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Woëvre
The Woëvre () (German: ''Waberland'') is a natural region of Lorraine in northeastern France. It forms part of Lorraine plateau and lies largely in the department of Meuse. Along with the Côtes de Moselle, the Woëvre is one of the areas in Lorraine that receives the least rainfall; nonetheless, its river system is very important and feeds into the Lac de Madine. Location It lies on the right bank of the river Meuse, from the valley of the Chiers in the north to the town of Neufchâteau in the south. To the west, the region follows the Meuse, and to the east, it extends into the neighboring department of Meurthe-et-Moselle. The Lac de Madine lies in the Woëvre, like does the western part of the Parc naturel régional de Lorraine. Neighboring natural regions include the Côtes de Meuse on the left bank of the Meuse, the Barrois to the south and the Côtes de Moselle to the east. The part French, part Belgian Gaume region lies to the north. Features Since the Middle Ages ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Woëvre Localization
The Woëvre () (German: ''Waberland'') is a natural region of Lorraine (region), Lorraine in northeastern France. It forms part of Lorraine plateau and lies largely in the departments of France, department of Meuse (department), Meuse. Along with the Côtes de Moselle, the Woëvre is one of the areas in Lorraine that receives the least rainfall; nonetheless, its river system is very important and feeds into the Lac de Madine. Location It lies on the right bank of the river Meuse, from the valley of the Chiers in the north to the town of Neufchâteau, Vosges, Neufchâteau in the south. To the west, the region follows the Meuse, and to the east, it extends into the neighboring department of Meurthe-et-Moselle. The Lac de Madine lies in the Woëvre, like does the western part of the Parc naturel régional de Lorraine. Neighboring natural regions include the Côtes de Meuse on the left bank of the Meuse, the Barrois to the south and the Côtes de Moselle to the east. The part French ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Woëvre
The Woëvre () (German: ''Waberland'') is a natural region of Lorraine in northeastern France. It forms part of Lorraine plateau and lies largely in the department of Meuse. Along with the Côtes de Moselle, the Woëvre is one of the areas in Lorraine that receives the least rainfall; nonetheless, its river system is very important and feeds into the Lac de Madine. Location It lies on the right bank of the river Meuse, from the valley of the Chiers in the north to the town of Neufchâteau in the south. To the west, the region follows the Meuse, and to the east, it extends into the neighboring department of Meurthe-et-Moselle. The Lac de Madine lies in the Woëvre, like does the western part of the Parc naturel régional de Lorraine. Neighboring natural regions include the Côtes de Meuse on the left bank of the Meuse, the Barrois to the south and the Côtes de Moselle to the east. The part French, part Belgian Gaume region lies to the north. Features Since the Middle Ages ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Parc Naturel Régional De Lorraine
Lorraine Regional Natural Park ( French: ''Parc naturel régional de Lorraine'') is a protected area of pastoral countryside in the Grand Est region of northeastern France, in the historic region of Lorraine. The park covers a total area of . The parkland is split in two non-contiguous parcels of land between the cities of Metz and Nancy, and spans the three departments of Meuse, Meurthe-et-Moselle, and Moselle. According to the World Database on Protected Areas, it is an IUCN category V area. Ancient ruins and modern monuments are common throughout the area. The land was officially designated a regional natural park in 1974. The park is crossed by the LGV Est high speed rail line, with large viaducts. Flora and fauna Animal species found in the park include badger, European wildcat, fox, polecat, roe deer, weasel, wild boar, and wolf, as well as a large variety of birds. Forests are composed of beech and hardwoods such as maple, cherry and whitebeams. Sessile and peduncu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zone Rouge
The ''Zone Rouge'' (English: Red Zone) is a chain of non-contiguous areas throughout northeastern France that the French government isolated after the First World War. The land, which originally covered more than , was deemed too physically and environmentally damaged by conflict for human habitation. Rather than attempt to immediately clean up the former battlefields, the land was allowed to return to nature. Restrictions within the ''Zone Rouge'' still exist today, although the control areas have been greatly reduced. The ''Zone Rouge'' was defined just after the war as "Completely devastated. Damage to properties: 100%. Damage to Agriculture: 100%. Impossible to clean. Human life impossible". Under French law, activities such as housing, farming, or forestry were temporarily or permanently forbidden in the ''Zone Rouge'', because of the vast amounts of human and animal remains, and millions of items of unexploded ordnance contaminating the land. Some towns and villages ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Meuse (department)
Meuse () is a department in northeast France, named after the River Meuse. Meuse is part of the current region of Grand Est and is landlocked and borders by the French departments of Ardennes, Marne, Haute-Marne, Vosges, Meurthe-et-Moselle, and Belgium to the north. Parts of Meuse belong to Parc naturel régional de Lorraine. It had a population of 184,083 in 2019.Populations légales 2019: 55 Meuse INSEE Front lines in during ran varying courses through the department and it hosted an important battle/offensive in 1916 in and aro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Barrois
Barrois () is a (a French territorial division roughly equivalent to a county) in eastern France. In the Middle Ages it was part of the Duchy of Bar, then bordering the Duchy of Lorraine The Duchy of Lorraine (french: Lorraine ; german: Lothringen ), originally Upper Lorraine, was a duchy now included in the larger present-day region of Lorraine in northeastern France. Its capital was Nancy. It was founded in 959 following t .... Today is a of the present-day region of Lorraine. External linksPays Barrois official website(in French) Former provinces of France {{france-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geography Of Grand Est
Geography (from Greek: , ''geographia''. Combination of Greek words ‘Geo’ (The Earth) and ‘Graphien’ (to describe), literally "earth description") is a field of science devoted to the study of the lands, features, inhabitants, and phenomena of Earth. The first recorded use of the word γεωγραφία was as a title of a book by Greek scholar Eratosthenes (276–194 BC). Geography is an all-encompassing discipline that seeks an understanding of Earth and its human and natural complexities—not merely where objects are, but also how they have changed and come to be. While geography is specific to Earth, many concepts can be applied more broadly to other celestial bodies in the field of planetary science. One such concept, the first law of geography, proposed by Waldo Tobler, is "everything is related to everything else, but near things are more related than distant things." Geography has been called "the world discipline" and "the bridge between the human and th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ramsar Site
A Ramsar site is a wetland site designated to be of international importance under the Ramsar Convention,8 ha (O) *** Permanent 8 ha (P) *** Seasonal Intermittent < 8 ha(Ts) ** es on inorganic soils: *** Permanent (herb dominated) (Tp) *** Permanent / Seasonal / Intermittent (shrub dominated)(W) *** Permanent / Seasonal / Intermittent (tree dominated) (Xf) *** Seasonal/intermittent (herb dominated) (Ts) ** Marshes on soils: *** Permanent (non-forested)(U) *** Permanent (forested)(Xp) ** Marshes on inorganic or peat soils: *** Marshes on inorganic or peat soils / High altitude (alpine) (Va) *** Marshes on inorganic or peat soils / Tundra (Vt) * Saline, |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aquifers
An aquifer is an underground layer of water-bearing, permeable rock, rock fractures, or unconsolidated materials (gravel, sand, or silt). Groundwater from aquifers can be extracted using a water well. Aquifers vary greatly in their characteristics. The study of water flow in aquifers and the characterization of aquifers is called hydrogeology. Related terms include aquitard, which is a bed of low permeability along an aquifer, and aquiclude (or ''aquifuge''), which is a solid, impermeable area underlying or overlying an aquifer, the pressure of which could create a confined aquifer. The classification of aquifers is as follows: Saturated versus unsaturated; aquifers versus aquitards; confined versus unconfined; isotropic versus anisotropic; porous, karst, or fractured; transboundary aquifer. Challenges for using groundwater include: overdrafting (extracting groundwater beyond the equilibrium yield of the aquifer), groundwater-related subsidence of land, groundwater becoming sa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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