Blast Crater
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Blast Crater
An explosion crater is a type of wikt:crater, crater formed when material is ejected from the surface of the ground by an explosive event at or immediately above or below the surface. A crater is formed by an explosive event through the displacement and ejection of material from the ground. It is typically bowl-shaped. High-pressure gas and shock waves cause three processes responsible for the creation of the crater: * Plastic deformation of the ground. * Projection of material (ejecta) from the ground by the explosion. * Spallation of the ground surface. Two processes partially fill the crater back in: * Fall-back of ejecta. * Erosion and landslides of the crater lip and wall.P. W. Cooper. ''Explosives Engineering''. Wiley-VCH. The relative importance of the five processes varies, depending on the height above or depth below the ground surface at which the explosion occurs and on the composition of the ground. Examples One of the largest explosion craters in Germany is ...
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Sedan Plowshare Crater
Sedan may refer to: Transportation * Sedan (automobile), a type of passenger car * Franklin Sedan, built by H. H. Franklin Manufacturing Company, Syracuse, New York * Prince Sedan, built by Prince Motor Company from 1952 to 1957 * Sero Sedan, an electric microcar marketed by Sero Electric since 2019 * Aeronca Sedan, a light aircraft built by Aeronca Aircraft from 1948 to 1951 * Curtiss-Wright CW-15 Sedan, a 1930s American utility aircraft * Luscombe 11 Sedan, a 1940s American utility aircraft * Sedan station, a railway station in Sedan, Ardennes, France Places France * Arrondissement of Sedan, Ardennes * Principality of Sedan, an independent Protestant state in the Ardennes from 1424 to 1642 * Sedan, Ardennes, a commune United States * Sedan, Indiana, an unincorporated community * Sedan, Iowa, an unincorporated community * Sedan, Kansas, a city * Sedan Township, Chautauqua County, Kansas * Sedan, Michigan, a former community * Sedan, Minnesota, a city * Sedan, Montana, a censu ...
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Crater
Crater may refer to: Landforms *Impact crater, a depression caused by two celestial bodies impacting each other, such as a meteorite hitting a planet *Explosion crater, a hole formed in the ground produced by an explosion near or below the surface **Subsidence crater, a depression from an underground (usually nuclear) explosion *Pit crater, a crater that forms through sinking of the surface and not as a vent for lava *Volcanic crater, a roughly circular depression in the ground caused by volcanic activity **Caldera, a large cauldron-like depression formed following the evacuation of a magma chamber/reservoir **Maar, a type of volcanic crate caused by a phreatic eruption or explosion **Volcanic crater lake, including a list of lakes that formed in a volcanic or impact crater Music * ''Crater'' (Daniel Menche and Mamiffer album), 2016 *Crater (Fission album), 2004 Places *Crati or Crater, a river of southern Italy *Crater, California, U.S. *Crater (Aden), a district of the Aden Gov ...
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Stylised Crater
In the visual arts, style is a "...distinctive manner which permits the grouping of works into related categories" or "...any distinctive, and therefore recognizable, way in which an act is performed or an artifact made or ought to be performed and made". It refers to the visual appearance of a work of art that relates it to other works by the same artist or one from the same period, training, location, "school", art movement or archaeological culture: "The notion of style has long been the art historian's principal mode of classifying works of art. By style he selects and shapes the history of art". Style is often divided into the general style of a period, country or cultural group, group of artists or art movement, and the individual style of the artist within that group style. Divisions within both types of styles are often made, such as between "early", "middle" or "late". In some artists, such as Picasso for example, these divisions may be marked and easy to see; in others ...
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Shock Wave
In physics, a shock wave (also spelled shockwave), or shock, is a type of propagating disturbance that moves faster than the local speed of sound in the medium. Like an ordinary wave, a shock wave carries energy and can propagate through a medium but is characterized by an abrupt, nearly discontinuous, change in pressure, temperature, and density of the medium. For the purpose of comparison, in supersonic flows, additional increased expansion may be achieved through an expansion fan, also known as a Prandtl–Meyer expansion fan. The accompanying expansion wave may approach and eventually collide and recombine with the shock wave, creating a process of destructive interference. The sonic boom associated with the passage of a supersonic aircraft is a type of sound wave produced by constructive interference. Unlike solitons (another kind of nonlinear wave), the energy and speed of a shock wave alone dissipates relatively quickly with distance. When a shock wave passes through ...
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Ejecta
Ejecta (from the Latin: "things thrown out", singular ejectum) are particles ejected from an area. In volcanology, in particular, the term refers to particles including pyroclastic materials (tephra) that came out of a volcanic explosion and magma eruption volcanic vent, or crater, has traveled through the air or under water, and fell back on the ground surface or on the ocean floor. Volcanology Typically in volcanology, ejecta is a result of explosive eruptions. In an explosive eruption, large amounts of gas are dissolved in extremely viscous lava; this lava froths to the surface until the material is expelled rapidly due to the trapped pressure. Sometimes in such an event a lava plug or volcanic neck forms from lava that solidifies inside a volcano's vent, causing heat and pressure to build up to an extreme with no way to escape. When the blockage breaks and cannot sustain itself any longer, a more violent eruption occurs, which allows materials to be ejected out of the volc ...
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Spallation
Spallation is a process in which fragments of material (spall) are ejected from a body due to impact or stress. In the context of impact mechanics it describes ejection of material from a target during impact by a projectile. In planetary physics, spallation describes meteoritic impacts on a planetary surface and the effects of stellar winds and cosmic rays on planetary atmospheres and surfaces. In the context of mining or geology, spallation can refer to pieces of rock breaking off a rock face due to the internal stresses in the rock; it commonly occurs on mine shaft walls. In the context of anthropology, spallation is a process used to make stone tools such as arrowheads by knapping. In nuclear physics, spallation is the process in which a heavy nucleus emits numerous nucleons as a result of being hit by a high-energy particle, thus greatly reducing its atomic weight. In industrial processes and bioprocessing the loss of tubing material due to the repeated flexing of the tu ...
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Prüm
Prüm () is a town in the Westeifel (Rhineland-Palatinate), Germany. Formerly a district capital, today it is the administrative seat of the ''Verbandsgemeinde'' ("collective municipality") Prüm. Geography Prüm lies on the river Prüm (a tributary of the Sauer) at the southeastern end of the Schneifel, which is 697 m high. Prüm is eponymous for the Prüm syncline (Ger. '' Prümer Kalkmulde''), the largest of the Eifel-lime-synclines. Here, the only GSSP-point in Germany identifies the geological border between the lower Devonian Emsian and the middle Devonian Eifelian. History See main article on the town's former monastery, Prüm Abbey. In 2005, the Prüm Convention was signed in the city by several European countries. Ninety-two percent of the town was destroyed by bombing and ground fighting during the Second World War. In 1949, it was wrecked again by an explosion on the Kalvarienberg hill caused by a fire in an underground ammunition bunker. Twelve people were kill ...
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Prüm Explosion
On 15 July 1949 an ammunition depot on the hill of Kalvarienberg in the Eifel mountains exploded. The cause of the explosion, in which the town was heavily damaged and 12 people killed, was never discovered. The crater, which is still visible today, is one of the largest man-made explosion craters in existence. A cross on the Kalvarienberg ('Calvary Hill') commemorates the victims of the disaster. History When the Siegfried Line (in German the ''Westwall'') was built in 1939, a standby bunker was constructed for the Wehrmacht inside the Kalvarienberg. The underground bunker was located 20 to 30 metres below the top of the hill and consisted of a 100-metre-long and a 60-metre-long tunnel. After the Second World War, French troops dumped 500 tons of ammunition there, which was supposed to be used to blow up the fortifications of the Siegfried Line. The population of Prüm knew about this storage and was concerned about it. On 15 July 1949, there was a fire in the bunker. Prüm ...
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Ammunition Depot
An ammunition dump, ammunition supply point (ASP), ammunition handling area (AHA) or ammunition depot is a military storage facility for live ammunition and explosives. The storage of live ammunition and explosives is inherently hazardous. There is the potential for accidents in the unloading, packing, and transfer of ammunition. Great care is taken in handling these dangerous explosives so as not to harm personnel or nearby ammunition. Despite the intensive preventive measures they get, ammunition depots around the world suffer from non-combat fires and explosions. Although this is a rare occurrence, there are devastating consequences when it does happen. Usually, an ammunition depot experiencing even minor explosions in one of its sites/buildings is immediately evacuated together with surrounding civilian areas. Thus, all of the stored ammunition is left to detonate itself completely for days or weeks, with very limited attempts at firefighting from a safe distance.How one c ...
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Hydrothermal Explosion
Hydrothermal explosions occur when superheated water trapped below the surface of the earth rapidly converts from liquid to steam, violently disrupting the confining rock. Boiling water, steam, mud, and rock fragments are ejected over an area of a few meters up to several kilometers in diameter. Although the energy originally comes from a deep igneous source, this energy is transferred to the surface by circulating meteoric water or mixtures of meteoric and magmatic water rather than by magma, as occurs in volcanic eruptions. The energy is stored as heat in hot water and rock within a few hundred feet of the surface. Hydrothermal explosions are caused by the same instability and chain reaction mechanism as geysers but are so violent that rocks and mud are expelled along with water and steam. Cause Hydrothermal explosions occur where shallow interconnected reservoirs of water at temperatures as high as 250° Celsius underlie thermal fields. Water usually boils at 100 °C, but u ...
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Maar
A maar is a broad, low-relief volcanic crater caused by a phreatomagmatic eruption (an explosion which occurs when groundwater comes into contact with hot lava or magma). A maar characteristically fills with water to form a relatively shallow crater lake which may also be called a maar. The name comes from a Moselle Franconian dialect word used for the circular lakes of the Daun area of Germany. Notes: * According to German Wikipedia's ''"Maar"'' article, in 1544 in his book ''Cosmographia'', Sebastian Münster (1488–1552) first applied the word "maar" (as ''Marh'') to the Ulmener Maar and the Laacher See. See: Sebastian Münster, ''Cosmographia'' (Basel, Switzerland: Heinrich Petri, 1544)p. 341. From p. 341: ''"Item zwen namhafftiger seen seind in der Eyfel / einer bey de schloß Ulmen / und ein ander bey dem Closter züm Laich / die seind sere tieff / habe kein ynflüß aber vil außflüß / die nennet man Marh unnd seind fischreich."'' (Also two noteworthy lakes are ...
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Pseudocrater
A rootless cone, also formerly called a pseudocrater, is a volcanic landform which resembles a true volcanic crater, but differs in that it is not an actual vent from which lava has erupted. They are characterised by the absence of any magma conduit which connects below the surface of a planet. Rootless cones are formed by steam explosions as flowing hot lava crosses over a wet surface, such as a swamp, a lake, or a pond. The explosive gases break through the lava surface in a manner similar to a phreatic eruption, and the tephra builds up crater-like forms which can appear very similar to real volcanic craters. Well known examples are found in Iceland such as the craters in the lake Mývatn (''Skútustaðagígar''), the Rauðhólar in the region of the capital city Reykjavík or the ''Landbrotshólar'' of South-Iceland's Katla UNESCO Global Geopark near Kirkjubæjarklaustur. Rootless cones have also been discovered in the Athabasca Valles region of Mars, where lava flows superh ...
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