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Moulin De Rouvres
The Moulin de Rouvres is a historic site in the Rouvres-en-Woëvre commune, in the France, French department of Meuse (department), Meuse. It was first mentioned in the 13th century. Originally part of a farm dating back to Gallic Empire, Gallo-Roman times, it was transformed into an abbey in the 11th century. A pond, which probably predates its construction, provided a dual function for milling and fish farming. Between the 13th and 18th centuries, it became an important watermill and a major source of income for the seigneury of Rouvres-en-Woëvre. However, faced with competition from French coastal fish and industrial gristmills, it was finally dismantled and its pond drained at the end of the 19th century. Initially transformed into a farm, it was located at the heart of the Battle of the Frontiers during World War I, then occupied by the Imperial German Army, German army and transformed into a military camp. Its proximity to the front line during the Battle of Verdun made it ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rouvres-en-Woëvre
Rouvres-en-Woëvre () is a commune in the Meuse department in Grand Est in northeastern France. INSEE See also * Etain-Rouvres Air Base *Communes of the Meuse department
The following is a list of the 499 Communes of France, communes of the Meuse (department), Meuse Departments of France, department of France.
The communes cooperate in the following Communes of France#Intercommunality, intercommunalities (as of ...
* Moulin de Rouvres [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bathonian
In the geologic timescale the Bathonian is an age (geology), age and stage (stratigraphy), stage of the Middle Jurassic. It lasted from approximately 168.2 ±1.2 annum, Ma to around 165.3 ±1.1 Ma (million years ago). The Bathonian Age succeeds the Bajocian Age and precedes the Callovian Age. Stratigraphic definitions The Bathonian Stage takes its name from Bath, Somerset, Bath, a spa town in England built on Jurassic limestone (the Latinized form of the town name is ''Bathonium''). The name was introduced in scientific literature by Belgian geologist Jean Baptiste Julien d'Omalius d'Halloy, d'Omalius d'Halloy in 1843. The original type locality (geology), type locality was located near Bath. The French palaeontologist Alcide d'Orbigny was in 1852 the first to define the exact length of the stage. The base of the Bathonian is at the first appearance of ammonite species ''Parkinsonia (ammonite), Parkinsonia (Gonolkites) convergens'' in the stratigraphic column. The global referen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marl
Marl is an earthy material rich in carbonate minerals, Clay minerals, clays, and silt. When Lithification, hardened into rock, this becomes marlstone. It is formed in marine or freshwater environments, often through the activities of algae. Marl makes up the lower part of the White cliffs of Dover, cliffs of Dover, and the Channel Tunnel follows these marl layers between France and the United Kingdom. Marl is also a common sediment in post-glacial lakes, such as the marl ponds of the northeastern United States. Marl has been used as a soil conditioner and neutralizing agent for acid soil and in the manufacture of cement. Description Marl or marlstone is a carbonate mineral, carbonate-rich mud or mudstone which contains variable amounts of Clay minerals, clays and silt. The term was originally loosely applied to a variety of materials, most of which occur as loose, earthy deposits consisting chiefly of an intimate mixture of clay and calcium carbonate, formed under freshwa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Phreatic Zone
The phreatic zone, saturated zone, or zone of saturation, is the part of an aquifer, below the water table The water table is the upper surface of the phreatic zone or zone of saturation. The zone of saturation is where the pores and fractures of the ground are saturated with groundwater, which may be fresh, saline, or brackish, depending on the loc ..., in which relatively all pores and fractures are saturated with water. The part above the water table is the vadose zone (also called unsaturated zone). The phreatic zone size, color, and depth may fluctuate with changes of season, and during wet and dry periods. Depending on the characteristics of soil particles, their packing and porosity, the boundary of a saturated zone can be stable or instable, exhibiting fingering patterns known as Saffman–Taylor instability. Predicting the onset of stable vs. unstable drainage fronts is of some importance in modelling phreatic zone boundaries. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carte Hydro Bassin Versant
Carte may refer to: People * Alexander Carte (1805–1881), Irish British zoologist * Anto Carte (1886–1954), Belgian painter * Helen Carte (1852–1913), Scottish British businesswoman * Richard Carte (1808–1891), British flute-maker * Samuel Carte (1652–1740), English antiquarian * Thomas Carte (1686–1754), English historian * Omer Carte Qalib (1930–2020), Somalian politician * Carte Goodwin (born 1974), U.S. politician * Carte Said (born 1997), Italian soccer player Other uses * CARTE Museum (Cartographic Acquisition Research Teaching and Exhibition), Baton Rouge, Louisiana, USA * Carte network, a French resistance network See also * Deidre LaCarte, Canadian dancer * Julio Lacarte Muró (1918–2016), Uruguayan diplomat * * Card (other) * Cart (other) * Cartes (other) * Cartesian (other) * Descartes (other), including ''des Cartes'' * D'Oyly Carte (other) * Carte blanche (other) A blank cheque or ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bronze Age
The Bronze Age () was a historical period characterised principally by the use of bronze tools and the development of complex urban societies, as well as the adoption of writing in some areas. The Bronze Age is the middle principal period of the three-age system, following the Stone Age and preceding the Iron Age. Conceived as a global era, the Bronze Age follows the Neolithic, with a transition period between the two known as the Chalcolithic. The final decades of the Bronze Age in the Mediterranean basin are often characterised as a period of widespread societal collapse known as the Late Bronze Age collapse (), although its severity and scope are debated among scholars. An ancient civilisation is deemed to be part of the Bronze Age if it either produced bronze by smelting its own copper and alloying it with tin, arsenic, or other metals, or traded other items for bronze from producing areas elsewhere. Bronze Age cultures were the first to History of writing, develop writin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Middle Ages
In the history of Europe, the Middle Ages or medieval period lasted approximately from the 5th to the late 15th centuries, similarly to the post-classical period of global history. It began with the fall of the Western Roman Empire and transitioned into the Renaissance and the Age of Discovery. The Middle Ages is the middle period of the three traditional divisions of Western history: classical antiquity, the medieval period, and the modern period. The medieval period is itself subdivided into the Early, High, and Late Middle Ages. Population decline, counterurbanisation, the collapse of centralised authority, invasions, and mass migrations of tribes, which had begun in late antiquity, continued into the Early Middle Ages. The large-scale movements of the Migration Period, including various Germanic peoples, formed new kingdoms in what remained of the Western Roman Empire. In the 7th century, North Africa and the Middle East—once part of the Byzantine Empireâ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rhynchonella
''Rhynchonella'' is an extinct genus of brachiopod known from the Late Jurassic ( Oxfordian) to the Early Cretaceous (Valanginian, possibly Barremian). Formerly this genus was understood much more widely (more or less an equivalent of the Rhynchonellida order in the present-day taxonomy) and less critical sources still list species of ''Rhynchonella'' from the Ordovician to the Eocene. Like most brachiopods, ''Rhynchonella'' was a stationary epifaunal suspension feeder Filter feeders are aquatic animals that acquire nutrients by feeding on organic matters, food particles or smaller organisms (bacteria, microalgae and zooplanktons) suspended in water, typically by having the water pass over or through a spec .... Description These 1.75 to 3.75 cm long articulate brachiopods are characterized by a triangular shell with a spherical profile, powerful ribs, a curved hinge line and a small umbo. The anterior margin shows a tongue like projection. Species *'' Rhynchonella ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oolite
Oolite or oölite () is a sedimentary rock formed from ooids, spherical grains composed of concentric layers. Strictly, oolites consist of ooids of diameter 0.25–2 millimetres; rocks composed of ooids larger than 2 mm are called pisolites. The term ''oolith'' can refer to oolite or individual ooids. Composition Ooids are most commonly composed of calcium carbonate (calcite or aragonite), but can be composed of phosphate, clays, chert, dolomite or iron minerals, including hematite. Dolomitic and chert ooids are most likely the result of the replacement of the original texture in limestone. Oolitic hematite occurs at Red Mountain near Birmingham, Alabama, along with oolitic limestone. They are usually formed in warm, supersaturated, shallow, highly agitated marine water intertidal environments, though some are formed in inland lakes. The mechanism of formation starts with a small fragment of sediment acting as a 'seed', such as a piece of a shell. Strong intertidal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone is a type of carbonate rock, carbonate sedimentary rock which is the main source of the material Lime (material), lime. It is composed mostly of the minerals calcite and aragonite, which are different Polymorphism (materials science), crystal forms of calcium carbonate . Limestone forms when these minerals Precipitation (chemistry), 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 (rock), dolomite, a closely related rock, which contains a high percentage of the mineral Dolomite (mine ... [...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 M ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Clay
Clay is a type of fine-grained natural soil material containing clay minerals (hydrous aluminium phyllosilicates, e.g. kaolinite, ). Most pure clay minerals are white or light-coloured, but natural clays show a variety of colours from impurities, such as a reddish or brownish colour from small amounts of iron oxide. Clays develop plasticity (physics), plasticity when wet but can be hardened through Pottery#Firing, firing. Clay is the longest-known ceramic material. Prehistoric humans discovered the useful properties of clay and used it for making pottery. Some of the earliest pottery shards have been radiocarbon dating, dated to around 14,000 BCE, and Clay tablet, clay tablets were the first known writing medium. Clay is used in many modern industrial processes, such as paper making, cement production, and chemical filtration, filtering. Between one-half and two-thirds of the world's population live or work in buildings made with clay, often baked into brick, as an essenti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
