|
Großer Eyberg
The Großer Eyberg is a hill in the southern Palatine Forest in Germany. It lies in the county of Südwestpfalz in the borough of Dahn in an area known as the Dahner Felsenland, a part of the 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 north .... This region which comprises the southern part of the Palatine Forest and the northern part of the Vosges Mountains. It is the highest hill in the western Wasgau. At the summit of the Eyberg is an 18-metre-high, observation tower, of steel lattice construction, built between 1945 and 1949 by the French Army. The tower can only be accessed over unmetalled hiking trails. References {{DEFAULTSORT:Eyberg, Grosser Mountains and hills of Rhineland-Palatinate Mountains and hills of the Palatinate Forest Dahn ... [...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 Phalsbour ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dahner Felsenland
The Dahner Felsenland, also referred to as the Dahn Rockland, is a landscape in the county of Südwestpfalz in the German federal state of Rhineland-Palatinate. It is located in the middle section of the Wasgau, which in turn forms the southern part of the Palatine Forest and the northern part of the Vosges in France. The Dahner Felsenland has numerous rock formations within the South Palatinate Climbing Area (''Klettergebiet Südpfalz''). Geographic location The landscape covers almost the same area as the collective municipality of the same name, which incorporates the town of Dahn and 14 villages. The Dahner Felsenland is part of the Palatine Forest Nature Park. It lies between 200 m (valleys) and 400 m (hilltops) high and is drained by the Lauter, which here in its upper reaches is called the ''Wieslauter'', into the River Rhine. Tourism The region has been opened up by a large number of waymarked walking routes. In Dahn itself is the Felsenland Youth ... [...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] |
Conical Hill
A conical hill (also cone or conical mountain) is a landform with a distinctly conical shape. It is usually isolated or rises above other surrounding foothills, and is often of volcanic origin. Conical hills or mountains occur in different shapes and are not necessarily geometrically-shaped cones; some are more tower-shaped or have an asymmetric curve on one side of the hill. Typically, however, they have a circular base and smooth sides with a gradient of up to 30°. Such conical mountains are found in all volcanically-formed areas of the world such as the Bohemian Central Uplands in the Czech Republic, the Rhön in Germany or the Massif Central in France. Term The conical hill as a geomorphological term first appeared in the German language, as ''Kegelberg'', coined by Goethe and geologists of his era. From their natural appearance these were mostly basaltic or phonolitic landforms in the shape of a mathematical cone, hence why the term came to be used in the early geolog ... [...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] |
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] |
Dahn
Dahn is a municipality in the Südwestpfalz district, in Rhineland-Palatinate, Germany. It is situated in the Palatinate Forest, approximately 15 km southeast of Pirmasens, and 25 km west of Landau. It is part of the ''Verbandsgemeinde'' ("collective municipality") of Dahner Felsenland. Geography Dahn is located 210 m above sea level in a valley of the Dahner Felsenland, a part of the Wasgau, which is itself a part of the Palatinate Forest. A small creek, the Lauter, flows through Dahn, and here, in the area of its headwaters, is called the ''Wieslauter''. The border with Alsace (France) is located 10 km south of Dahn. History Coat of arms In 1952 the coat of arms was recreated as a result of historical research. The new shield, parted per chevron, has on its dexter chief: azure (blue), a cross argent (silver); on its sinister chief: gules (red), an eagle argent (silver) and on its base: or (gold), a fir tree vert (green). The fir tree (german: Tanne, ssu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vosges Mountains
The Vosges ( , ; german: Vogesen ; Franconian and gsw, Vogese) are a range of low mountains in Eastern France, near its border with Germany. Together with the Palatine Forest to the north on the German side of the border, they form a single geomorphological unit and low mountain range of around in area. It runs in a north-northeast direction from the Burgundian Gate (the Belfort–Ronchamp– Lure line) to the Börrstadt Basin (the Winnweiler– Börrstadt–Göllheim line), and forms the western boundary of the Upper Rhine Plain. The Grand Ballon is the highest peak at , followed by the Storkenkopf (), and the Hohneck ().IGN maps available oGéoportail/ref> Geography Geographically, the Vosges Mountains are wholly in France, far above the Col de Saverne separating them from the Palatinate Forest in Germany. The latter area logically continues the same Vosges geologic structure but traditionally receives this different name for historical and political reasons. From ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains And Hills Of Rhineland-Palatinate
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
