Den Bommel
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Den Bommel
Den Bommel is a village in the Dutch province of South Holland. It is a part of the municipality of Goeree-Overflakkee, and lies about 14 km south of Spijkenisse. History The village was first mentioned in 1473 as Bommele, and refers to a form of peat. It was originally the name of a shoal which was diked between 1476 and 1477 by order of Mary of Burgundy. Den Bommel became an independent parish in 1642. The Dutch Reformed church is an aisleless church built between 1646 and 1647. The ridge turret was added in 1759. The grist mill De Bommelaer was built in 1735. The windmill had become derelict and started to deteriorate by 1951. Between 1969 and 1971, it was restored and returned to active service. Den Bommel was home to 620 people in 1840. In 1944, the sluice from 1722 was blown up by the Germans causing the destruction of the town hall. Den Bommel was flooded during the North Sea flood of 1953 and was later extended further east. It was an independent municipality until ...
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List Of Sovereign States
The following is a list providing an overview of sovereign states around the world with information on their status and recognition of their sovereignty. The 206 listed states can be divided into three categories based on membership within the United Nations System: 193 UN member states, 2 UN General Assembly non-member observer states, and 11 other states. The ''sovereignty dispute'' column indicates states having undisputed sovereignty (188 states, of which there are 187 UN member states and 1 UN General Assembly non-member observer state), states having disputed sovereignty (16 states, of which there are 6 UN member states, 1 UN General Assembly non-member observer state, and 9 de facto states), and states having a special political status (2 states, both in free association with New Zealand). Compiling a list such as this can be a complicated and controversial process, as there is no definition that is binding on all the members of the community of nations concerni ...
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Mary Of Burgundy
Mary (french: Marie; nl, Maria; 13 February 1457 – 27 March 1482), nicknamed the Rich, was a member of the House of Valois-Burgundy who ruled a collection of states that included the duchies of Limburg, Brabant, Luxembourg, the counties of Namur, Holland, Hainaut and other territories, from 1477 until her death in 1482. As the only child of Charles the Bold, Duke of Burgundy, and his wife Isabella of Bourbon, she inherited the Burgundian lands at the age of 19 upon the death of her father in the Battle of Nancy on 5 January 1477. In order to counter the appetite of the French king Louis XI for her lands, she married Maximilian of Austria. The marriage kept large parts of the Burgundian lands from disintegration, but also changed of the dynasty from the Valois to the Habsburg (the Duchy of Burgundy itself soon became a French possession). This was a turning point in European politics, leading to a French–Habsburg rivalry that would endure for centuries. Early years Mary ...
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Former Municipalities Of South Holland
A former is an object, such as a template, gauge or cutting die, which is used to form something such as a boat's hull. Typically, a former gives shape to a structure that may have complex curvature. A former may become an integral part of the finished structure, as in an aircraft fuselage, or it may be removable, being using in the construction process and then discarded or re-used. Aircraft formers Formers are used in the construction of aircraft fuselage, of which a typical fuselage has a series from the nose to the empennage, typically perpendicular to the longitudinal axis of the aircraft. The primary purpose of formers is to establish the shape of the fuselage and reduce the column length of stringers to prevent instability. Formers are typically attached to longerons, which support the skin of the aircraft. The "former-and-longeron" technique (also called stations and stringers) was adopted from boat construction, and was typical of light aircraft built until the ...
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Olivier B
Olivier is the French form of the given name Oliver. It may refer to: * Olivier (given name), a list of people and fictional characters * Olivier (surname), a list of people * Château Olivier, a Bordeaux winery * Olivier, Louisiana, a rural populated place in the United States * Olivier (crater), on the Moon * Olivier salad, a popular dish of Russian cuisine * ''Olivier'' (novel), the first published novel by French author Claire de Duras * The Olivier Theatre (named after the actor Laurence Olivier), one of three auditoria at the Royal National Theatre * The Laurence Olivier Awards The Laurence Olivier Awards, or simply the Olivier Awards, are presented annually by the Society of London Theatre to recognise excellence in professional theatre in London at an annual ceremony in the capital. The awards were originally known as ..., a theatrical award * Olivier (comics), a foe of The Punisher See also * '' Olivier, Olivier'', a 1992 drama film {{disambiguation ...
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Grog (clay)
Grog, also known as firesand and chamotte, is a raw material usually made from crushed and ground potsherds, reintroduced back into crude clay to temper it before making ceramic ware. It has a high percentage of silica and alumina. It is normally available as a powder or chippings, and is an important ingredient in Coade stone. Production It can be produced by firing selected fire clays to high temperature before grinding and screening to specific particle sizes. Another method makes it from pitchers. The particle size distribution is generally coarser in size than the other raw materials used to prepare clay bodies. It tends to be porous and have low density. Properties Grog is composed of 40% minimum alumina, 30% minimum silica, 4% maximum iron(III) oxide, up to 2% calcium oxide and magnesium oxide combined.. Its melting point is approximately . Its boiling point is over . Its water absorption is maximum 7%. Its thermal expansion coefficient is 5.2 mm/m and thermal ...
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Oostflakkee
Oostflakkee () is a former municipality on the island of Goeree-Overflakkee in the western Netherlands, in the province of South Holland. The former municipality covered an area of about 107 km² (of which about 33 km² was covered by water), and had a population of about 10,000 in 2007. On January 1, 2013, Oostflakkee merged with Goedereede, Dirksland, and Middelharnis into the new municipality of Goeree-Overflakkee. The former municipality of Oostflakkee was formed by the amalgamation of the former municipalities of Den Bommel, Ooltgensplaat, and Oude Tonge in 1966. It consisted of the communities of Achthuizen, Langstraat, Den Bommel (with Zuidzijde), Ooltgensplaat, Oude-Tonge, and Zuidzijde. Oude Tonge was the main town of this former municipality and has a considerable industrial area. It also has a large busstation. Den Bommel is quite similar as Stad aan 't Haringvliet with a harbor and beach on the shores of the Haringvliet. A few kilometers east of Den Bommel ...
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North Sea Flood Of 1953
The 1953 North Sea flood was a major flood caused by a heavy storm surge that struck the Netherlands, north-west Belgium, England and Scotland. Most sea defences facing the surge were overwhelmed, causing extensive flooding. The storm and flooding occurred at the end of Saturday, 31 January 1953 and morning of the next day. A combination of a high spring tide and a severe European windstorm over the North Sea caused a storm tide. The combination of wind, high tide, and low pressure caused the sea to flood land up to above mean sea level. Flooding summary In the Netherlands 20% of the land was below mean sea level (subsequently with the expansion of Flevoland this proportion has increased); the next-highest 30% sat at less than above sea level. Such land relies heavily on sea defences and was worst affected, recording 1,836 deaths and widespread damage. Most of the casualties occurred in the southern province of Zeeland. In England, 307 people were killed in the counties of ...
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Sluice
Sluice ( ) is a word for a channel controlled at its head by a movable gate which is called a sluice gate. A sluice gate is traditionally a wood or metal barrier sliding in grooves that are set in the sides of the waterway and can be considered as a bottom opening in a wall. Sluice gates are one of the most common hydraulic structures in controlling flow rate and water level in open channels such as rivers and canals. They also could be used to measure the flow. A water channel containing a sluice gate forms a type of lock to manage the water flow and water level. It can also be an open channel which processes material, such as a River Sluice used in gold prospecting or fossicking. A mill race, leet, flume, penstock or lade is a sluice channeling water toward a water mill. The terms sluice, sluice gate, knife gate, and slide gate are used interchangeably in the water and wastewater control industry. They are also used in wastewater treatment plants and to recover minerals in minin ...
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Grist Mill
A gristmill (also: grist mill, corn mill, flour mill, feed mill or feedmill) grinds cereal grain into flour and Wheat middlings, middlings. The term can refer to either the Mill (grinding), grinding mechanism or the building that holds it. Grist is grain that has been separated from its chaff in preparation for grinding. History Early history The Greek geographer Strabo reports in his ''Geography'' a water-powered grain-mill to have existed near the palace of king Mithradates VI Eupator at Cabira, Asia Minor, before 71 BC. The early mills had horizontal paddle wheels, an arrangement which later became known as the "Water wheel#Vertical axis, Norse wheel", as many were found in Scandinavia. The paddle wheel was attached to a shaft which was, in turn, attached to the centre of the millstone called the "runner stone". The turning force produced by the water on the paddles was transferred directly to the runner stone, causing it to grind against a stationary "Mill machinery#Wat ...
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Shoal
In oceanography, geomorphology, and geoscience, a shoal is a natural submerged ridge, bank, or bar that consists of, or is covered by, sand or other unconsolidated material and rises from the bed of a body of water to near the surface. It often refers to those submerged ridges, banks, or bars that rise near enough to the surface of a body of water as to constitute a danger to navigation. Shoals are also known as sandbanks, sandbars, or gravelbars. Two or more shoals that are either separated by shared troughs or interconnected by past or present sedimentary and hydrographic processes are referred to as a shoal complex.Neuendorf, K.K.E., J.P. Mehl Jr., and J.A. Jackson, eds. (2005) ''Glossary of Geology'' (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. The term ''shoal'' is also used in a number of ways that can be either similar or quite different from how it is used in geologic, geomorphic, and oceanographic literature. Sometimes, this term refer ...
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Netherlands
) , anthem = ( en, "William of Nassau") , image_map = , map_caption = , subdivision_type = Sovereign state , subdivision_name = Kingdom of the Netherlands , established_title = Before independence , established_date = Spanish Netherlands , established_title2 = Act of Abjuration , established_date2 = 26 July 1581 , established_title3 = Peace of Münster , established_date3 = 30 January 1648 , established_title4 = Kingdom established , established_date4 = 16 March 1815 , established_title5 = Liberation Day (Netherlands), Liberation Day , established_date5 = 5 May 1945 , established_title6 = Charter for the Kingdom of the Netherlands, Kingdom Charter , established_date6 = 15 December 1954 , established_title7 = Dissolution of the Netherlands Antilles, Caribbean reorganisation , established_date7 = 10 October 2010 , official_languages = Dutch language, Dutch , languages_type = Regional languages , languages_sub = yes , languages = , languages2_type = Reco ...
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Peat
Peat (), also known as turf (), is an accumulation of partially decayed vegetation or organic matter. It is unique to natural areas called peatlands, bogs, mires, moors, or muskegs. The peatland ecosystem covers and is the most efficient carbon sink on the planet, because peatland plants capture carbon dioxide (CO2) naturally released from the peat, maintaining an equilibrium. In natural peatlands, the "annual rate of biomass production is greater than the rate of decomposition", but it takes "thousands of years for peatlands to develop the deposits of , which is the average depth of the boreal orthernpeatlands", which store around 415 gigatonnes (Gt) of carbon (about 46 times 2019 global CO2 emissions). Globally, peat stores up to 550 Gt of carbon, 42% of all soil carbon, which exceeds the carbon stored in all other vegetation types, including the world's forests, although it covers just 3% of the land's surface. ''Sphagnum'' moss, also called peat moss, is one of th ...
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