|
Ernstberg
The Ernstberg (also Erresberg) southeast of Hinterweiler is, at 698.8 m, the highest of the west Eifel volcanoes and, after the Hohe Acht, the second highest mountain in the Eifel overall. Its summit consists of pyroclastic rocks (''Schweißschlacken'') that form a volcanic crater that is open towards the east. This is where the basalt masses flowed out, forming a semicircle on the eastern slope of the mountain. It lies within the Waldeifel region. In winter there are excellent winter sports conditions on the Ernstberg due to its height. Cut langlauf tracks, a toboggan slope and ski hire hut are available. Somewhat below the summit is a cave that runs through to the other side of the mountain and which is a natural monument. The cave entrances are barred to prevent access. in the database of cul ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hinterweiler
Hinterweiler is an ''Ortsgemeinde'' – a Municipalities of Germany, municipality belonging to a ''Verbandsgemeinde'', a kind of collective municipality – in the Vulkaneifel Districts of Germany, district in Rhineland-Palatinate, Germany. It belongs to the Daun (Verbandsgemeinde), ''Verbandsgemeinde'' of Daun, whose seat is in the Daun, Germany, like-named town. Geography The municipality lies in the Vulkan Eifel, 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. History Although Hinterweiler has never had the importance of some other centres, it can look back on a long history. Finds in the area called ''Im Gemeindewinkel'' (“In the Municipality’s Corner”) show that there must have been a Celts, Celtic settlement there. Traces of settlement from Ancient Rome, Roman times found to the north of the village at the foot of the Ernstb ... [...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] |
Vulkan Eifel
The Volcanic Eifel or Vulkan Eifel (german: Vulkaneifel) is a region in the Eifel Mountains in Germany that is defined to a large extent by its volcanic geological history. Characteristic of this volcanic field are its typical explosion crater lakes or maars, and numerous other signs of volcanic activity such as volcanic tuffs, lava streams and volcanic craters like the Laacher See. The Volcanic Eifel is still volcanically active today. One sign of this activity is the escaping gases in the Laacher See. Geographical location The Volcanic Eifel stretches from the Rhine to the Wittlich Depression. It is bordered in the south and southwest by the South Eifel, in the west by Luxembourg and Belgian Ardennes and in the north by the North Eifel including the Hohes Venn. To the east the Rhine forms its geographical boundary, with no volcanicity immediately beyond it. The Volcanic Eifel is divided into three natural regions: * Volcanic West Eifel ( Manderscheid, Daun, Gerolstein, Ober ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Weinfelder Maar
__NOTOC__ The Weinfelder Maar, also called the Totenmaar, is a maar around two kilometres southeast of the town of Daun in the Eifel Mountains, in the German state of Rhineland-Palatinate. Geography The maar lake was formed about 10,500 years ago by a volcanic steam explosion and is around 525 metres long, 375 metres wide and 51 metres deep. It has a surface area of about 16.8 hectares. The maar lies at a height of . The embankment surrounding the lake is made from tuff and is higher in the west and south than in the north and east. Along the course of this bank is the ''Mäuseberg'' (561.2 m) and the ''Maarkreuz'' (534.5 m). The lake region is now a nature reserve and bathing in the lake is forbidden.eifelreise.deWeinfelder Maar/ref> Name The description "Totenmaar" ("maar of the dead") comes from the cemetery in the immediate vicinity of the maar with its little chapel, parts of which date to the 14th century. This was the old parish church ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nature Reserve (Germany)
A ''Naturschutzgebiet'' (abbreviated NSG) is a category of protected area (nature reserve) within Germany's Federal Nature Conservation Act (the ''Bundesnaturschutzgesetz'' or ''BNatSchG''). Although often translated as 'Nature Reserve' in English, the Federal Agency for Nature Conservation (BfN) refers to them as 'Nature Conservation Areas'. It meets the criteria of an IUCN IUCN protected area categories#Category IV – Habitat/Species Management Area, Category IV Habitat and Species Management Area.https://www.bfn.de/fileadmin/MDB/documents/themen/gebietsschutz/IUCN_Kat_Schutzgeb_Richtl_web.pdf Document of the Federal Agency for Nature Conservation of Germany Points of law The use of the term ''Naturschutzgebiet'' or terms that could be confused with it for anything other than the legally protected areas is forbidden under this law. Signage Because legal restrictions are placed on activity within German nature reserves they have to be signed on the ground. Only by this mea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nature Reserves In Rhineland-Palatinate
Nature, in the broadest sense, is the physical world or universe. "Nature" can refer to the phenomena of the physical world, and also to life in general. The study of nature is a large, if not the only, part of science. Although humans are part of nature, human activity is often understood as a separate category from other natural phenomena. The word ''nature'' is borrowed from the Old French ''nature'' and is derived from the Latin word ''natura'', or "essential qualities, innate disposition", and in ancient times, literally meant "birth". In ancient philosophy, ''natura'' is mostly used as the Latin translation of the Greek word '' physis'' (φύσις), which originally related to the intrinsic characteristics of plants, animals, and other features of the world to develop of their own accord. The concept of nature as a whole, the physical universe, is one of several expansions of the original notion; it began with certain core applications of the word φύσις by pre-So ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Under 1000 Metres
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 terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains And Hills Of The Eifel
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 terrain ... [...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 terrain ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Perennial Honesty
''Lunaria rediviva'', known as perennial honesty, is a species of plant in the cabbage family Brassicaceae. This hairy-stemmed herbaceous perennial is found throughout Europe. It often grows in damp woods on lime substrates. Growing up to tall, it has large, pointed oval leaves with marked serrations. Clusters of fragrant, pale pink flowers are borne in spring, followed by translucent oval seedheads, often used in flower arranging. It is cultivated as a garden plant, and has gained the Royal Horticultural Society's Award of Garden Merit. The Latin specific epithet ''rediviva'' means "growing again", "reviving", in reference to its perennial habit, which distinguishes it from its biennial or annual cousin, ''Lunaria annua ''Lunaria annua'', called honesty or annual honesty in English, is a species of flowering plant in the cabbage and mustard family Brassicaceae. It is native plant, native to the Balkans and south west Asia, and cultivated throughout the temperate ...''. Lu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nepheline
Nepheline, also called nephelite (), is a rock-forming mineral in the feldspathoid groupa silica-undersaturated aluminosilicate, Na3 K Al4 Si4 O16, that occurs in intrusive and volcanic rocks with low silica, and in their associated pegmatites. It is used in glass and ceramic manufacturing and other industries, and has been investigated as an ore of aluminium. Description and properties Nepheline crystals are rare and belong to the hexagonal system, usually having the form of a short, six-sided prism terminated by the basal plane. The crystals appear to have more symmetry than they actually possess, but unsymmetrical etched figures produced artificially on the prism faces indicate that the crystals are hemimorphic and tetartohedral, the only element of symmetry being a polar hexad axis. Nepheline is found in compact, granular aggregates, and can be white, yellow, gray, green, or reddish. Its hardness on the Mohs scale is 5.5–6, and its specific gravity 2.60–2.65. It i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stratovolcano
A stratovolcano, also known as a composite volcano, is a conical volcano built up by many layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a summit crater and periodic intervals of explosive eruptions and effusive eruptions, although some have collapsed summit craters called calderas. The lava flowing from stratovolcanoes typically cools and hardens before spreading far, due to high viscosity. The magma forming this lava is often felsic, having high-to-intermediate levels of silica (as in rhyolite, dacite, or andesite), with lesser amounts of less-viscous mafic magma. Extensive felsic lava flows are uncommon, but have travelled as far as . Stratovolcanoes are sometimes called composite volcanoes because of their composite stratified structure, built up from sequential outpourings of erupted materials. They are among the most common types of volcanoes, in contrast to the less common shield volca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
.jpg "Click for more on -> Nature Reserves In Rhineland-Palatinate")
