Vottem
Vottem ( wa, Votem) is a village of Wallonia and a district of the municipality of Herstal, located in the province of Liège, Belgium. The Rida river has its springs in Vottem. It was a fully-fledged municipality up to 1976. The Jolivet and Bernalmont hamlets had already been transferred to the town of Liège in 1975. Hamlets and neighbourhoods * Bouxhtay, ''Å Bouh'tè, Å Bouf'tè'', hamlet mentioned since 1278 * Chapeauville, ''A chapêvêye'', neighbourhood mentioned since 1534 * Cheval Blanc, ''Å blanc Dj'vå'', after the "White Horse inn" that was located there * Croix Jouette, ''Creû Djouwète'', hamlet mentioned since 1552 * Gaillard-Cheval, ''Å Galiår'', hamlet mentioned since 1530 * Gascogniers, ''Ås Cascognîs'', hamlet mentioned since 1812 * Haxhes, ''Hå'', ''Håhe'' * Haren, ''Harin'' * Jolivet, ''è Djolivè'' (hamlet mentioned since 1430; transferred to Liège in 1975) * Tiyou, after the Walloon word for the linden that was once growing there. There ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Herstal
Herstal (; wa, Hesta), formerly known as Heristal, or Héristal, is a city and municipality of Wallonia located in the province of Liège, Belgium. It lies along the Meuse river. Herstal is included in the "Greater Liège" agglomeration, which counts about 600,000 inhabitants. The municipality consists of the following districts: Herstal, Liers, Milmort, and Vottem. A large armaments factory, the ''Fabrique Nationale'' or FN, and the biggest industrial zone of Wallonia (Haut-Sart) provide employment locally. History Merovingian and Carolingian golden age The proximity of the river Meuse and the abundance of local resources attracted settlers in this area since the fifth millennium BC. Around the end of the Roman era and at the beginning of the Merovingian period, the hamlet had become a fortified stronghold. The major road that linked Tongeren to Aachen crossed the Meuse here, where a ferry likely carried travelers to Jupille. The name Herstal is of Franconian origin, co ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Chapelle Du Chateau Du Bouxthay 2
Chapelle or La Chapelle may refer to: Communes in France * La Chapelle, Allier * La Chapelle, Ardennes * La Chapelle, Charente * La Chapelle, Savoie * Les Chapelles, Savoie department Other places * Église de la Chapelle or Kapellekerk, a church in Brussels * Quartier de La Chapelle, a neighborhood of Paris, France * La Chapelle (Paris Metro), a metro station in Paris, France * Porte de la Chapelle (Paris Metro), a metro station in Paris, France * Sainte-Chapelle, a Gothic chapel on the Île de la Cité, Paris, France * La Chapelle, Artibonite, a commune in Artibonite department, Haiti * La Chapelle, a commune of Plan-les-Ouates, Switzerland * Chapelle, Glâne, a municipality of the canton of Fribourg, Switzerland * Archbishop Chapelle High School, a high school in New Orleans, United States * Aix-la-Chapelle or Aachen, Germany Other uses * La Chapelle (Church), a Baptist Evangelical multi-site church based in Montreal, Canada. *Chapelle (surname) *Chapelle Jewellery, a br ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Clay With Flint
Clay is a type of fine-grained natural soil material containing clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4). Clays develop plasticity when wet, due to a molecular film of water surrounding the clay particles, but become hard, brittle and non–plastic upon drying or firing. 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. Clay is the oldest 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 dated to around 14,000 BC, and clay tablets were the first known writing medium. Clay is used in many modern industrial processes, such as paper making, cement production, and chemical filtering. Between one-half and two-thirds of the world's population live or work in buildings made with clay, often bak ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Fedasil
Fedasil (''Federal Agency for the Reception of Asylum Seekers'') is a Belgian institution that is responsible for the reception of asylum seekers. The organisation is further responsible for the observation and orientation of unaccompanied minor foreign nationals (UMFNs). The reception of asylum seekers is provided at individual reception locations or collective reception centres. Fedasil operates under the supervision of the State Secretary for Asylum Policy, Migration and Social Integration, Sammy Mahdi. In accordance with the Reception Act of 12 January 2007, the agency provides material assistance: accommodation, food, clothing, medical, social and psychological counselling and access to legal support and certain services (interpreters, training). For those wishing to return to their country of origin either during or after an asylum procedure, Fedasil will provide a programme for voluntary return. Fedasil is also authorised to perform resettlement. Fedasil is led by Mic ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Moulin Bouquette
Moulins or Moulin (French for '' mill'') may refer to: Places France * Diocese of Moulins * Moulins, Allier, in the Allier department (the largest Moulins) * Moulins, Aisne, in the Aisne department * Moulins, Ille-et-Vilaine, in the Ille-et-Vilaine department * Moulins-Engilbert, in the Nièvre department * Moulins-en-Tonnerrois, in the Yonne department * Moulins-la-Marche, in the Orne department * Moulins-le-Carbonnel, in the Sarthe department * Moulins-lès-Metz, in the Moselle department * Moulins-Saint-Hubert, in the Meuse department * Moulins-sur-Céphons, in the Indre department * Moulins-sur-Orne, in the Orne department * Moulins-sur-Ouanne, in the Yonne department * Moulins-sur-Yèvre, in the Cher department * Moulin-Mage, in the Tarn department * Moulin-Neuf, Ariège, in the Ariège department * Moulin-Neuf, Dordogne, in the Dordogne department * Moulin-sous-Touvent, in the Oise department Scotland *Moulin, Scotland, a small settlement just outside Pitlochry, in Perth an ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Temple Antoiniste De Vottem
A temple (from the Latin ) is a building reserved for spiritual rituals and activities such as prayer and sacrifice. Religions which erect temples include Christianity (whose temples are typically called churches), Hinduism (whose temples are called Mandir), Buddhism, Sikhism (whose temples are called gurudwara), Jainism (whose temples are sometimes called derasar), Islam (whose temples are called mosques), Judaism (whose temples are called synagogues), Zoroastrianism (whose temples are sometimes called Agiary), the Baha'i Faith (which are often simply referred to as Baha'i House of Worship), Taoism (which are sometimes called Daoguan), Shinto (which are sometimes called Jinja), Confucianism (which are sometimes called the Temple of Confucius), and ancient religions such as the Ancient Egyptian religion and the Ancient Greek religion. The form and function of temples are thus very variable, though they are often considered by believers to be, in some sense, the "hous ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Germany
Germany,, officially the Federal Republic of Germany, is a country in Central Europe. It is the second most populous country in Europe after Russia, and the most populous member state of the European Union. Germany is situated between the Baltic and North seas to the north, and the Alps to the south; it covers an area of , with a population of almost 84 million within its 16 constituent states. Germany borders Denmark to the north, Poland and the Czech Republic to the east, Austria and Switzerland to the south, and France, Luxembourg, Belgium, and the Netherlands to the west. The nation's capital and most populous city is Berlin and its financial centre is Frankfurt; the largest urban area is the Ruhr. Various Germanic tribes have inhabited the northern parts of modern Germany since classical antiquity. A region named Germania was documented before AD 100. In 962, the Kingdom of Germany formed the bulk of the Holy Roman Empire. During the 16th ce ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Freshwater Tufa
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 term specifically excludes seawater and brackish water, it does include non- salty mineral-rich waters such as chalybeate springs. Fresh water may encompass frozen and meltwater in ice sheets, ice caps, glaciers, snowfields and icebergs, natural precipitations such as rainfall, snowfall, hail/ sleet and graupel, and surface runoffs that form inland bodies of water such as wetlands, ponds, lakes, rivers, streams, as well as groundwater contained in aquifers, subterranean rivers and lakes. Fresh water is the water resource that is of the most and immediate use to humans. Water is critical to the survival of all living organisms. Many organisms can thrive on salt water, but the great majority of higher plants and most insects, amphibians, reptiles, mammals and birds need fresh water to survive. Fresh wat ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Palaeozoic
The Paleozoic (or Palaeozoic) Era is the earliest of three geologic eras of the Phanerozoic Eon. The name ''Paleozoic'' ( ;) was coined by the British geologist Adam Sedgwick in 1838 by combining the Greek words ''palaiós'' (, "old") and ''zōḗ'' (), "life", meaning "ancient life" ). It is the longest of the Phanerozoic eras, lasting from , and is subdivided into six geologic periods (from oldest to youngest): # Cambrian # Ordovician # Silurian # Devonian # Carboniferous # Permian The Paleozoic comes after the Neoproterozoic Era of the Proterozoic Eon and is followed by the Mesozoic Era. The Paleozoic was a time of dramatic geological, climatic, and evolutionary change. The Cambrian witnessed the most rapid and widespread diversification of life in Earth's history, known as the Cambrian explosion, in which most modern phyla first appeared. Arthropods, molluscs, fish, amphibians, reptiles, and synapsids all evolved during the Paleozoic. Life began in the ocean but eve ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Coal
Coal is a combustible black or brownish-black sedimentary rock, formed as rock strata called coal seams. Coal is mostly carbon with variable amounts of other elements, chiefly hydrogen, sulfur, oxygen, and nitrogen. Coal is formed when dead plant matter decays into peat and is converted into coal by the heat and pressure of deep burial over millions of years. Vast deposits of coal originate in former wetlands called coal forests that covered much of the Earth's tropical land areas during the late Carboniferous ( Pennsylvanian) and Permian times. Many significant coal deposits are younger than this and originate from the Mesozoic and Cenozoic eras. Coal is used primarily as a fuel. While coal has been known and used for thousands of years, its usage was limited until the Industrial Revolution. With the invention of the steam engine, coal consumption increased. In 2020, coal supplied about a quarter of the world's primary energy and over a third of its electricity. Some iron ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Schists
Schist ( ) is a medium-grained metamorphic rock showing pronounced schistosity. This means that the rock is composed of mineral grains easily seen with a low-power hand lens, oriented in such a way that the rock is easily split into thin flakes or plates. This texture reflects a high content of platy minerals, such as micas, talc, chlorite, or graphite. These are often interleaved with more granular minerals, such as feldspar or quartz. Schist typically forms during regional metamorphism accompanying the process of mountain building (orogeny) and usually reflects a medium grade of metamorphism. Schist can form from many different kinds of rocks, including sedimentary rocks such as mudstones and igneous rocks such as tuffs. Schist metamorphosed from mudstone is particularly common and is often very rich in mica (a ''mica schist''). Where the type of the original rock (the protolith) is discernible, the schist is usually given a name reflecting its protolith, such as ''schistose met ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |