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Schnee-Eifel
The Schnee Eifel is a heavily wooded landscape in Germany's Central Uplands, up to , that forms part of the western Eifel in the area of the German-Belgian border. The name may have been derived in the 19th century from the Schneifel chain of hills which had nothing to do with snow (''Schnee''), but with the name for a forest swathe (''Schneise''). Geography The Schnee Eifel natural region is formed by the southern part of the Hohes Venn-Eifel Nature Park. To the north it is bounded by the river Kyll, the border with the North Eifel, that begins near Hallschlag and Kronenburg with the Zitter Forest; To the east the Kyll forms the boundary river with the High Eifel. To the south the Schnee Eifel merges into the South Eifel to Pronsfeld in the Prümer Land. Its highest elevation is found on the Schneifel ridge: the high Schwarzer Mann ("Black Man"). The term ''Schneifel'' is frequently employed in publications to mean the whole Schnee Eifel region, but they are not syn ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eifel - Deutsche Mittelgebirge, Serie A-de
The Eifel (; lb, Äifel, ) is a low mountain range in western Germany and eastern Belgium. It occupies parts of southwestern North Rhine-Westphalia, northwestern Rhineland-Palatinate and the southern area of the German-speaking Community of Belgium. The Eifel is part of the Rhenish Massif; within its northern portions lies the Eifel National Park. Geography Location The Eifel lies between the cities of Aachen to the north, Trier to the south and Koblenz to the east. It descends in the northeast along a line from Aachen via Düren to Bonn into the Lower Rhine Bay. In the east and south it is bounded by the valleys of the Rhine and the Moselle. To the west it transitions in Belgium and Luxembourg into the geologically related Ardennes and the Luxembourg Ösling. In the north it is limited by the Jülich-Zülpicher Börde. Within Germany it lies within the states of Rhineland-Palatinate and North Rhine-Westphalia; in the Benelux the area of Eupen, St. Vith and Luxembourg. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eifel
The Eifel (; lb, Äifel, ) is a low mountain range in western Germany and eastern Belgium. It occupies parts of southwestern North Rhine-Westphalia, northwestern Rhineland-Palatinate and the southern area of the German-speaking Community of Belgium. The Eifel is part of the Rhenish Massif; within its northern portions lies the Eifel National Park. Geography Location The Eifel lies between the cities of Aachen to the north, Trier to the south and Koblenz to the east. It descends in the northeast along a line from Aachen via Düren to Bonn into the Lower Rhine Bay. In the east and south it is bounded by the valleys of the Rhine and the Moselle. To the west it transitions in Belgium and Luxembourg into the geologically related Ardennes and the Luxembourg Ösling. In the north it is limited by the Jülich-Zülpicher Börde. Within Germany it lies within the states of Rhineland-Palatinate and North Rhine-Westphalia; in the Benelux the area of Eupen, St. Vith and Luxemb ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schneifel
The Schneifel is a range of low mountains, up to , in the western part of the Eifel in Germany, near the Belgian border. It runs from Brandscheid near Prüm in a northeasterly direction to Ormont. The name Schneifel has nothing to do with the German words ''Schnee'' (snow) and ''Eifel''. It is derived from the former dialect of this region and means something like ''Schneise'' ("swathe"). This swathe ran over the mountains. The term was "Germanised" during the Prussian era and the term Schnee-Eifel ("Snow Eifel") was born, albeit referring to a larger area. Winters in this low mountainous region are unusually cold and snowy for western and parts of central Europe and snow lies here for longer than anywhere else in the Eifel. As a result, the winter sports season is longer here than in the surrounding region. The highest point of the Schneifel is the 699.1-metre-high Schwarze Mann ("Black Man"), which is also the third highest point of the Eifel range after the Hohe Acht and the Er ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hallschlag
Hallschlag is a village in the Vulkaneifel district in Rhineland-Palatinate, Germany. The municipality (German: ''Ortsgemeinde'') belongs to the ''Verbandsgemeinde'' of Obere Kyll, whose seat is in the municipality of Gerolstein. Geography The municipality lies between and above sea level on the boundary between the Vulkaneifel – a part of the Eifel known for its volcanic history, geographical and geological features, and even ongoing activity today, including gases that sometimes well up from the earth – and the Rheinisches Schiefergebirge (Rhenish Slate Mountains), on the edge of the Schnee-Eifel. Hallschlag lies in a hollow and is nestled in the charming countryside of the Middle Eifel. It belongs to the recreational region of ''Oberes Kylltal'' (“Upper Kyll Valley”). Three kilometres away to the west runs the Belgian border. The municipal area borders in the west, north and east on North Rhine-Westphalia. History In 1322, Hallschlag had its first documenta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brandscheid
Brandscheid is a municipality in the district of Bitburg-Prüm, in Rhineland-Palatinate, western 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 .... References Bitburg-Prüm {{BitburgPrüm-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Devonian
The Devonian ( ) is a geologic period and system of the Paleozoic era, spanning 60.3 million years from the end of the Silurian, million years ago (Mya), to the beginning of the Carboniferous, Mya. It is named after Devon, England, where rocks from this period were first studied. The first significant adaptive radiation of life on dry land occurred during the Devonian. Free-sporing vascular plants began to spread across dry land, forming extensive forests which covered the continents. By the middle of the Devonian, several groups of plants had evolved leaves and true roots, and by the end of the period the first seed-bearing plants appeared. The arthropod groups of myriapods, arachnids and hexapods also became well-established early in this period, after starting their expansion to land at least from the Ordovician period. Fish reached substantial diversity during this time, leading the Devonian to often be dubbed the Age of Fishes. The placoderms began dominating ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Erosion
Erosion is the action of surface processes (such as water flow or wind) that removes soil, rock, or dissolved material from one location on the Earth's crust, and then transports it to another location where it is deposited. Erosion is distinct from weathering which involves no movement. Removal of rock or soil as clastic sediment is referred to as ''physical'' or ''mechanical'' erosion; this contrasts with ''chemical'' erosion, where soil or rock material is removed from an area by dissolution. Eroded sediment or solutes may be transported just a few millimetres, or for thousands of kilometres. Agents of erosion include rainfall; bedrock wear in rivers; coastal erosion by the sea and waves; glacial plucking, abrasion, and scour; areal flooding; wind abrasion; groundwater processes; and mass movement processes in steep landscapes like landslides and debris flows. The rates at which such processes act control how fast a surface is eroded. Typically, physical erosion procee ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quaternary
The Quaternary ( ) is the current and most recent of the three periods of the Cenozoic Era in the geologic time scale of the International Commission on Stratigraphy (ICS). It follows the Neogene Period and spans from 2.58 million years ago to the present. The Quaternary Period is divided into two epochs: the Pleistocene (2.58 million years ago to 11.7 thousand years ago) and the Holocene (11.7 thousand years ago to today, although a third epoch, the Anthropocene, has been proposed but is not yet officially recognised by the ICS). The Quaternary Period is typically defined by the cyclic growth and decay of continental ice sheets related to the Milankovitch cycles and the associated climate and environmental changes that they caused. Research history In 1759 Giovanni Arduino proposed that the geological strata of northern Italy could be divided into four successive formations or "orders" ( it, quattro ordini). The term "quaternary" was introduced by Jules Desnoye ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quartzite
Quartzite is a hard, non- foliated metamorphic rock which was originally pure quartz sandstone.Essentials of Geology, 3rd Edition, Stephen Marshak, p 182 Sandstone is converted into quartzite through heating and pressure usually related to tectonic compression within orogenic belts. Pure quartzite is usually white to grey, though quartzites often occur in various shades of pink and red due to varying amounts of hematite. Other colors, such as yellow, green, blue and orange, are due to other minerals. The term ''quartzite'' is also sometimes used for very hard but unmetamorphosed sandstones that are composed of quartz grains thoroughly cemented with additional quartz. Such sedimentary rock has come to be described as orthoquartzite to distinguish it from metamorphic quartzite, which is sometimes called metaquartzite to emphasize its metamorphic origins. Quartzite is very resistant to chemical weathering and often forms ridges and resistant hilltops. The nearly pure silica conte ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
European Wildcat
The European wildcat (''Felis silvestris'') is a small wildcat species native to continental Europe, Scotland, Turkey and the Caucasus. It inhabits forests from the Iberian Peninsula, Italy, Central and Eastern Europe to the Caucasus. Its fur is brownish to grey with stripes on the forehead and on the sides and has a bushy tail with a black tip. It reaches a head-to-body length of up to with a long tail, and weighs up to . In France and Italy, the European wildcat is predominantly nocturnal, but also active in the daytime when undisturbed by human activities. It preys foremost on small mammals such as lagomorphs and rodents, but also on ground-dwelling birds. Taxonomy ''Felis (catus) silvestris'' was the scientific name proposed in 1778 by Johann von Schreber when he described a wild cat based on texts from the early 18th century and before. In the 19th and 20th centuries, several wildcat type specimens were described and proposed as subspecies, including: * ''Felis silvest ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ormont
Ormont is an ''Ortsgemeinde'' (a municipality belonging to a ''Verbandsgemeinde'', a kind of collective municipality) situated in the Vulkaneifel district in Rhineland-Palatinate, Germany. It belongs to the ''Verbandsgemeinde'' of Gerolstein, whose seat is in the municipality of Gerolstein. Name It is often supposed that Ormont's name is of French origin (''or'' = “gold”; ''mont'' = “mountain”), but this is not so. In the ''Liber Aureus'', the “Golden Book” of the town of Prüm, is a boundary description for the centres of Olzheim and Ormont. Here, the village is called ''Aurimuncio'', in Mediaeval Latin. Nonetheless, this does have the same literal meaning as the supposed French derivation (''aurum'' = “gold”; ''mons/montem'' = “mountain”). Either way, therefore, the municipality's name means “Gold Mountain”. Geography Location The municipality lies at the foot of the Schneifel in the Vulkaneifel, a part of the Eifel known for its volcanic history ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stadtkyll
Stadtkyll is an ''Ortsgemeinde'' – a municipality belonging to a ''Verbandsgemeinde'', a kind of collective municipality – in the Vulkaneifel district in Rhineland-Palatinate, Germany. It belongs to the ''Verbandsgemeinde'' of Gerolstein, whose seat is in the municipality of Gerolstein. Stadtkyll is a state-recognized climatic spa (''Luftkurort''). Geography Location The municipality lies in the Vulkaneifel, a part of the Eifel known for its volcanic history, geographical and geological features, and even ongoing activity today, including gases that sometimes well up from the earth. Stadtkyll lies on the river Kyll. Constituent communities Stadtkyll's ''Ortsteile'' are Niederkyll, Schönfeld and Stadtkyll. History Near the village and in the outlying centre of Niederkyll, many finds from Roman times have been unearthed during excavation work. In the lists of the Archiepiscopal Cathedraticum, which come from about 1100, is a mention of the village under the name Kyl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
