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Côte D'Or (escarpment)
The Côte d'Or is a limestone escarpment in Burgundy, France of the same name of the ''department'' which was formed around it. It stretches from Dijon in the north to the river Dheune to the south, overlooking the valley of the Saône to the east. The east-facing slope of the Côte d'Or is home to some of the greatest names of Burgundy wine, such as Gevrey-Chambertin, Clos de Vougeot, Meursault and Montrachet. The northern half, the Côte de Nuits, produces red wine almost exclusively. The Côte de Beaune, around Beaune in the south, produces a mix of white wine and red wine. The Route des Grands Crus (Route Nationale 74) runs along the foot of the ridge and is popular with tourists. Scientists have not yet conclusively determined what factors cause the few small parcels of land on the Côte d'Or to produce superlative wines. Hugh Johnson and Jancis Robinson, ''The World Atlas of Wine 7th ed.'' Octopus Publishing Group, 2013 p. 50. History The area was settled by the Celts, a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fixin Bourgogne Vineyards1
Fixin is a Communes of France, commune in the Côte-d'Or Departments of France, department in the Bourgogne (region), Bourgogne Regions of France, region on the Route des Grands Crus, Grand Crus route in eastern France. The French archaeologist Roland Martin (archaeologist), Roland Martin (1912–1997) died in Fixin. Wine Fixin is one of the wine communes of Côte de Nuits. Administration Population Sights * Fixey Church (built 10th & 12th century) stands in the middle of the vineyards, a masterpiece of Roman architecture. The oratory of St Anthony and the square bell tower date from 902. The eastern and western parts of the nave were rebuilt in the twelfth and thirteenth centuries. The apse was enlarged in 1720. The tower is now covered in glazed tiles. * Church of St Martin (12th century) * The Washhouse (19th century) * Museum and Park Noisot See also * Route des Grands Crus * Côte de Nuits References Communes of Côte-d'Or Côte-d'Or communes articl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Route Des Grands Crus
The Route des Grands Crus (roughly, "road of the great wines") is the name of a tourist route situated in Burgundy, France. The approximately 60-kilometre route runs along the foot of the Côte d'Or escarpment, from Dijon in the north to Santenay in the south. Thus it runs through many of the great appellations of Burgundy wine, hence the name of the route. It takes the visitor through the vineyards of the Côte de Nuits and the Côte de Beaune and the back hills ( Hautes-Côtes) behind and above the wine slopes. It is punctuated by 33 villages or little towns, including Beaune, many of which have picturesque churches. Route From north to south: * Marsannay-la-Côte * Côte de Nuits ** Fixin ** Gevrey-Chambertin ** Morey-Saint-Denis ** Chambolle-Musigny ** Vougeot ** Flagey-Echézeaux ** Vosne-Romanée ** Nuits-Saint-Georges * Côte de Beaune ** Aloxe-Corton ** Savigny-Lès-Beaune ** Beaune ** Pommard ** Volnay ** Meursault See also *French wine *Burgundy wine *Côte d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Massif Central
The (; oc, Massís Central, ; literally ''"Central Massif"'') is a highland region in south-central France, consisting of mountains and plateaus. It covers about 15% of mainland France. Subject to volcanism that has subsided in the last 10,000 years, these central mountains are separated from the Alps by a deep north–south cleft created by the Rhône river and known in French as the ' (literally "Rhône furrow"). The region was a barrier to transport within France until the opening of the A75 motorway, which not only made north–south travel easier, but also opened access to the massif itself. Geography and geology The is an old massif, formed during the Variscan orogeny, consisting mostly of granitic and metamorphic rocks. It was powerfully raised and made to look geologically younger in the eastern section by the uplift of the Alps during the Paleogene period and in the southern section by the uplift of the Pyrenees. The massif thus presents a strongly asymmet ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geology Of The Alps
The Alps form part of a Cenozoic orogenic belt of mountain chains, called the Alpide belt, that stretches through southern Europe and Asia from the Atlantic all the way to the Himalayas. This belt of mountain chains was formed during the Alpine orogeny. A gap in these mountain chains in central Europe separates the Alps from the Carpathians to the east. Orogeny took place continuously and tectonic subsidence has produced the gaps in between. The Alps arose as a result of the collision of the African and Eurasian tectonic plates, in which the Alpine Tethys, which was formerly in between these continents, disappeared. Enormous stress was exerted on sediments of the Alpine Tethys basin and its Mesozoic and early Cenozoic strata were pushed against the stable Eurasian landmass by the northward-moving African landmass. Most of this occurred during the Oligocene and Miocene epochs. The pressure formed great recumbent folds, or ''nappes'', that rose out of what had been the Alp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Graben
In geology, a graben () is a depressed block of the crust of a planet or moon, bordered by parallel normal faults. Etymology ''Graben'' is a loan word from German, meaning 'ditch' or 'trench'. The word was first used in the geologic context by Eduard Suess in 1883. The plural form is either ''graben'' or ''grabens''. Formation A graben is a valley with a distinct escarpment on each side caused by the displacement of a block of land downward. Graben often occur side by side with horsts. Horst and graben structures indicate tensional forces and crustal stretching. Graben are produced from parallel normal faults, where the displacement of the hanging wall is downward, while that of the footwall is upward. The faults typically dip toward the center of the graben from both sides. Horsts are parallel blocks that remain between graben; the bounding faults of a horst typically dip away from the center line of the horst. Single or multiple graben can produce a rift valley. Half-g ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Seine
) , mouth_location = Le Havre/Honfleur , mouth_coordinates = , mouth_elevation = , progression = , river_system = Seine basin , basin_size = , tributaries_left = Yonne, Loing, Eure, Risle , tributaries_right = Ource, Aube, Marne, Oise, Epte The Seine ( , ) is a river in northern France. Its drainage basin is in the Paris Basin (a geological relative lowland) covering most of northern France. It rises at Source-Seine, northwest of Dijon in northeastern France in the Langres plateau, flowing through Paris and into the English Channel at Le Havre (and Honfleur on the left bank). It is navigable by ocean-going vessels as far as Rouen, from the sea. Over 60 percent of its length, as far as Burgundy, is negotiable by large barges and most tour boats, and nearly its whole length is available for recreational boating; excursion boats offer sightseeing tours of the river banks in the capital city, Paris. There are 37 bridges in P ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
English Channel
The English Channel, "The Sleeve"; nrf, la Maunche, "The Sleeve" (Cotentinais) or ( Jèrriais), (Guernésiais), "The Channel"; br, Mor Breizh, "Sea of Brittany"; cy, Môr Udd, "Lord's Sea"; kw, Mor Bretannek, "British Sea"; nl, Het Kanaal, "The Channel"; german: Ärmelkanal, "Sleeve Channel" ( French: ''la Manche;'' also called the British Channel or simply the Channel) is an arm of the Atlantic Ocean that separates Southern England from northern France. It links to the southern part of the North Sea by the Strait of Dover at its northeastern end. It is the busiest shipping area in the world. It is about long and varies in width from at its widest to at its narrowest in the Strait of Dover."English Channel". ''The Columbia Encyclopedia'', 2004. It is the smallest of the shallow seas around the continental shelf of Europe, covering an area of some . The Channel was a key factor in Britain becoming a naval superpower and has been utilised by Britain as a natural def ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pays De Caux
The Pays de Caux (, , literally ''Land of Caux'') is an area in Normandy occupying the greater part of the French ''département'' of Seine Maritime in Normandy. It is a chalk plateau to the north of the Seine Estuary and extending to the cliffs on the English Channel coast; its coastline is known as the Côte d'Albâtre. In the east, it borders on the Pays de Bray where the strata below the chalk show through. Cauchois is a notable dialect of the Norman language. The Pays de Caux is one of the remaining strongholds of the Norman language outside the Cotentin (or Cherbourg) peninsula. The principal communities are Le Havre, Dieppe, Fécamp, Yvetot, and Étretat. Etymology In the Norman language ''caux'' means lime, calcium carbonate. In French, for comparison, the word is ''chaux'' (the French 'ch' being pronounced as an English 'sh'. Example: Caux dialect ''candelle'', English ''candle'', French ''chandelle'' ). The name of the neighbouring ''Pays de Bray'' comes from an Ol ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chalk
Chalk is a soft, white, porous, sedimentary carbonate rock. It is a form of limestone composed of the mineral calcite and originally formed deep under the sea by the compression of microscopic plankton that had settled to the sea floor. Chalk is common throughout Western Europe, where deposits underlie parts of France, and steep cliffs are often seen where they meet the sea in places such as the Dover cliffs on the Kent coast of the English Channel. Chalk is mined for use in industry, such as for quicklime, bricks and builder's putty, and in agriculture, for raising pH in soils with high acidity. It is also used for " blackboard chalk" for writing and drawing on various types of surfaces, although these can also be manufactured from other carbonate-based minerals, or gypsum. Description Chalk is a fine-textured, earthy type of limestone distinguished by its light color, softness, and high porosity. It is composed mostly of tiny fragments of the calcite shells or skeletons ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Drainage Basin
A drainage basin is an area of land where all flowing surface water converges to a single point, such as a river mouth, or flows into another body of water, such as a lake or ocean. A basin is separated from adjacent basins by a perimeter, the '' drainage divide'', made up of a succession of elevated features, such as ridges and hills. A basin may consist of smaller basins that merge at river confluences, forming a hierarchical pattern. Other terms for a drainage basin are catchment area, catchment basin, drainage area, river basin, water basin, and impluvium. In North America, they are commonly called a watershed, though in other English-speaking places, "watershed" is used only in its original sense, that of a drainage divide. In a closed drainage basin, or endorheic basin, the water converges to a single point inside the basin, known as a sink, which may be a permanent lake, a dry lake, or a point where surface water is lost underground. Drainage basins are similar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geology
Geology () is a branch of natural science concerned with Earth and other astronomical objects, the features or rocks of which it is composed, and the processes by which they change over time. Modern geology significantly overlaps all other Earth sciences, including hydrology, and so is treated as one major aspect of integrated Earth system science and planetary science. Geology describes the structure of the Earth on and beneath its surface, and the processes that have shaped that structure. It also provides tools to determine the relative and absolute ages of rocks found in a given location, and also to describe the histories of those rocks. By combining these tools, geologists are able to chronicle the geological history of the Earth as a whole, and also to demonstrate the age of the Earth. Geology provides the primary evidence for plate tectonics, the evolutionary history of life, and the Earth's past climates. Geologists broadly study the properties and processes of E ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hydrology
Hydrology () is the scientific study of the movement, distribution, and management of water on Earth and other planets, including the water cycle, water resources, and environmental watershed sustainability. A practitioner of hydrology is called a hydrologist. Hydrologists are scientists studying earth or environmental science, civil or environmental engineering, and physical geography. Using various analytical methods and scientific techniques, they collect and analyze data to help solve water related problems such as environmental preservation, natural disasters, and water management. Hydrology subdivides into surface water hydrology, groundwater hydrology (hydrogeology), and marine hydrology. Domains of hydrology include hydrometeorology, surface hydrology, hydrogeology, drainage-basin management, and water quality, where water plays the central role. Oceanography and meteorology are not included because water is only one of many important aspects within those fields. H ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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