|
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eifel - Deutsche Mittelgebirge, Serie A-de
The Eifel (; , ) is a low mountain range in western Germany, eastern Belgium and northern Luxembourg. 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. The Eifelian stage in geological history is named after the region because rocks of that period reach the surface in the Eifel at the Wetteldorf Richtschnitt outcrop. The inhabitants of the Eifel are known as Eiflers or Eifelers. 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 a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rhine Massif
The Rhenish Massif, Rhine Massif or Rhenish Uplands (, : 'Rhenish Slate Uplands') is a geologic massif in western Germany, eastern Belgium, Luxembourg and northeastern France. It is drained centrally, south to north by the river Rhine and a few of its tributaries. West of the indent of the Cologne Bight it has the Eifel and the Belgian and French Ardennes; east is its greatest German component, the Süder Uplands. The Hunsrück hills form its southwest. The Westerwald is an eastern strip. The Lahn-Dill area is a small central zone and the Taunus Mountains form the rest, the south-east. The massif hosts the Middle Rhine Valley ( Rhine Gorge), a UNESCO World Heritage site linked to the lowest parts of the Moselle (, ). Geology Geologically the Rhenish Massif consists of metamorphic rocks, mostly slates (hence its German name), deformed and metamorphosed during the Hercynian orogeny (around 300 million years ago). Most of the massif is part of the Rhenohercynian zone of thi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alfred Andersch
Alfred Hellmuth Andersch (; 4 February 1914 – 21 February 1980) was a German writer, publisher, and radio editor. The son of a conservative East Prussian army officer, he was born in Munich, Germany, and died in Berzona, Ticino, Switzerland. Martin Andersch, his brother, was also a writer. Life His parents were Alfred Andersch (1875–1929) and his wife Hedwig, née Watzek (1884–1976). His school master was Joseph Gebhard Himmler, the father of Heinrich Himmler. He wrote about this in '' The Father of a Murderer''. 1914 to 1945 In 1930, after an apprenticeship as a bookseller, Andersch became a youth leader in the Communist Party. As a consequence, he was held for six months in the Dachau concentration camp in 1933. He then left the party and entered a depressive phase of "total introversion". It was during this period that he first became engaged in the arts, adopting the stance that became known as ''innere Emigration'' ("internal emigration") – despite remaining in G ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Winterspelt
Winterspelt 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 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 popu .... References Bitburg-Prüm {{BitburgPrüm-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eurasian Lynx
The Eurasian lynx (''Lynx lynx'') is one of the four wikt:extant, extant species within the medium-sized wild Felidae, cat genus ''Lynx''. It is widely distributed from Northern Europe, Northern, Central Europe, Central and Eastern Europe to Central Asia and Siberia, the Tibetan Plateau and the Himalayas. It inhabits Temperate forest, temperate and boreal forests up to an elevation of . Despite its wide distribution, it is threatened by habitat loss and habitat fragmentation, fragmentation, poaching and depletion of prey. Taxonomy ''Felis lynx'' was the scientific name used in 1758 by Carl Linnaeus in his work ''Systema Naturae''. In the 19th and 20th centuries, the following Eurasian lynx subspecies were proposed: The following were also proposed, but are not considered Valid name (zoology), valid taxa: *Altai lynx (''L. l. wardi'') *Baikal lynx (''L. l. kozlovi'') *Amur lynx (''L. l. stroganovi'') *Sardinian lynx (''L. l. sardiniae'') Characteristics The Eurasian lyn ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
European Wildcat
The European wildcat (''Felis silvestris'') is a small wildcat species native to continental Europe, Great Britain, Turkey and 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 silvestris caucasica'' proposed by Konstantin Satunin in 1905 was a skin of a female cat collected ne ... [...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 ... [...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 histor ... [...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 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 popu .... References Bitburg-Prüm {{BitburgPrüm-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quartzite
Quartzite is a hard, non- foliated metamorphic rock that 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, and hence quartzite is a metasandstone. 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 resist ... [...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), as well as the current and most recent of the twelve periods of the Phanerozoic eon. 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); a proposed third epoch, the Anthropocene, was rejected in 2024 by IUGS, the governing body of the ICS. The Quaternary is typically defined by the Quaternary glaciation, 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 succ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Erosion
Erosion is the action of surface processes (such as Surface runoff, water flow or wind) that removes soil, Rock (geology), rock, or dissolved material from one location on the Earth's crust#Crust, Earth's crust and then sediment transport, transports it to another location where it is deposit (geology), 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 Solvation, 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 Wind wave, waves; glacier, glacial Plucking (glaciation), plucking, Abrasion (geology), abrasion, and scour; areal flooding; Aeolian processes, wind abrasion; groundwater processes; and Mass wastin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
