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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 ...
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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 ...
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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 ...
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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 ...
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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 ...
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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 ...
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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