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";s:4:"text";s:30774:"WebPersistent non-explosive passive degassing is a common characteristic of active volcanoes. WebOne of the defining characteristics of andesite is its overall lack of quartz. Interestingly, andesite has been found throughout Earth's solar system. This most commonly occurs in volcanic arcs associated with subduction zones but also occurs in hot spots and other settings. Aside from its uses in road construction, andesite also represents a useful material in the landscape industry, where it can be shaped into pavers and gravel used to create pathways and other forms of hardscaping. It continues to the surface where it eventually erupts, forming andesite. Basalt: Identification, Pictures & Info for Rockhounds, Dacite: Identification, Pictures, & Info for Rockhounds. Phenocrysts of pyroxene or hornblende are also common. Heather has taught high school and college science courses, and has a master's degree in geography-climatology. Examples of igneous rock are basalt, granite, and andesite (Fig. The rock is majorly formed after the eruption of volcanic magma and crystallization. To study the mechanical and deformation characteristics of ballastless track subgrade filled with micro-expansion fillers in a water-immersed environment, a physical Subduction zones are often associated with a variety of geological features such as island arcs, tectonically active mountain ranges, and volcanoes. Andesite Flow: One of numerous massive andesite flows from the Zarembo Island area of southeastern Alaska. This texture is known as aphanitic and it occurs when magma cools rapidly, preventing crystals from having enough time to grow before becoming completely solidified. Due to its strength and durability, andesite is commonly used in the production of road and exterior construction materials, sculptures, and kitchen countertops. The composition of all igneous rocks is based on the degree of melting and remelting of the Earth's crust. The presence of phenocrysts, in conjunction with its fine-grained texture, makes andesite a type of porphyritic rock. This texture describes large, visible crystals surrounded by a fine-grained groundmass. You also have the option to opt-out of these cookies. They have some uses in the construction industry, but generally are a very average rock. This website uses cookies to improve your experience while you navigate through the website. WebAndesite, containing phenocrysts of plagioclase, clinopyroxene and olivine, was dredged from the Meander Reef on the Cagayan Ridge (Kudrass et al., 1986 ). this note is legal tender. Magmas in these reservoirs become evolved in composition (dacitic to rhyolitic) through both the process of fractional crystallization and partial melting of the surrounding country rock. While all andesites are aphanitic, it is also possible (and even common) to describe their texture in other ways. The best way to learn about rocks is to have specimens available for testing and examination. Water vapor produced when hydrous minerals dehydrate in the heat of a subduction zone. Mafic rocks are formed from extremely hot magma that has reached the Earth's surface and are rich in iron and magnesium, making these rocks darker in color. Magma is Earth's most powerful solvent. | Formula, Structure, & Uses, Bowen's Reaction Series | Magmatic Differentiation & Crystallization of Magma, Comparing Silicate & Non-silicate Minerals. On its way to the surface, the melt stalls and cools, enabling the fractional crystallization of silica-poor minerals. The water and initial slab melts rise into the mantle wedge, prompting melting of the peridotite to produce a basaltic melt. of great consequence. Webcharacteristics noun plural of characteristic as in qualities something that sets apart an individual from others of the same kind the ability to fashion tools and other characteristics that distinguish human beings from other animals Synonyms & Similar Words Relevance qualities traits attributes features attributions properties criteria hallmarks Andesite is intermediate in composition, meaning it is somewhere between basaltic and granitic magma. This partial melting causes the basaltic magma to work its way up through the granitic continental crust where it melts and mixes with sediments and granitic rock, fundamentally changing the chemistry of the magma. Read this ScienceStruck article to know the facts, origin, formation, and properties of andesite rocks. What type of rock is andesitic? %PDF-1.4 If it is under 40% and over 10% then your rock is intermediate, which helps you rule out basalt and rhyolite as possibilities. <> Be notified when an answer is posted. However, it is lighter in color than basalt. Besides this mountain range, the Cordillera mountain range of North and Central America houses these rocks too. This category only includes cookies that ensures basic functionalities and security features of the website. courageous. When observing and identifying a rock like andesite it can often be useful to use a hand lens like this one from Amazon. Wiki User. If you examine a rock that appears to be andesite, but you are not confident that it meets the mineralogical or chemical classification of andesite, you might properly call it an "andesitoid" rock. Basalt thus formed can contribute to the formation of andesite through fractional crystallization, partial melting of crust, or magma mixing, all of which are discussed next. 254 lessons. They usually appear black, green or even brown. The partial melting of the crust leads to the creation of andesitic magma. The study of andesite has helped scientists understand the geological processes by which this igneous rock can be formed. endobj Andesites are typically formed at subduction zones, in which one tectonic plate slides beneath a second plate. Chances are good that you have seen and touched andesite many times in your life, whether or not you were aware of it at the time. Andesite is an extrusive igneous rock that has a porphyritic texture. They behave in a similar manner to a flows but their more viscous nature causes the surface to be covered in smooth-sided angular fragments (blocks) of solidified lava instead of clinkers. Andesite consists of plagioclase feldspar along with pyroxene. Several samples of Martian soil and crust have been shown to contain andesite, which being a volcanic rock, should only be found in locations that have active or dormant volcanoes. For casual purposes, assigning an identification by visually estimating the percentages of minerals based on overall color is almost always sufficient. As such, andesite uses are varied and include: For example, the durability of andesite makes it particularly useful in the bedding used as the foundation for many road projects including highways, bridges, and overpasses. WebThe basaltic andesite consists of plagioclase (20 %-35 %), augite (2 %-12 %), hypersthene (2 %-5 %), opaque (1 %-3 %) and groundmass (47 %-72 %). Andesite is usually porphyritic, containing larger crystals (phenocrysts) of plagioclase formed prior to the extrusion that brought the magma to the surface, embedded in a finer-grained matrix. Introduction to Physical Geology: Help and Review, Igneous Rocks in Geology: Help and Review, Psychological Research & Experimental Design, All Teacher Certification Test Prep Courses, Mineral Types, Properties, and Uses: Help and Review, Earth and Celestial Rocks: Help and Review, Volcanic vs Plutonic Igneous Rocks: Definition and Differences, Bowen's Reaction Series: Crystallization Process & Magmatic Differentiation, Classification of Igneous Rocks: Textures and Composition, Locating Igneous Rocks: The Relationship Between Igneous Rocks & Tectonic Plates, Sedimentary Rocks in Geology: Help and Review, Metamorphic Rocks in Geology: Help and Review, Rock Deformation, Geological Folds & Faults: Help and Review, Weathering, Soil & Erosion: Help and Review, Running Water in Geology: Help and Review, Water Balance in Geology: Help and Review, Geologic Time & Radiometric Dating: Help and Review, Earth's Spheres, Surface & Structure: Help and Review, Plate Tectonics in Geology: Help and Review, Energy Resources in Geology: Help and Review, Renewable & Nonrenewable Resources: Help and Review, Economic Geology & Mineral Resources: Help and Review, Human Impact on the Earth & Environment: Help and Review, Environmental Sustainability in Physical Geology: Help and Review, Environmental Risk Analysis in Physical Geology: Help and Review, Ethics, Politics & the Environment: Help and Review, UExcel Microbiology: Study Guide & Test Prep, High School Biology: Homework Help Resource, Environmental Science 101: Environment and Humanity, Prentice Hall Biology: Online Textbook Help, The Cambrian Explosion: Definition & Timeline, Distribution of Plants & Animals Around the World, Landforms, Climates & Ecosystems of the Earth: Patterns & Characteristics, What is Lichen Planus? This distinctive salt and pepper coloration is derived from the presence of phenocrysts, or clearly visible crystals that are larger in size than the surrounding rock texture. Olivine is also sometimes present in smaller quantities and, while considered a mafic (or ultramafic) mineral, it has a characteristic green color that sometimes gives andesite a greenish tinge. The average composition of the continental crust is andesitic. This contributes to the salt and pepper appearance of this rock type. 28 chapters | This site is devoted to sharing my love of rocks with you. able to face and deal with danger or fear without flinching. An extrusive igneous rock is a rock that was formed at the volcanic surface of the earth. The mineral assembly is typically dominated by plagioclase, with pyroxene and/or hornblende. It has a porphyritic texture. The crust undergoing subduction melts and turns into lava that returns to the Earth's surface via volcanic activity to form andesite and other extrusive igneous rocks. Andesite is a comfortably average igneous rock. This article is part of my rock identification series. Andesite outcrop: Close view of an andesite lava flow at Brokeoff Volcano in California. As with a flows, the molten interior of the flow, which is kept insulated by the solidified blocky surface, advances over the rubble that falls off the flow front. Even small differences in these conditions can have a drastic impact on what andesite looks like. in accordance with New World Encyclopedia standards. Andesite represents an extremely strong and durable type of extrusive igneous rock. endobj Pavlof Volcano - plate tectonics: Simplified plate tectonics cross-section showing how Pavlof Volcano is located in the Aleutian Island chain, above a subduction zone, where basaltic crust of the Pacific Plate is being partially melted at depth. Melting of subducted slab containing sediments. Because of its strength and durability, andesite is used in road construction and in the creation of monuments, statues, and sculptures. In order to study the influence of water content on the mechanical properties of sandstone and evolution of crack propagation, laboratory compression tests and Engineering Discrete Element Method (EDEM) numerical simulation of sandstone under different conditions were carried out by the RMT-150B rock mechanics test system. It occurs when minerals with a higher melt point have time to crystallize in the magma melt before the magma erupts to the surface and the entire melt rapidly crystallizes around them. Any cookies that may not be particularly necessary for the website to function and is used specifically to collect user personal data via analytics, ads, other embedded contents are termed as non-necessary cookies. Other accessory minerals like olivine may also be present in small quantities. Andesite vents tend to build up composite volcanoes rather than the shield volcanoes characteristic of basalt, with its much lower viscosity resulting from its lower silica content and higher eruption temperature. Andesite that is not porphyritic may often be described as equigranular, which means that all of the crystals are approximately the same size. At times, magma crystallizes into rocks and certain minerals get removed from the rock once the process of crystallization is over. The darker varieties of these rocks are sometimes mistaken as basalt rocks. In the field, weathered specimens must be broken to properly see their color and their mineral composition. This produces the characteristic basalt-andesite-rhyolite association of island arcs, with andesite the most distinctive rock type. Joanna holds a PhD in Biology from the University of Michigan and is currently working towards a degree in Veterinary Medicine at Michigan State University. This is how you get different morphologies when the andesite finally cools into its solid form. document.getElementById( "ak_js_1" ).setAttribute( "value", ( new Date() ).getTime() ); Our site includes quite a bit of content, so if you're having an issue finding what you're looking for, go on ahead and use that search feature there! It is mandatory to procure user consent prior to running these cookies on your website. [20], Partially molten basalt in the mantle wedge moves upwards until it reaches the base of the overriding crust. Its magmas aren't highly explosive or highly viscous. These resemble aa in having tops consisting largely of However, because its moderately high silica content, andesite is rarely used in the formation of concrete. The ''salt,'' or light coloration is derived largely from the plagioclase phenocrysts, which are white or light grey in color. These cookies will be stored in your browser only with your consent. Meteorite Classification & Composition | What are Meteorites Made Of? Like most rocks, andesite is very strong in compression. Andesites will often contain phenocrysts, which are mineral crystals that are slightly larger in size than the overall grain size of the rock as a whole. They are chemically intermediate, containing a fairly even mix of dark colored pyroxene and lighter colored silica and plagioclase feldspar. Rapid cooling results in a fine-grained texture with small crystals, while slow cooling creates coarse grained rocks with larger, more visible crystals. Andesite Composition The composition of all igneous rocks is based on the degree Our expert volcanologists and photographers offer unique travel experiences: Typical andesite from the Methana peninsula (Greece). Magma mixing between felsic rhyolitic and mafic. [2] For example, hornblende-phyric andesite indicates that hornblende is the principal accessory mineral within andesite. Intrusive igneous rocks refer to rocks that are formed from magma below the surface of the Earth. Alkali feldspars are also sometimes present at up to 35% of the total feldspar content. Chances are good that you have seen plenty of andesite in your day-to-day life, but it can be easy to miss if youre not paying attention. The best you can do is to first estimate the percentage of dark, mafic minerals in the rock. To cite this article click here for a list of acceptable citing formats.The history of earlier contributions by wikipedians is accessible to researchers here: The history of this article since it was imported to New World Encyclopedia: Note: Some restrictions may apply to use of individual images which are separately licensed. 1 0 obj tic ker-ik-t-ri-stik ka-rik- 1 : a distinguishing trait, quality, or property the characteristics of this breed of dog 2 : the integral part of a common logarithm 3 : the smallest positive integer n which for an operation in a ring or field yields 0 when any element is used n times with the operation characteristic 2 of 2 A rock must meet all of these requirements to be considered andesite: If your rock meets all of those criteria then it is very likely andesite, or at least something very closely related. Crystallization will continue until all of the magma is solidified, leaving behind interlocking crystals with virtually no porosity between them. In New Zealand, it is found in Raglan-Kawhia area, Coromandel Peninsula, Great and Little Barrier Islands, West Auckland, Western Bay of Plenty, Central North Island, and Taranaki. A rock with porphyritic texture has large-grained crystals dispersed in a fine-grained groundmass. To unlock this lesson you must be a Study.com Member. This type of rock is plentiful around volcanoes that line the Pacific Basin. Other examples can be peperino volcanic tuff located at Rome (Italy), or the trass volcanic tuff located at Eifel district (Germany). It was first applied by Christian Leopold von Buch in 1826. WebAndesite is a type of igneous rock that is found in most volcanic regions of the world, especially around volcanoes that line the Pacific Basin. There are many different varieties of andesite, each with its own unique properties and appearance, but all varieties of andesite have quite a bit in common when it comes to their overall look. Its like a teacher waved a magic wand and did the work for me. Andesite: The specimen shown is about two inches (five centimeters) across and has a porphyritic texture. It is useful to know what some closely-related rock types are called and what their mineralogy looks like. Andesite is a gray to black volcanic rock with intermediate silica content, typical for lava domes and stratovolcanoes in subduction zones. Because these lavas cooled rapidly at the surface, they are generally composed of small crystals. The name andesite is derived from a mountain range, the Andes in South America. They result from the formation of lava and thus, belong to the volcanic category of rocks. Skinner, Brian J., Stephen C. Porter, and Jeffrey Park. Geologic Maps: Topographic, Cross-Sectional & Structural, Volcanic vs. Plutonic Igneous Rocks | Formation, Differences & Examples, ILTS Science - Environmental Science (112): Test Practice and Study Guide, ILTS Science - Physics (116): Test Practice and Study Guide, SAT Subject Test Chemistry: Practice and Study Guide, CSET Science Subtest II Earth and Space Sciences (219): Test Prep & Study Guide, ILTS Science - Earth and Space Science (108): Test Practice and Study Guide, UExcel Anatomy & Physiology: Study Guide & Test Prep, DSST Principles of Physical Science: Study Guide & Test Prep, Create an account to start this course today. [5][6][7][8] However, it is often not possible to determine the mineral composition of volcanic rocks, due to their very fine grain size, and andesite is then defined chemically as volcanic rock with a content of 57% to 63% silica and not more than about 6% alkali metal oxides. In addition to South America, andesite can be found worldwide. One of the biggest reasons andesite and similar rocks are so popular as a building material is because it doesnt break down in the rain, ice, and wind as easily as other rocks. These differences are due to subtle variations in mineralogy, the gas content of the lava, and how the lava cooled. By contrast, felsic rocks contain high amounts of silicon, potassium, and sodium, making these rocks lighter in color. Andesite is the name of a family of fine-grained, extrusive igneous rocks that are usually light to dark gray in color. Andesite was named from the Andes Mountains. I would definitely recommend Study.com to my colleagues. If that can of beer is shaken and suddenly depressurized by opening the can, the gas and the beer will erupt from the opening. They may describe the physical body. As with any rock, it is important to take a systematic approach when identifying andesite. Andesite possesses a salt and pepper color and texture due to its mafic and felsic composition, making andesite a chemically intermediate rock. x=k?!tS* ran*C~YKz1?e>]g;/]wV*fw(x,Y^9[/]w~>;;{)LBy?JN*($fqrEbr>R*X86pNU4N~P:XZP,p`LN|M WebAndesite is an exclusive igneous rock that has a light to dark grey color. The phenocryst refers to the larger, conspicuous crystals within the smaller grained groundmass. Andesite is most commonly used for interior and exterior building applications. Rock Cycle Overview & Examples | How Does the Rock Cycle Work? This rock is considered to be the volcanic equivalent of diorite, which is a granular crystalline rock. Pieces of andesite can survive in a river for great distances, which is why you can sometimes find pieces downriver from its source. [33], Along with basalts, andesites are a component of the Martian crust. Andesite represents an extrusive igneous rock. "Andesite porphyry" is the name used for these rocks with two crystal sizes. Geologists categorize rocks into three main types: sedimentary, metamorphic, and igneous. Create your account. It generally occurs in the hues of gray. Andesite is a fine-grained, extrusive igneous or volcanic rock. [14], Block lava flows are typical of andesitic lavas from composite volcanoes. By contrast, the presence of hornblende, augite, and biotite comprise the the ''pepper'' portion of andesite's appearance, as these crystals are usually black or dark green in color. An error occurred trying to load this video. Finally, the medium gray 1995. This website uses cookies to improve your experience. Andesite is usually light to dark gray and often contains larger crystals called phenocrysts. These crystals form because they had a longer time to cool and crystallize. It can be difficult to know exactly what andesite looks like and how to identify it, but it is relatively simple if you know what to look for. Magnetite, zircon, apatite, ilmenite, biotite, and garnet are common accessory minerals. The density of this type of rocks is 2.11 2.36 g/cm. Andesite is an extrusive igneous rock composed primarily of plagioclase feldspar and large amounts of mafic minerals like hornblende. These are known as phenocrysts and are usually made of plagioclase feldspar, hornblende, or pyroxene. Andesite is intermediate in composition between basalt and rhyolite. These particles, known as volcanic ash, can be blown high into the atmosphere and carried long distances by the wind. The term andesite is derived from the Andes mountain range, where specific types of lava were given this name. Discover how andesite is formed and learn what type of rock it is. Andesite usually does not contain olivine. Three general types are recognized: Basaltic magma -- SiO 2 45-55 wt%, high in Fe, Mg, Ca, low in K, Na; Andesitic magma - 800 to 1000 o C; Rhyolitic magma - 650 to 800 o C. Viscosity of Magmas Alkali feldspar may be present in minor amounts. The plagioclase in andesite varies widely in sodium content, from anorthite to oligoclase, but is typically andesine, in which anorthite makes up about 40 mol% of the plagioclase. Andesite can also form away from the subduction zone environment. [16] The presence of convergent margins dominated by andesite is so characteristic of the Earth's unique plate tectonics that the Earth has been described as an "andesite planet". Of course, it is usually impossible to estimate the percentage of quartz in an andesitic rock (if any is present at all) because the crystals are too small to see. Like most rocks, andesite can become very weathered when exposed to the elements. This coincides with the subduction zones at the western boundary of the Pacific Plate. This is largely true in comparison with the other nations of the British Isles and Northern Europeans in general, which see relatively few instances of black hair. Andesitic lava flows slowly when compared to basaltic lava because it has a higher viscosity. Some geologists prefer to classify these tuffs as a variety of andesite, but for our purposes, we will treat them as a separate rock type. It could also be called a "hornblende andesite" because of its composition. These form when certain mineral grains have slightly more time inside the volcano to cool and crystallize before being ejected. Pavlof Volcano is one of the most active volcanoes in Alaska. Some examples of intrusive igneous rocks include granite, diorite, and gabbro. These high-crystallization-temperature minerals begin forming below the surface and grow to visible sizes before the magma erupts. Igneous rock composition chart: This chart shows that andesite is typically composed of plagioclase, amphiboles, and micas; sometimes with minor amounts of pyroxenes, quartz, or orthoclase. Andesite (/ndzat/)[1] is a volcanic rock of intermediate composition. The creation of andesite really begins with oceanic plates, which are basaltic in composition. studied the The slab itself, or the overlying mantle wedge, may melt. 2 0 obj Like many things in geology, andesite is named for where it is found: the Andes Mountains of South America. This type of rock could be called an "andesite porphyry" because of its texture. Characteristic of subduction zones, andesite represents the dominant rock type in island arcs. Andesite is considered an average igneous rock. Models of heat transfer, however, show that arc basalts emplaced at temperatures 11001240C cannot provide enough heat to melt lower crustal amphibolite. Sediment Examples, Types & Features | What is Sediment? They could also describe the psychological makeup or personality of a person. Enrolling in a course lets you earn progress by passing quizzes and exams. One of the defining characteristics of andesite is its overall lack of quartz. These cookies do not store any personal information. An example is the hornblende andesite porphyry shown in the accompanying photo. Andesite is usually light or dark gray, but can also be brown, green, or reddish. It can also form during eruptions at continental plate interiors where deep-source magma melts continental crust or mixes with continental magmas. Basaltic Lava Overview & Characteristics | What is Basaltic Lava? Many volcanic plumes and ash eruptions occur when gas-charged andesitic magmas erupt. Feldspar has much more variety than quartz. The presence of plagioclase phenocrysts is also a great indication that your rock is andesite. Water in the subducted oceanic crust "boils off" from the slab by dehydration of hydrated minerals such as amphibole, zeolites, and chlorite. [20] These mafic minerals settle out of the magma, forming mafic cumulates. The andesite is believed to have originated from the mixing of two separate types of magma, one more like a basalt and the other more rhyolitic in character. As hot basaltic magma is injected upward into the cooler rhyolite magma chamber, it triggers the eruption. The following are common personality characteristics. The gas pressure that causes the eruption blows large amounts of tiny rock and magma particles into the atmosphere. Small amounts of mica will be present as biotite or muscovite. This definition is very specific, but without sophisticated methods for measuring mineral types and percentages it is impractical (or even impossible) for us to determine if an andesite-like rock falls into those specific percentage ranges. Traces of andesite have also been found in meteorites that have struck Earth over the years, which have led researchers to speculate about the role that meteorites have played in the formation of both Earth and Martian crust material. Geologists use this measure to identify rocks and understand their characteristics. In areas where diorite occurs near the surface, it is What type of a rock is andesite?VolcanicIgneousPorphyriticExtrusive WebLavas of andesitic or intermediate composition commonly form a somewhat different type of flow, known as a block lava flow. Andesite has a mineral composition which is intermediate between granite and basalt. In the U.S., andesite is most commonly found in the western states particularly in the Pacific Northwest in association with large stratovolcanoes such as Mount Rainier and Mt. For example, it can form at ocean ridges and oceanic hot spots from partial melting of basaltic rocks. [17], During subduction, the subducted oceanic crust is subjected to increasing pressure and temperature, leading to metamorphism. It means that the rock looks like andesite, but, a microscopic examination or chemical analysis might prove you wrong! The rock derives its name from Andes mountain ranges, which possess a large number of andesite rocks. Besides this, it is used in designing landscapes and gardens. WebDownload Table | Physico-mechanical characteristics of andesite sample. It is also sometimes associated with hot spots and any other geologic environments where basaltic magma mixes with granitic magma. They also move much more slowly downhill and are thicker in depth than a flows. Types of Magma. Slow cooling facilitates the growth of large mineral crystals in the rock. Andesite is a fine-grained extrusive igneous rock, forming when volcanic magmas erupt and crystallize outside of the volcano. In this lesson, the characteristics, formation, and composition of andesite rocks will be further explored. These rocks are formed due to the constant subduction processes that lead to pushing of tectonic plates downward along the continental margins. lessons in math, English, science, history, and more. We focus here on characteristics of long-period events, and their role in the pressurization of the volcanic plumbing system. Classroom specimens usually do not require breakage. The presence of andesite on Mars has been used as evidence of volcanic activity in Mars' geologic past. [10] Alkali feldspar may be present in minor amounts. There are many variations of andesite that can look quite different from one another. This intermediate mixture usually occurs when the two different magma types are mixed together. Ill walk you through identifying andesite, what it looks like, and where it can be found. The pyroxene minerals that may be present include augite, pigeonite, or orthopyroxene. In, "Rock Classification Scheme - Vol 1 - Igneous", "Magmatic differentiation processes at Merapi Volcano: inclusion petrology and oxygen isotopes", "Erratum to: Melting the hydrous, subarc mantle: the origin of primitive andesites", "Early formation of evolved asteroidal crust", "VolcanoIce Interaction as a Microbial Habitat on Earth and Mars", Origins of the Continental Crust, Abstract, Origins of the Continental Crust, Full paper, Experimental and Theoretical Constraints on Peridotite Partial Melting in the Mantle Wedge, https://en.wikipedia.org/w/index.php?title=Andesite&oldid=1116030889, Wikipedia articles needing page number citations from August 2013, Short description is different from Wikidata, Creative Commons Attribution-ShareAlike License 3.0, This page was last edited on 14 October 2022, at 12:40. 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