|
Schwarzwälder Hochwald
The Schwarzwälder Hochwald (; literally 'Black Forest High Forest'), not to be confused with the High Black Forest, is the high south-western part of the Hunsrück in the German states of Saarland and Rhineland-Palatinate. SWRDer Schwarzwälder Hochwald/ref> The mountains are up to 816.32 m high. Geography Location The Schwarzwälder Hochwald lies within the Saar-Hunsrück Nature Park, running roughly from Mettlach in the Saarland to the Erbeskopf in Rhineland-Palatinate. It lies northwest of Losheim, Weiskirchen, Wadern and Nonnweiler in the Saarland and between Hermeskeil and Birkenfeld and between Thalfang and Idar-Oberstein in Rhineland-Palatinate. North of the Schwarzwälder Hochwald lies the Osburger Hochwald; both forested mountain ranges are known simply as the Hochwald ("High Forest"). The southeastern part of the Schwarzwälder Hochwald is called the Dollberge. To the northeast of the Schwarzwälder Hochwald is the Idar Forest. Mountains The mountains a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Osburger Hochwald
The Osburger Hochwald ("Osburg Upland Forest") lies southeast of the Osburger Hunsrück and has an area of 75 square kilometres. Together with the Schwarzwälder Hochwald, it forms the ''Hochwald'' or "upland forest" of the Hunsrück, the southwestern part of the Rhenish Massif in the German state of Rhineland-Palatinate. The area belongs to the Saar-Hunsrück Nature Park. Northeast of the Hochwald are the Idar Forest and Soonwald. At the foot of the Rösterkopf rises the River Ruwer, a right tributary of the Moselle. The watershed between the Moselle (Feller Bach and Ruwer) and the Saar (Wadrill/Prims The Prims is a 91 km long river in western Germany, right tributary of the Saar. It rises in the Hunsrück mountains, near the village Malborn. It flows generally south through the towns Nonnweiler, Wadern and Schmelz. It flows into the Saar ...) runs through the Osburger Hochwald. The B 52 federal road and A 1 motorway, as well as several local, county and state roa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Trier-Saarburg
Trier-Saarburg (; lb, Landkrees Tréier-Saarburg ) is a district in the west of Rhineland-Palatinate, Germany. Neighboring districts are (from the north and clockwise) Bitburg-Prüm, Bernkastel-Wittlich, Birkenfeld, Sankt Wendel (Saarland), and Merzig-Wadern (Saarland). To the west it borders Luxembourg. The district-free city Trier is surrounded by the district. History The district was created in 1969 by merging the previous districts Trier and Saarburg. Geography The main river in the district is the Moselle. The area between its tributaries, the Ruwer and the Saar, is also well known as one of the prime wine regions of Germany. Museums * Roscheider Hof Open Air Museum, Konz * Fell Exhibition Slate Mine * Air museum, Hermeskeil * Railway and steam engine museum, Hermeskeil Coat of arms The coat of arms largely resembles the coat of arms of the Saarburg district. The castle in the middle shows the castle of Saarburg, even though now only the ruins of the castle remains. Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Neuhütten (Hochwald)
Neuhütten is a community in the Main-Spessart district in the ''Regierungsbezirk'' of Lower Franconia (''Unterfranken'') in Bavaria, Germany and a member of the ''Verwaltungsgemeinschaft'' (municipal association) of Partenstein. It has a population of around 1,100. Geography Location Neuhütten lies in the Main-Spessart district in the Würzburg region. I is located in the '' Mittelgebirge'' Spessart. The municipal territory mostly lies in the valley of a tributary of the Lohrbach but stretches into the valley of the Lohrbach river itself, which passes to the north. The highest elevation of the municipality is to the southeast, on the slopes of Hengstkopf. Subdivision The community has two ''Gemarkungen'' (traditional rural cadastral area): Neuhütten and Forst Lohrer Strasse. The former contains the ''Ortsteil'' Neuhütten (Dorf). The latter consists of three exclaves: Bischborner Hof, Lohrerstrasse and Birkig. These lie on the Bundesstrasse 26 and are surrounded ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landkreis Birkenfeld
Birkenfeld () is a district (''Landkreis'') in Rhineland-Palatinate, Germany. Its seat is the town of Birkenfeld. It is bounded by (from the south and clockwise) the districts of Sankt Wendel (Saarland), Trier-Saarburg, Bernkastel-Wittlich, Rhein-Hunsrück, Bad Kreuznach and Kusel. History In the early nineteenth century, the Nahe River was the boundary between two tiny principalities: Birkenfeld, west of the Nahe; and Lichtenberg, east of it. The principality of Birkenfeld was annexed by Oldenburg in 1817; Lichtenberg became an exclave of the Duchy Saxe-Coburg (Saxe-Coburg-Saalfeld until 1826, Saxe-Coburg and Gotha thereafter). Prussia bought Lichtenberg in 1834 and made it the District of Sankt Wendel Sankt Wendel is a town in northeastern Saarland. It is situated on the river Blies 36 km northeast of Saarbrücken, the capital of Saarland, and is named after Saint Wendelin of Trier. According to a survey by the German Association for Hou .... After World War I, th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Börfink
Börfink is an ''Ortsgemeinde'' – a municipality belonging to a ''Verbandsgemeinde'', a kind of collective municipality – in the Birkenfeld district in Rhineland-Palatinate, Germany. It belongs to the ''Verbandsgemeinde'' of Birkenfeld, whose seat is in the like-named town. Geography Location The municipality lies on the Traunbach near the 816 m-high Erbeskopf in the ''Schwarzwälder Hochwald'' (forest) in the Hunsrück. The municipal area is 78.8% wooded. Neighbouring municipalities Börfink borders in the southeast on Abentheuer and in the southwest on Muhl, an outlying centre of Neuhütten. Constituent communities Also belonging to Börfink are the outlying homesteads of Einschiederhof, Forellenhof Trauntal and Thranenweier. Climate Yearly precipitation in Börfink amounts to 1 133 mm, which is very high, falling into the highest tenth of the precipitation chart for all Germany. At 91% of the German Weather Service's weather stations, lower figures are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Normalnull
("standard zero") or (short N. N. or NN ) is an outdated official vertical datum used in Germany. Elevations using this reference system were to be marked (“meters above standard zero”). has been replaced by (NHN). History In 1878 reference heights were taken from the Amsterdam Ordnance Datum and transferred to the New Berlin Observatory in order to define the . has been defined as a level going through an imaginary point 37.000 m below . When the New Berlin Observatory was demolished in 1912 the reference point was moved east to the village of Hoppegarten (now part of the town of Müncheberg, Brandenburg, 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 betwe ...).S. German: ''Was ist "Normal-Null"?''. In: ''Physikalische Blätter'' 1958, vol 14, issue 2, p. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sea Level
Mean sea level (MSL, often shortened to sea level) is an average surface level of one or more among Earth's coastal bodies of water from which heights such as elevation may be measured. The global MSL is a type of vertical datuma standardised geodetic datumthat is used, for example, as a chart datum in cartography and marine navigation, or, in aviation, as the standard sea level at which atmospheric pressure is measured to calibrate altitude and, consequently, aircraft flight levels. A common and relatively straightforward mean sea-level standard is instead the midpoint between a mean low and mean high tide at a particular location. Sea levels can be affected by many factors and are known to have varied greatly over geological time scales. Current sea level rise is mainly caused by human-induced climate change. When temperatures rise, Glacier, mountain glaciers and the Ice sheet, polar ice caps melt, increasing the amount of water in water bodies. Because most of human settlem ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hill
A hill is a landform that extends above the surrounding terrain. It often has a distinct Summit (topography), summit. Terminology The distinction between a hill and a mountain is unclear and largely subjective, but a hill is universally considered to be not as tall, or as Grade (slope), steep as a mountain. Geographers historically regarded mountains as hills greater than above sea level, which formed the basis of the plot of the 1995 film ''The Englishman who Went up a Hill but Came down a Mountain''. In contrast, hillwalkers have tended to regard mountains as peaks above sea level. The ''Oxford English Dictionary'' also suggests a limit of and Whittow states "Some authorities regard eminences above as mountains, those below being referred to as hills." Today, a mountain is usually defined in the UK and Ireland as any summit at least high, while the official UK government's definition of a mountain is a summit of or higher. Some definitions include a topographical pro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain
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 (topography), 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 Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, 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 Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
