Großer Eyberg
   HOME





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. 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, Eyburg Tower, 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]  


picture info

Palatine Forest
The Palatinate Forest (; ), sometimes also called the Palatine Forest, is a low-mountain region in southwestern Germany, located in the Palatinate in the state of Rhineland-Palatinate. The forest is a designated nature park () covering 1,771 km2 and its highest elevation is the Kalmit (672.6 m). Together with the northern part of the adjacent Vosges Mountains in France it forms the UNESCO-designated Palatinate Forest-North Vosges Biosphere Reserve. Geography Topography The Palatinate Forest, together with the Vosges south of the French border, from which it has no morphological separation, is part of a single central upland region of about 8,000 km2 in area, that runs from the Börrstadt Basin (a line from Winnweiler via Börrstadt and Göllheim) to the Burgundian Gate (on the line Belfort– Ronchamp– Lure) and which forms the western boundary of the Upper Rhine Plain. This landscape forms, in turn, the eastern part of the very extensive eastern s ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Wasgau
The Wasgau (, ) is a France, Franco-Germany, German Mountain range, hill range in the German state of Rhineland-Palatinate and the French departments of France, departments of Bas-Rhin and Moselle (department), Moselle. It is formed from the southern part of the Palatine Forest and the northern part of the Vosges, 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 Normalhöhennull, NHN) near Niederbronn-les-Bains in northern Alsace. Next, at 577 m is the only slightly lower Rehberg (Wasgau), Rehberg near Annweiler am Trifels, 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 der Pfalz, Landau in the north that, ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Dahner Felsenland
The Dahner Felsenland, also referred to as the Dahn Rockland, is a landscape in the county of Südwestpfalz in the Germany, 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 Verbandsgemeinde, collective municipality of Verbandsgemeinde Dahner Felsenland, 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 (Rhine), Lauter, which here in its upper reaches is called the ''Wieslauter'', into the River Rhine. Tourism The region has been opened up by a larg ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


Rhineland-Palatinate
Rhineland-Palatinate ( , ; ; ; ) 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 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 was returned to German control in 1957. Rhineland-Palatinate's natural and c ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


Germany
Germany, officially the Federal Republic of Germany, is a country in Central Europe. It lies between the Baltic Sea and the North Sea to the north and the Alps to the south. Its sixteen States of Germany, constituent states have a total population of over 84 million in an area of , making it the most populous member state of the European Union. It 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 Capital of Germany, nation's capital and List of cities in Germany by population, most populous city is Berlin and its main financial centre is Frankfurt; the largest urban area is the Ruhr. Settlement in the territory of modern Germany began in the Lower Paleolithic, with various tribes inhabiting it from the Neolithic onward, chiefly the Celts. Various Germanic peoples, Germanic tribes have inhabited the northern parts of modern Germany since classical ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

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 geol ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

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 sma ...
[...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''. G ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

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 Stream, creek, the Lauter (Rhine), 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 t ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Vosges Mountains
The Vosges ( , ; ; Franconian (linguistics), Franconian and ) is a range of medium mountains in Eastern France, near its France–Germany border, border with Germany. Together with the Palatine Forest to the north on the German side of the border, they form a single Geomorphology, 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, Haute-Saône, 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 (Vosges), Hohneck ().Institut Géographique National, 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 geolog ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

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 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 terrain and climate, mountains t ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]