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Bèze (river)
The Bèze () is a French river in the Côte-d'Or department, in the Bourgogne-Franche-Comté region. It is a right tributary of the Saône, and thus a sub-tributary of the Rhône. The river rises in the Crétanne cave in the village of Bèze, then crosses several communes in its course before entering the Saône in Vonges. Its source is the outlet of a vast underground network fed by the Tille and the Venelle. A walk has been laid out around the spring, which is a major tourist attraction in the region. The watershed of the Bèze river and its main tributary, the Albane, irrigates the Saône Vingeanne country, over a total area of Along its course the landscape alternates between forested areas and areas of large crops, livestock meadows and ponds. The basin is home to four natural areas of interest for their ecology, fauna and flora. Human occupation along the river began as early as the Paleolithic. In Roman Gaul the sanctuary of Mirebeau-sur-Bèze, on an important axi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bèze
Bèze () is a commune in the Côte-d'Or department Department may refer to: * Departmentalization, division of a larger organization into parts with specific responsibility Government and military *Department (administrative division), a geographical and administrative division within a country, ... in eastern France. It takes its name from the Bèze river, which rises in the commune. Population See also * Communes of the Côte-d'Or department References External links Official website Communes of Côte-d'Or Côte-d'Or communes articles needing translation from French Wikipedia {{CôteOr-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Poudrerie Nationale De Vonges
The Poudrerie nationale de Vonges (Vonges National Powder Mill) is a French powder mill established in 1691 in Vonges, Côte-d'Or. It manufactured explosives for use in quarries, mines and fireworks. During World War I (1914–18) it manufactured munitions. It expanded after the war, producing explosives for civil use. During World War II (1939–45) production was scaled back drastically, but expanded again after the war. The powder mill was fully privatized in 2008. Location and facilities The powder mill is located in the communes of Vonges and Pontailler-sur-Saône, east of Dijon in the department of the Côte d'Or. The site is bounded by the Bèze and Saône rivers. Etienne Berthelot de Planeuf, Commissary General of Powders and Saltpeter, leased the site beside the Bèze river on 20 February 1691 to build two powder mills, a powder grinder, a winter dryer, a powder magazine and a small refinery. The five year leases were renewed until July 1753, when the site was purchas ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oxfordian (stage)
The Oxfordian is, in the ICS' geologic timescale, the earliest age of the Late Jurassic Epoch, or the lowest stage of the Upper Jurassic Series. It spans the time between 163.5 ± 1.0 Ma and 157.3 ± 1.0 Ma (million years ago). The Oxfordian is preceded by the Callovian and is followed by the Kimmeridgian. Stratigraphic definitions The Oxfordian Stage was called "Clunch Clay and Shale" by William Smith (1815–1816); in 1818 W. Buckland described them under the unwieldy title "Oxford, Forest or Fen Clay". The term Oxfordian was introduced by Alcide d'Orbigny in 1844. The name is derived from the English city of Oxford, where the beds are well developed, but they crop out almost continuously from Dorset to the coast of Yorkshire, generally forming low, broad valleys. They are well exposed at Weymouth, Oxford, Bedford, Peterborough, and in the cliffs at Scarborough, Red Cliff and Gristhorpe Bay. Rocks of this age are found also in Uig and Skye. The base of the Oxfordian ... [...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 lime ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Beze River Entrance Of The Cave
Theodore Beza ( la, Theodorus Beza; french: Théodore de Bèze or ''de Besze''; June 24, 1519 – October 13, 1605) was a French Calvinist Protestant theologian, reformer and scholar who played an important role in the Protestant Reformation. He was a disciple of John Calvin and lived most of his life in Geneva. Beza succeeded Calvin as a spiritual leader of the Republic of Geneva, which was originally founded by John Calvin himself. Biography Early life Theodore Beza was born at Vézelay, in Burgundy, France. His father, Pierre de Beze, royal governor of Vézelay, descended from a Burgundian family of distinction; his mother, Marie Bourdelot, was known for her generosity. Beza's father had two brothers; Nicholas, who was member of Parliament at Paris; and Claude, who was abbot of the Cistercian monastery of Froimont in the diocese of Beauvais. Nicholas, who was unmarried, during a visit to Vézelay was so pleased with Theodore that, with the permission of his parents, he ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bèze River Spring In Bèze 3
Bèze () is a commune in the Côte-d'Or department in eastern France. It takes its name from the Bèze river, which rises in the commune. Population See also *Communes of the Côte-d'Or department The following is a list of the 698 communes of the Côte-d'Or department of France. The communes cooperate in the following intercommunalities (as of 2020):Official website Communes of Côte-d'Or Côte-d'Or communes articles needing translation from French Wikipedia {{Côte ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sump (cave)
A sump, or siphon, is a passage in a cave that is submerged under water. A sump may be static, with no inward or outward flow, or active, with continuous through-flow. Static sumps may also be connected underwater to active stream passage. When short in length, a sump may be called a duck, however this can also refer to a section or passage with some (minimal) airspace above the water. Depending on hydrological factors specific to a cave – such as the sea tide, changes in river A river is a natural flowing watercourse, usually freshwater Fresh water or freshwater is any naturally occurring liquid or frozen water containing low concentrations of dissolved salts and other total dissolved solids. Although the ... flow, or the relationship with the local water table – sumps and ducks may fluctuate in water level and depth (and sometimes in length, due to the shape of adjacent passage). Exploration past a sump Diving Short sumps may be passed simply by hold ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fontaine De Vaucluse (spring)
The Fontaine de Vaucluse () is a karst spring in the commune of Fontaine-de-Vaucluse, France. It is the largest karst spring in metropolitan France by flow and fifth largest in the world, with annual output of of water. The spring is the prime example in hydrogeology of a "Vaucluse spring". It is the source of the Sorgue. Geography Location The Fontaine de Vaucluse is in the commune of Fontaine-de-Vaucluse in the department of Vaucluse. The commune was formerly called "Vaucluse", but being in a department with the same name caused confusion, so the commune was renamed "Fontaine-de-Vaucluse", after the spring. Origin of the name The village in which the spring is located was called "''Vallis Clausa''" ("closed valley") in Latin because of its topographical position. This in time became "Vaucluse", from which the spring takes its name. The name in the Provençal dialect is "Fònt de Vauclusa", the spring of the closed valley. The word ''font'' has two meanings in Provençal, " ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karst Spring
A karst spring or karstic spring is a spring (outflow of groundwater) that is part of a karst hydrological system. Description Because of their often conical or inverted bowl shape, karst springs are also known in German-speaking lands as a ''Topf'' ("pot") which is reflected in names such as Aachtopf (the source of the Radolfzeller Aach) or Blautopf (the source of the Blau river in Blaubeuren). Karst springs often have a very high yield or discharge rate, because they are often fed by underground drainage from a large catchment basin. Because the springs are usually the terminus of a cave drainage system at the place where a river cave reaches the Earth's surface, it is often possible to enter the caves from karst springs for exploration. Large karst springs are located in many parts of the world; the largest ones are believed to be in Papua New Guinea, with others located in Mediterranean countries such as Bosnia and Herzegovina, Croatia, Turkey, Slovenia, and Italy. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kimmeridgian
In the geologic timescale, the Kimmeridgian is an age in the Late Jurassic Epoch and a stage in the Upper Jurassic Series. It spans the time between 157.3 ± 1.0 Ma and 152.1 ± 0.9 Ma (million years ago). The Kimmeridgian follows the Oxfordian and precedes the Tithonian. Stratigraphic definition The Kimmeridgian Stage takes its name from the village of Kimmeridge on the Dorset coast, England. The name was introduced into the literature by French geologist Alcide d'Orbigny in 1842. The Kimmeridge Clay Formation takes its name from the same type location (although this formation extends from the Kimmeridgian stage of the Upper Jurassic into the Lower Cretaceous). It is the source for about 95% of the petroleum in the North Sea. Historically, the term Kimmeridgian has been used in two different ways. The base of the interval is the same but the top was defined by British stratigraphers as the base of the Portlandian (''sensu anglico'') whereas in France the top was defined ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dijon
Dijon (, , ) (dated) * it, Digione * la, Diviō or * lmo, Digion is the prefecture of the Côte-d'Or department and of the Bourgogne-Franche-Comté region in northeastern France. the commune had a population of 156,920. The earliest archaeological finds within the city limits of Dijon date to the Neolithic period. Dijon later became a Roman settlement named ''Divio'', located on the road between Lyon and Paris. The province was home to the Dukes of Burgundy from the early 11th until the late 15th centuries, and Dijon became a place of tremendous wealth and power, one of the great European centres of art, learning, and science. The city has retained varied architectural styles from many of the main periods of the past millennium, including Capetian, Gothic, and Renaissance. Many still-inhabited town-houses in the city's central district date from the 18th century and earlier. Dijon's architecture is distinguished by, among other things, '' toits bourguignon ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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