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Côte D'Or (escarpment)
The Côte d'Or () is a limestone escarpment in Burgundy, France, and the namesake of the department in which it is located. 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 Burgundy wines such as Gevrey-Chambertin, Clos de Vougeot, Meursault and Montrachet. The northern half, the Côte de Nuits, produces red wine almost exclusively. To the south, the Côte de Beaune 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. History The area was settled by the Celts, and there is considerable evidence of Roman occupation in the area. Later it came under the influence of the Dukes of Burgundy, with the Cistercians from Cîteaux Abbey playing a prominent role in the development of the vineyards. Geology If the Paris hydrological and geological basin is vi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fixin Bourgogne Vineyards1
Fixin () is a commune in the Côte-d'Or department in the Bourgogne region on the Grand Crus route in eastern France. The French 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 The Côte de Nuits () is a French wine region located in the northern part of the Côte d'Or (escarpment), Côte d'Or, the limestone ridge that is at the heart of the Burgundy wine region. It exten ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cîteaux Abbey
Cîteaux Abbey ( ) is a Catholic abbey located in Saint-Nicolas-lès-Cîteaux, south of Dijon, France. It is notable for being the original house of the Order of Cistercians. Today, it belongs to the Trappists (also called the Cistercians of the Strict Observance). The abbey has about 35 monks. The community produces a cheese branded under the abbey's name, as well as caramels and honey-based candies. History Cîteaux Abbey was founded on Saint Benedict's Day, 21 March 1098, by a group of monks from Molesme Abbey seeking to follow more closely the Rule of St. Benedict. The Abbey was supported by Renaud, Vicomte de Beaune, and Odo I, Duke of Burgundy. They were led by Saint Robert of Molesme, who became the first abbot. The site was wooded and swampy, in a sparsely populated area. The toponym predates the abbey, but its origin is uncertain. Theories include a derivation from ''cis tertium'' [''lapidem miliarium''], "this side of the third (milliarium, milestone)" of the Roman ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jurassic
The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately 143.1 Mya. The Jurassic constitutes the second and middle period of the Mesozoic, Mesozoic Era as well as the eighth period of the Phanerozoic, Phanerozoic Eon and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic magmatic province, Central Atlantic Magmatic Province (CAMP). The beginning of the Toarcian Age started around 183 million years ago and is marked by the Toarcian Oceanic Anoxic Event, a global episode of Anoxic event, oceanic anoxia, ocean acidification, and elevated global temperatures associated with extinctions, likely caused by the eruption of the Kar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aspect (geography)
In physical geography and physical geology, aspect (also known as exposure) is the compass direction or azimuth that a terrain surface faces. For example, a slope landform on the eastern edge of the Rockies toward the Great Plains is described as having an ''easterly aspect''. A slope which falls down to a deep valley on its western side and a shallower one on its eastern side has a ''westerly aspect'' or is a ''west-facing slope''. The direction a slope faces can affect the physical and biotic features of the slope, known as a slope effect. The term aspect can also be used to describe a related distinct concept: the horizontal alignment of a coastline. Here, the aspect is the direction which the coastline is facing towards the sea. For example, a coastline with sea to the northeast (as in most of Queensland) has a ''northeasterly aspect''. Aspect is complemented by '' grade'' (or inclination angle) to characterize the surface gradient. Importance Aspect can have a str ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Base (chemistry)
In chemistry, there are three definitions in common use of the word "base": '' Arrhenius bases'', '' Brønsted bases'', and '' Lewis bases''. All definitions agree that bases are substances that react with acid An acid is a molecule or ion capable of either donating a proton (i.e. Hydron, hydrogen cation, H+), known as a Brønsted–Lowry acid–base theory, Brønsted–Lowry acid, or forming a covalent bond with an electron pair, known as a Lewis ...s, as originally proposed by Guillaume-François Rouelle, G.-F. Rouelle in the mid-18th century. In 1884, Svante Arrhenius proposed that a base is a substance which dissociates in aqueous solution to form hydroxide ions OH−. These ions can react with Hydron (chemistry), hydrogen ions (H+ according to Arrhenius) from the dissociation of acids to form water in an acid–base reaction. A base was therefore a metal hydroxide such as NaOH or Calcium hydroxide, Ca(OH)2. Such aqueous hydroxide solutions were also described by ... [...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 Alpine ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Graben
In geology, a graben () is a depression (geology), depressed block of the Crust (geology), crust of a planet or moon, bordered by parallel normal faults. Etymology ''Graben'' is a loan word from German language, German, meaning 'ditch' or 'trench'. The first known usage of the word in the geologic context was 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 Horst (geology), horsts. Horst and graben structures indicate tensional forces and crustal stretching. Graben are produced by sets of normal faults that have parallel fault traces, 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 t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Seine
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 (region), Burgundy, is negotiable by large barges and most tour boats, and nearly its whole length is available for recreational boating; Bateaux Mouches, excursion boats offer sightseeing tours of the river banks in the capital city, Paris. There are 37 List of bridges in Paris#Seine, bridges in Paris across the Seine (the most famous of which are the Pont Alexandre III and the Pont Neuf) and dozens List of crossings of the River Seine, more outside the city. A notable bridge, which is also the last along the course of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
English Channel
The English Channel, also known as 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 Sea lane, 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 aided the United Kingdom in becoming a naval superpower, serving as a natural defence against invasions, such as in the Napoleonic Wars and in the World War II, Second World War. The northern, English coast of the Channel is more populous than the southern, French coast. The major languages spoken in this region are English language, English and French language, French. Names Roman historiography, Roman sources as (or , ... [...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'' c ... [...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 colour, softness, and high porosity. It is composed mostly of tiny fragments of the calcite shells or sk ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
