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Dutch Brick
Dutch brick (Dutch: :nl:IJsselsteen, IJsselsteen) is a small type of red brick made in the Netherlands, or similar brick, and an architectural style of building with brick developed by the Dutch people, Dutch. The brick, made from clay dug from river banks or dredged from river beds of the river IJssel and fired over a long period of time, was known for its durability and appearance. Traditional Dutch brick architecture is characterized by rounded or stepped gables. The bricks were imported as ballast into Great Britain and the colonies in the east of America. Trinity College, Dublin, Ireland, founded in 1591, was originally built of red Dutch brick. Dutch brickmakers emigrated to New Netherland in America, where they built kilns for firing bricks locally. Bricks were being burned in New Amsterdam (New York) by 1628, but the imported bricks were of better quality. At first the bricks were used only for chimneys, but they were later used to face the lower story of the house, and ...
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Malacca
Malacca (), officially the Historic State of Malacca (), is a States and federal territories of Malaysia, state in Malaysia located in the Peninsular Malaysia#Other features, southern region of the Malay Peninsula, facing the Strait of Malacca. The state is bordered by Negeri Sembilan to the north and west and Johor to the south. The Enclaves and exclaves, exclave of Tanjung Tuan also borders Negeri Sembilan to the north. Its capital is Malacca City, which has been listed as a UNESCO World Heritage Site since 7 July List of World Heritage Sites by year of inscription#2008 (32nd session), 2008. Malacca has diverse tropical rainforest and experiences an equatorial climate. Situated immediately south of the Titiwangsa Mountains, the state is mostly level and dotted with inselbergs, with Bukit Gapis as the highest point. Although it was the location of one of the earliest Malay sultanates, namely the Malacca Sultanate, the local monarchy was abolished when the Portuguese Capture o ...
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Chaussee
''Chaussee'' is an historic term used in German-speaking countries for early, metalled, rural highways, designed by road engineers, as opposed to the hitherto, traditional, unpaved country roads. The term is no longer used in modern road construction in Western Europe, but survives in road names and is used by historians. In Eastern Europe and the post-Soviet states it remains a generic term for a common paved highway outside of built-up areas, but they may transition into prospekts within towns and cities. Origin of the word and usage The German word was borrowed from the French by the German construction industry in the 18th century. The French word, in turn, went back to the Gallo-Romanic and meant a road surfaced with firmly compacted crushed rock bound with lime. :fr:Chaussée Contemporary German translations of the word were ('road embankment') and ('high way') and even the roughly similar English word, highway. Around 1790, Adelung complained that "several new aut ...
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Zeeland
Zeeland (; ), historically known in English by the Endonym and exonym, exonym Zealand, is the westernmost and least populous province of the Netherlands. The province, located in the southwest of the country, borders North Brabant to the east, South Holland to the north, as well as the country of Belgium to the south and west. It consists of a number of islands and peninsulas (hence its name, meaning "Sealand") and a strip bordering the Flanders, Flemish provinces of East Flanders, East and West Flanders. Its capital is Middelburg, Zeeland, Middelburg with a population of 48,544 as of November 2019, although the largest municipality in Zeeland is Terneuzen (population 54,589). Zeeland has two Port, seaports: Vlissingen and Terneuzen. Its area is , of which is water; it had a population of about 391,000 as of January 2023. Large parts of Zeeland are below sea level. The North Sea flood of 1953, last great flooding of the area was in 1953. Tourism is an important economic activ ...
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Vitrification
Vitrification (, via French ') is the full or partial transformation of a substance into a glass, that is to say, a non- crystalline or amorphous solid. Glasses differ from liquids structurally and glasses possess a higher degree of connectivity with the same Hausdorff dimensionality of bonds as crystals: dimH = 3. In the production of ceramics, vitrification is responsible for their impermeability to water. Vitrification is usually achieved by heating materials until they liquify, then cooling the liquid, often rapidly, so that it passes through the glass transition to form a glassy solid. Certain chemical reactions also result in glasses. In terms of chemistry, vitrification is characteristic for amorphous materials or disordered systems and occurs when bonding between elementary particles (atoms, molecules, forming blocks) becomes higher than a certain threshold value. Thermal fluctuations break the bonds; therefore, the lower the temperature, the higher the ...
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Clinker Brick
Clinker bricks are partially-vitrified bricks used in the construction of buildings. Clinker bricks are produced when wet clay bricks are exposed to excessive heat during the firing process, sintering the surface of the brick and forming a shiny, dark-colored coating.  Clinker bricks have a blackened appearance, and they are often misshapen or split. Clinkers are so named for the metallic sound they make when struck together. Clinker bricks are denser, heavier, and more irregular than standard bricks. Clinkers are water-resistant and durable, but have higher thermal conductivity than more porous red bricks, lending less insulation to climate-controlled structures. The brick-firing kilns of the early 20th century—called brick clamps or "beehive" kilns—did not heat evenly, and the bricks that were too close to the fire emerged harder, darker, and with more vibrant colors, according to the minerals present in the clay. Initially, these clinkers were discarded as defectiv ...
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Charcoal
Charcoal is a lightweight black carbon residue produced by strongly heating wood (or other animal and plant materials) in minimal oxygen to remove all water and volatile constituents. In the traditional version of this pyrolysis process, called charcoal burning, often by forming a charcoal kiln, the heat is supplied by burning part of the starting material itself, with a limited supply of oxygen. The material can also be heated in a closed retort. Modern charcoal briquettes used for outdoor cooking may contain many other additives, e.g. coal. The early history of wood charcoal production spans ancient times, rooted in the abundance of wood in various regions. The process typically involves stacking wood billets to form a conical pile, allowing air to enter through openings at the bottom, and igniting the pile gradually. Charcoal burners, skilled professionals tasked with managing the delicate operation, often lived in isolation to tend their wood piles . Throughout histo ...
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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 Chemical element, elements, chiefly hydrogen, sulfur, oxygen, and nitrogen. Coal is a type of fossil fuel, formed when dead plant matter decays into peat which 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 (geology), Pennsylvanian) and Permian times. 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 generation, electricity. Some iron and steel-maki ...
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Peat
Peat is an accumulation of partially Decomposition, decayed vegetation or organic matter. It is unique to natural areas called peatlands, bogs, mires, Moorland, moors, or muskegs. ''Sphagnum'' moss, also called peat moss, is one of the most common components in peat, although many other plants can contribute. The biological features of sphagnum mosses act to create a habitat aiding peat formation, a phenomenon termed 'habitat manipulation'. Soils consisting primarily of peat are known as histosols. Peat forms in wetland conditions, where flooding or stagnant water obstructs the flow of oxygen from the atmosphere, slowing the rate of decomposition. Peat properties such as organic matter content and saturated hydraulic conductivity can exhibit high spatial heterogeneity. Peatlands, particularly bogs, are the primary source of peat; although less common, other wetlands, including fens, pocosins and peat swamp forests, also deposit peat. Landscapes covered in peat are home to sp ...
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Rhine
The Rhine ( ) is one of the List of rivers of Europe, major rivers in Europe. The river begins in the Swiss canton of Graubünden in the southeastern Swiss Alps. It forms part of the Swiss-Liechtenstein border, then part of the Austria–Switzerland border, Swiss-Austrian border. From Lake Constance downstream, it forms part of the Germany-Switzerland border, Swiss-German border. After that the Rhine defines much of the Franco-German border. It then flows in a mostly northerly direction through the German Rhineland. Finally, the Rhine turns to flow predominantly west to enter the Netherlands, eventually emptying into the North Sea. It drains an area of 185,000 km2. Its name derives from the Gaulish language, Gaulish ''Rēnos''. There are two States of Germany, German states named after the river, North Rhine-Westphalia and Rhineland-Palatinate, in addition to several districts of Germany, districts (e.g. Rhein-Sieg-Kreis, Rhein-Sieg). The departments of France, department ...
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Waal (river)
The Waal ( Dutch name, ) is the main distributary branch of the river Rhine flowing approximately through the Netherlands. It is the major waterway connecting the port of Rotterdam to Germany. Before it reaches Rotterdam, it joins with the Afgedamde Maas near Woudrichem to form the Boven Merwede. Along its length, Nijmegen, Tiel, Zaltbommel and Gorinchem are towns of importance with direct access to the river. The river, which is the main channel in the Rhine–Meuse–Scheldt delta system, carries 65% of the total flow of the Rhine. History The name Waal, in Roman times called ''Vacalis, Vahalis'' or ''Valis'', later ''Vahal'', is of Germanic origin and is named after the many meanders in the river (). It is, in turn, thought to have inspired early Dutch settlers of the Hudson Valley region in New York to name the Wallkill River after it (''Waalkil'' "Waal Creek"). The current river shows little signs of these great bends, since it has been the subject of numero ...
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