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Plateau-de-Beille
Plateau de Beille (Occitan: ''Plan de Belha'') is a ski resort in the Pyrenees. It is situated in the Ariège department, and in the region of the Occitanie. The winter sports resort lies at a height of . For a long time, this plateau was only a place of livestock, especially cattle. It has recently become the site of a large winter sports resort of the Pyrenees, mainly dedicated to the practice of cross-country skiing, with tracks between altitude. The ski station is located between Tarascon-sur-Ariège and Ax-les-Thermes, close to the Spanish border, and above the communes of Les Cabannes, Albiès and Vèbre. Road access to the plateau (the D522) starts from Les Cabannes. Moreover, the Plateau de Beille is a crossing point of the GR 10 hiking trail that crosses the Pyrenees from east to west. Since 1998, the ascent from Les Cabannes to the plateau has regularly been used as the final ascent of a stage in the Tour de France. On the first four such occasions, the stage winner a ...
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Plateau De Beille
Plateau de Beille (Occitan language, Occitan: ''Plan de Belha'') is a ski resort in the Pyrenees. It is situated in the Ariège (department), Ariège Departments of France, department, and in the Regions of France, region of the Occitania (administrative region), Occitanie. The winter sports resort lies at a height of . For a long time, this plateau was only a place of livestock, especially cattle. It has recently become the site of a large winter sports resort of the Pyrenees, mainly dedicated to the practice of cross-country skiing, with tracks between altitude. The ski station is located between Tarascon-sur-Ariège and Ax-les-Thermes, close to the Spanish border, and above the communes of Les Cabannes, Ariège, Les Cabannes, Albiès and Vèbre. Road access to the plateau (the D522) starts from Les Cabannes. Moreover, the Plateau de Beille is a crossing point of the GR 10 (France), GR 10 hiking trail that crosses the Pyrenees from east to west. Since 1998, the ascent from Les C ...
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Gneiss
Gneiss ( ) is a common and widely distributed type of metamorphic rock. It is formed by high-temperature and high-pressure metamorphic processes acting on formations composed of igneous or sedimentary rocks. Gneiss forms at higher temperatures and pressures than schist. Gneiss nearly always shows a banded texture characterized by alternating darker and lighter colored bands and without a distinct cleavage. Gneisses are common in the ancient crust of continental shields. Some of the oldest rocks on Earth are gneisses, such as the Acasta Gneiss. Description Orthogneiss from the Czech Republic In traditional English and North American usage, a gneiss is a coarse-grained metamorphic rock showing compositional banding (gneissic banding) but poorly developed schistosity and indistinct cleavage. In other words, it is a metamorphic rock composed of mineral grains easily seen with the unaided eye, which form obvious compositional layers, but which has only a weak tendency to fracture ...
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Comarum Palustre
''Comarum palustre'' ( syn. ''Potentilla palustris''), known by the common names purple marshlocks, swamp cinquefoil and marsh cinquefoil, is a common waterside shrub. It has a circumboreal distribution, occurring throughout North America, Europe, and Asia, particularly the northern regions. It is most commonly found on lake shores, marshy riversides and stream margins, often partly submerged with foliage floating. It is a parent of some ''Fragaria''–''Comarum'' hybrids, ornamental plants produced by crossing with strawberries. Description Its branches spread into leaves with three to seven narrow leaflets which are sharply jagged. The stem is a reddish-brown, low sprawling, vine-like structure. Flowers extend from the branch which vary from red to purple, and are about one inch in diameter, blooming in summer. The stems roots at the base then rises to about .Parnell, J. and Curtis, T. 2012. ''Webb's An Irish Flora.'' Cork University Press. Cultivation Swamp cinquefoil prefers ...
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Lycopodiella Inundata
''Lycopodiella inundata'' is a species of club moss known by the common names inundated club moss, marsh clubmoss and northern bog club moss. It has a circumpolar and circumboreal distribution, occurring throughout the northern Northern Hemisphere from the Arctic to montane temperate regions in Eurasia and North America. It grows in wet habitat, such as bogs, ponds, moist spots on the tundra, and long-standing borrow pits. Description It is a small plant forming patches on the ground, its leafy sterile stems branching and lying horizontal along the ground, rooting at intervals. The sporing cone-bearing stems stand erect in July and August, a few centimeters tall. The leaves are curving, green, narrow, and sharply pointed, measuring a few millimeters long. Distribution and habitat This club moss is an arctic-alpine species with a circumpolar boreal and montane distribution in the Northern Hemisphere. It mostly occurs in Europe, but is also present in East Asia and North America. ...
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Drosera Rotundifolia
''Drosera rotundifolia'', the round-leaved sundew, roundleaf sundew, or common sundew, is a carnivorous species of flowering plant that grows in bogs, marshes and fens. One of the most widespread sundew species, it has a circumboreal distribution, being found in all of northern Europe, much of Siberia, large parts of northern North America, Korea and Japan but is also found as far south as California, Mississippi and Alabama in the United States of America and in New Guinea. Description The leaves of the common sundew are arranged in a basal rosette. The narrow, hairy, long petioles support round laminae. The upper surface of the lamina is densely covered with red glandular hairs that secrete a sticky mucilage. A typical plant has a diameter of around , with a tall inflorescence. The flowers grow on one side of a single slender, hairless stalk that emanates from the centre of the leaf rosette. White or pink in colour, the five-petalled flowers produce , light brown, sl ...
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Drosera Intermedia
''Drosera intermedia'', commonly known as the oblong-leaved sundew, spoonleaf sundew, or spatulate leaved sundew, is an insectivorous plant species belonging to the sundew genus. It is a temperate or tropical species native to Europe, southeastern Canada, the eastern half of the United States, Cuba, Hispaniola, and northern South America. Description ''Drosera intermedia'' is a perennial herb which forms a semi-erect stemless rosette of spatulate leaves up to 10 cm tall. Plants in temperate regions undergo dormancy during which they form a winter resting bud called a hibernaculum. As is typical for sundews, the leaf blades are densely covered with stalked mucilaginous glands which secrete a sugary nectar to attract insects. These then become ensnared by the mucilage and, unless they are strong enough to escape, are suffocated or die from exhaustion. The plant then secretes digestive enzymes from sessile glands and later absorbs the resulting nutrient solution to supplemen ...
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Moorland
Moorland or moor is a type of habitat found in upland areas in temperate grasslands, savannas, and shrublands and montane grasslands and shrublands biomes, characterised by low-growing vegetation on acidic soils. Moorland, nowadays, generally means uncultivated hill land (such as Dartmoor in South West England), but also includes low-lying wetlands (such as Sedgemoor, also South West England). It is closely related to heath, although experts disagree on what precisely distinguishes these types of vegetation. Generally, moor refers to highland and high rainfall zones, whereas heath refers to lowland zones which are more likely to be the result of human activity. Moorland habitats mostly occur in tropical Africa, northern and western Europe, and neotropical South America. Most of the world's moorlands are diverse ecosystems. In the extensive moorlands of the tropics, biodiversity can be extremely high. Moorland also bears a relationship to tundra (where the subsoil is permafros ...
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Beech
Beech (''Fagus'') is a genus of deciduous trees in the family Fagaceae, native to temperate Europe, Asia, and North America. Recent classifications recognize 10 to 13 species in two distinct subgenera, ''Engleriana'' and ''Fagus''. The ''Engleriana'' subgenus is found only in East Asia, distinctive for its low branches, often made up of several major trunks with yellowish bark. The better known ''Fagus'' subgenus beeches are high-branching with tall, stout trunks and smooth silver-grey bark. The European beech (''Fagus sylvatica'') is the most commonly cultivated. Beeches are monoecious, bearing both male and female flowers on the same plant. The small flowers are unisexual, the female flowers borne in pairs, the male flowers wind-pollinating catkins. They are produced in spring shortly after the new leaves appear. The fruit of the beech tree, known as beechnuts or mast, is found in small burrs that drop from the tree in autumn. They are small, roughly triangular, and edible, w ...
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Pinus Mugo
''Pinus mugo'', known as bog pine, creeping pine, dwarf mountain pine, mugo pine, mountain pine, scrub mountain pine, or Swiss mountain pine, is a species of conifer, native to high elevation habitats from southwestern to Central Europe and Southeast Europe. Description The tree has dark green leaves ("needles") in pairs, long. The cones are nut-brown, long. Custura Bucurei.jpg, ''Pinus mugo'' subsp. ''mugo'', Romania Pinus mugo uncinata trees.jpg, ''Pinus mugo'' subsp. ''uncinata'' Swiss National Park 007.JPG, ''Pinus mugo'' subsp. ''rotundata'', Swiss National Park Бор кривул 01.JPG, On Jakupica mountain, Republic of North Macedonia Taxonomy There are three subspecies: *''Pinus mugo'' subsp. ''mugo'' — in the east and south of the range (southern & eastern Alps, Balkan Peninsula), a low, shrubby, often multi-stemmed plant to tall with matte-textured symmetrical cones, which are thin-scaled. *''Pinus mugo'' subsp. ''uncinata'' — in the west and north o ...
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Zone Naturelle D'intérêt écologique, Faunistique Et Floristique
A Zone naturelle d'intérêt écologique, faunistique et floristique (Natural zone of ecological interest, fauna and flora), abbreviated as ZNIEFF, is a type of natural environment recognized by France. The inventory of a ZNIEFF area is an inventory of natural resources and scientific program launched in 1982 by Minister of Environment Huguette Bouchardeau and confirmed by the Act of July 12, 1983 called the Bouchardeau act. A ZNIEFF is not a measure of regulatory protection, but an inventory. It corresponds to the census of outstanding natural land areas in the twenty-two metropolitan areas as well as the overseas departments of France. The designation of a ZNIEFF based primarily on the presence of species or groups of species with strong heritage interest. The presence of at least one population of critical species ( :fr:espèce déterminante in French) defines a ZNIEFF. This is one of the bases for prioritizing natural heritage issues as part of the National Biodiversity Strat ...
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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 ...
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Cenozoic
The Cenozoic ( ; ) is Earth's current geological era, representing the last 66million years of Earth's history. It is characterised by the dominance of mammals, birds and flowering plants, a cooling and drying climate, and the current configuration of continents. It is the latest of three geological eras since complex life evolved, preceded by the Mesozoic and Paleozoic. It started with the Cretaceous–Paleogene extinction event, when many species, including the non-avian dinosaurs, became extinct in an event attributed by most experts to the impact of a large asteroid or other celestial body, the Chicxulub impactor. The Cenozoic is also known as the Age of Mammals because the terrestrial animals that dominated both hemispheres were mammalsthe eutherians (placentals) in the northern hemisphere and the metatherians (marsupials, now mainly restricted to Australia) in the southern hemisphere. The extinction of many groups allowed mammals and birds to greatly diversify so that l ...
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