is taken surrounded with hewn stones from the typical local red sandstone. There are also benches and a foot baths. Course and tributaries The Queich first flows as a small stream north through ''Stephanstal'' valley to Hauenstein. There, it turns east and moves in large arcs through the ''Queich valley''. It flows past Wilgartswiesen and Rinnthal, where i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rhineland-Palatinate
Rhineland-Palatinate ( , ; german: link=no, Rheinland-Pfalz ; lb, Rheinland-Pfalz ; pfl, Rhoilond-Palz) is a western state of Germany. It covers and has about 4.05 million residents. It is the ninth largest and sixth most populous of the sixteen states. Mainz is the capital and largest city. Other cities are Ludwigshafen am Rhein, Koblenz, Trier, Kaiserslautern, Worms and Neuwied. It is bordered by North Rhine-Westphalia, Saarland, Baden-Württemberg and Hesse and by the countries France, Luxembourg and Belgium. Rhineland-Palatinate was established in 1946 after World War II, from parts of the former states of Prussia (part of its Rhineland and Nassau provinces), Hesse (Rhenish Hesse) and Bavaria (its former outlying Palatinate kreis or district), by the French military administration in Allied-occupied Germany. Rhineland-Palatinate became part of the Federal Republic of Germany in 1949 and shared the country's only border with the Saar Protectorate until the latter wa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Germany
Germany,, officially the Federal Republic of Germany, is a country in Central Europe. It is the second most populous country in Europe after Russia, and the most populous member state of the European Union. Germany is situated between the Baltic and North seas to the north, and the Alps to the south; it covers an area of , with a population of almost 84 million within its 16 constituent states. Germany borders Denmark to the north, Poland and the Czech Republic to the east, Austria and Switzerland to the south, and France, Luxembourg, Belgium, and the Netherlands to the west. The nation's capital and most populous city is Berlin and its financial centre is Frankfurt; the largest urban area is the Ruhr. Various Germanic tribes have inhabited the northern parts of modern Germany since classical antiquity. A region named Germania was documented before AD 100. In 962, the Kingdom of Germany formed the bulk of the Holy Roman Empire. During the 16th ce ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Palatine Forest-North Vosges Biosphere Reserve
The Franco-German Palatinate Forest-North Vosges Biosphere Reserve (german: Biosphärenreservat Pfälzerwald-Nordvogesen, french: Réserve de biosphère transfrontalière des Vosges du Nord-Forêt palatine) was created in 1998 as the first UNESCO trans-boundary biosphere reserve in Europe. The German part became the 12th of 16 biosphere reserves in Germany and the French one the 6th of 14 in France. The biosphere reserve is a fusion of the older Palatinate Forest Nature Park in Germany and Northern Vosges Regional Nature Park in France, covering a total area of 3,018 km², with 1,809.7 km² in Germany and 1208.3 km² in France respectively. Geography Location The biosphere reserve lies in the Palatinate Forest and in the North Vosges on the boundary between the southwest German state of Rhineland-Palatinate and the northeast French region of Grand Est. Gallery File:Biosphärenhaus.jpg, Biosphere house in Fischbach near Dahn File:WipfelpfadTurm.jpg, Platforms on the Bau ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Palatinate Region
The Palatinate (german: Pfalz; Palatine German: ''Palz'') is a region of Germany. In the Middle Ages it was known as the Rhenish Palatinate (''Rheinpfalz'') and Lower Palatinate (''Unterpfalz''), which strictly speaking designated only the western part of the Electorate of the Palatinate (''Kurfürstentum Pfalz''), as opposed to the Upper Palatinate (''Oberpfalz''). It occupies roughly the southernmost quarter of the German federal state of Rhineland-Palatinate (''Rheinland-Pfalz''), covering an area of with about 1.4 million inhabitants. Its residents are known as Palatines (''Pfälzer''). Geography The Palatinate borders Saarland in the west, historically also comprising the state's Saarpfalz District. In the northwest, the Hunsrück mountain range forms the border with the Rhineland region. The eastern border with Hesse and the Baden region runs along the Upper Rhine river, while the left bank, with Mainz and Worms as well as the Selz basin around Alzey, belong to the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bunter Sandstone
The Buntsandstein (German for ''coloured'' or ''colourful sandstone'') or Bunter sandstone is a lithostratigraphic and allostratigraphic unit (a sequence of rock strata) in the subsurface of large parts of west and central Europe. The Buntsandstein predominantly consists of sandstone layers of the Lower Triassic series and is one of three characteristic Triassic units, together with the Muschelkalk and Keuper that form the Germanic Trias Supergroup. The Buntsandstein is similar in age, facies and lithology with the Bunter of the British Isles. It is normally lying on top of the Permian Zechstein and below the Muschelkalk. In the past the name Buntsandstein was in Europe also used in a chronostratigraphic sense, as a subdivision of the Triassic system. Among reasons to abandon this use was the discovery that its base lies actually in the latest Permian. Origin The Buntsandstein was deposited in the Germanic Basin, a large sedimentary basin that was the successor of the smal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
