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Crystal

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1697: 1628: 1651: 1616: 1663: 68: 1567: 1586: 953: 302: 1696: 2577: 1601: 471: 592: 557:. Galena also sometimes crystallizes as octahedrons, and the eight faces of the octahedron belong to another crystallographic form reflecting a different symmetry of the isometric system. A crystallographic form is described by placing the Miller indices of one of its faces within brackets. For example, the octahedral form is written as {111}, and the other faces in the form are implied by the symmetry of the crystal. 1384: 2048: 1101: 330: 1192: 581: 54: 1650: 560:
Forms may be closed, meaning that the form can completely enclose a volume of space, or open, meaning that it cannot. The cubic and octahedral forms are examples of closed forms. All the forms of the isometric system are closed, while all the forms of the monoclinic and triclinic crystal systems are
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Crystallized sugar. Crystals on the right were grown from a sugar cube, while the left from a single seed crystal taken from the right. Red dye was added to the solution when growing the larger crystal, but, insoluble with the solid sugar, all but small traces were forced to precipitate out as it
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and single-crystal metals. The latter are grown synthetically, for example, fighter-jet turbines are typically made by first growing a single crystal of titanium alloy, increasing its strength and melting point over polycrystalline titanium. A small piece of metal may naturally form into a single
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are often composed of single crystal, or many large crystals that may be several meters in size, due to very slow cooling in the vacuum of space. The slow cooling may allow the precipitation of a separate phase within the crystal lattice, which form at specific angles determined by the lattice,
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crystals consist of a stack of sheets, and although each individual sheet is mechanically very strong, the sheets are rather loosely bound to each other. Therefore, the mechanical strength of the material is quite different depending on the direction of stress.
2771: 618:. Crystals found in rocks typically range in size from a fraction of a millimetre to several centimetres across, although exceptionally large crystals are occasionally found. As of 1999, the world's largest known naturally occurring crystal is a crystal of 1366:
form molecular bonds because the large molecules do not pack as tightly as atomic bonds. This leads to crystals that are much softer and more easily pulled apart or broken. Common examples include chocolates, candles, or viruses. Water ice and
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is a noncrystalline form. Polymorphs, despite having the same atoms, may have very different properties. For example, diamond is the hardest substance known, while graphite is so soft that it is used as a lubricant.
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is constrained by the requirement that the unit cells stack perfectly with no gaps. There are 219 possible crystal symmetries (230 is commonly cited, but this treats chiral equivalents as separate entities), called
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Quasicrystals, first discovered in 1982, are quite rare in practice. Only about 100 solids are known to form quasicrystals, compared to about 400,000 periodic crystals known in 2004. The 2011
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A specimen consisting of a bornite-coated chalcopyrite crystal nestled in a bed of clear quartz crystals and lustrous pyrite crystals. The bornite-coated crystal is up to 1.5 cm across.
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for a crystal—a crystal is scientifically defined by its microscopic atomic arrangement, not its macroscopic shape—but the characteristic macroscopic shape is often present and easy to see.
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typically form when a metal reacts with a non-metal, such as sodium with chlorine. These often form substances called salts, such as sodium chloride (table salt) or potassium nitrate (
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Crystallization is a complex and extensively-studied field, because depending on the conditions, a single fluid can solidify into many different possible forms. It can form a
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materials generally will form crystalline regions, but the lengths of the molecules usually prevent complete crystallization—and sometimes polymers are completely amorphous.
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consists of arrays of atoms that are ordered but not strictly periodic. They have many attributes in common with ordinary crystals, such as displaying a discrete pattern in
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Yoshinori Furukawa, "Ice"; Matti Leppäranta, "Sea Ice"; D.P. Dobhal, "Glacier"; and other articles in Vijay P. Singh, Pratap Singh, and Umesh K. Haritashya, eds.,
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Not all solids are crystals. For example, when liquid water starts freezing, the phase change begins with small ice crystals that grow until they fuse, forming a
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An apatite crystal sits front and center on cherry-red rhodochroite rhombs, purple fluorite cubes, quartz and a dusting of brass-yellow pyrite cubes.
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Crystallization is the process of forming a crystalline structure from a fluid or from materials dissolved in a fluid. (More rarely, crystals may be
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can form six different types of crystals, but only one has the suitable hardness and melting point for candy bars and confections. Polymorphism in
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Crystals are commonly recognized, macroscopically, by their shape, consisting of flat faces with sharp angles. These shape characteristics are not
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are formed from molten magma and the degree of crystallization depends primarily on the conditions under which they solidified. Such rocks as
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often take the shape of cubes, and the six faces of the cube belong to a crystallographic form that displays one of the symmetries of the
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has redefined the term "crystal" to include both ordinary periodic crystals and quasicrystals ("any solid having an essentially discrete
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Quasicrystals are most famous for their ability to show five-fold symmetry, which is impossible for an ordinary periodic crystal (see
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Not all crystals have all of these properties. Conversely, these properties are not quite exclusive to crystals. They can appear in
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Macroscopic (~16 cm) halite crystal. The right-angles between crystal faces are due to the cubic symmetry of the atoms' arrangement
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crystal has every atom in a perfect, exactly repeating pattern. However, in reality, most crystalline materials have a variety of
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open. A crystal's faces may all belong to the same closed form, or they may be a combination of multiple open or closed forms.
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are sets of possible faces of the crystal that are related by one of the symmetries of the crystal. For example, crystals of
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crystal is growing, new atoms can very easily attach to the parts of the surface with rough atomic-scale structure and many
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consists of measuring the three-dimensional orientations of the faces of a crystal, and using them to infer the underlying
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were poured out at the surface and cooled very rapidly, and in this latter group a small amount of amorphous or
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The scientific definition of a "crystal" is based on the microscopic arrangement of atoms inside it, called the
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with specific, characteristic orientations. The scientific study of crystals and crystal formation is known as
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fluid, or by crystallization out of a solution. Some ionic compounds can be very hard, such as oxides like
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have acted on them by erasing their original structures and inducing recrystallization in the solid state.
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of the crystal, i.e. the lack of rotational symmetry in its atomic arrangement. One such property is the
1715: 1288: 1150: 416: 38: 373:" or "grains") is a true crystal with a periodic arrangement of atoms, but the whole polycrystal does 2300: 2180: 1811: 1473: 1212: 1052: 501: 447: 427: 320: 2328: 1547:(in other words, the atomic arrangement) of a crystal. One widely used crystallography technique is 2800: 2760: 2544: 1793: 1684: 1576: 1343: 1160:, meaning that the "wrong" type of atom is present in a crystal. For example, a perfect crystal of 1138: 1021: 952: 520: 2738: 2638: 2475: 1976: 1740: 1517: 1318: 1264: 1071: 1044: 1025: 276: 31: 2411: 1489: 614:
By volume and weight, the largest concentrations of crystals in the Earth are part of its solid
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consists of smaller crystalline units that are somewhat misaligned with respect to each other.
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One or more of the preceding sentences incorporates text from a publication now in the
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crystallize rapidly and are almost always polycrystalline, though there are exceptions like
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Other rock crystals have formed out of precipitation from fluids, commonly water, to form
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gaseous-solution of water vapor and air, when the temperature of the air drops below its
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Nucleation of Water: From Fundamental Science to Atmospheric and Additional Applications
888:(a crystal). Likewise, if a substance can form crystals, it can also form polycrystals. 685:
condition nor entirely in solution, but the high temperature and pressure conditions of
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are common crystalline/polycrystalline structures on Earth and other planets. A single
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How Long Is the Coast of Britain? Statistical Self-Similarity and Fractional Dimension
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Crystals can have certain special electrical, optical, and mechanical properties that
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crystals do not, usually because the crystal is one grain in a polycrystalline solid.
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is the ability of a solid to exist in more than one crystal form. For example, water
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have a periodic arrangement of atoms, because the periodic pattern is broken at the
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A crystal structure (an arrangement of atoms in a crystal) is characterized by its
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by Museum and Galleries Commission -- Museum and Galleries Commission 2005 Page 57
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Angelo State University: Formulas and Nomenclature of Ionic and Covalent Compounds
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and some limestones have been deposited from aqueous solution, mostly owing to
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by Tilman Spohn, Doris Breuer, Torrence V. Johnson -- Elsevier 2014 Page 632
1898: 1725: 1688: 1669: 1298: 1283: 1232: 1095: 913: 892: 825: 789: 777: 765: 741: 701: 678: 670: 666: 382: 206: 88: 1594:: A type of ice crystal (picture taken from a distance of about 5 cm). 1043:
Large single crystals can be created by geological processes. For example,
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structure. In the final block of ice, each of the small crystals (called "
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matter is common. Other crystalline rocks, the metamorphic rocks such as
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in Naica, Mexico. For more details on geological crystal formation, see
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Specific industrial techniques to produce large single crystals (called
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is a similar phenomenon where the same atoms can exist in more than one
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The same group of atoms can often solidify in many different ways.
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is a phenomenon somewhere between a crystallographic defect and a
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crystal are oriented in a specific way relative to the underlying
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In addition, the same atoms may be able to form noncrystalline
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also help hold together certain crystals, such as crystalline
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crystals are those that have obvious, well-formed flat faces.
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This article is about crystalline solids. For other uses, see
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by Ari Laaksonen, Jussi Malila -- Elsevier 2022 Page 239--240
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In general, solids can be held together by various types of
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crystals, but rather types of glass, i.e. amorphous solids.
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Science for Conservators, Volume 3: Adhesives and Coatings
1551:. Large numbers of known crystal structures are stored in 1417:, and the ability to form shapes with smooth, flat faces. 756:, snowflakes, or small ice crystals suspended in the air ( 744:
is a single crystal or a collection of crystals, while an
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faces, where new atoms cannot as easily attach themselves.
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Crystals can also be formed by biological processes, see
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is its visible external shape. This is determined by the
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that extends in all directions. In addition, macroscopic
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The American Heritage Dictionary of the English Language
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to slightly blue. Likewise, the only difference between
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processes, giving origin to large masses of crystalline
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Solid material with highly ordered microscopic structure
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Howard, J. Michael; Darcy Howard (Illustrator) (1998).
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Snow Engineering 2000: Recent Advances and Developments
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are examples of other materials with molecular bonding.
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atoms, but a real crystal might perhaps contain a few
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Halite (table salt, NaCl): Microscopic and macroscopic
30:"Crystalline" redirects here. For the Björk song, see 1468:
normally cannot. These properties are related to the
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Another common type of crystallographic defect is an
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For pure chemical elements, polymorphism is known as
143:. The process of crystal formation via mechanisms of 2783: 2676: 2584: 2482: 2012:. Princeton, N.J.: Van Nostrand. pp. 134–138. 1133:A few examples of crystallographic defects include 263:Crystals, or crystalline solids, are often used in 95:) has no periodic arrangement even microscopically. 2194:Britain), Science Research Council (Great (1972). 83:is composed of many microscopic crystals (called " 2412:"Crystal Lattice Structures:Index by Space Group" 1172:atoms as well. These boron impurities change the 385:solids are polycrystalline, including almost all 466:Crystal faces, shapes and crystallographic forms 430:in three-dimensional space to form the crystal. 2246:International Union of Crystallography (1992). 2105:Libbrecht, Kenneth; Wing, Rachel (2015-09-01). 1395:, which can take on the macroscopic shape of a 1305:crystals can be created by solidification of a 534:One of the oldest techniques in the science of 458:(where the crystals may form hexagons, such as 2460: 1235:is a spread of crystal plane orientations. A 217:. Most inorganic solids are not crystals but 8: 2248:"Report of the Executive Committee for 1991" 1995:, by Victor E. Henrich, P. A. Cox, page 28, 1609:, a metal that easily forms large crystals. 1137:(an empty space where an atom should fit), 780:are able to produce crystals grown from an 37:"Xtal" redirects here. For other uses, see 2467: 2453: 2445: 1676:crystal and oxidized on their surfaces to 838:is ordinarily found in the hexagonal form 2312: 2271: 2036:, London, Natural History Museum, page 58 1063: 283:beliefs and related religious movements. 1954:International Tables for Crystallography 1772:"Chem1 online textbook—States of matter" 1070:crystallization from occurring, such as 924:, giving it a wide range of properties. 2108:The Snowflake: Winter's Frozen Artistry 1894:"Using Crystals and Gemstones in Magic" 1762: 1562: 1350:, as well as the interlayer bonding in 1207:, a special type of impurity, called a 1184:is the type of impurities present in a 1104:Two types of crystallographic defects. 2085:Encyclopedia of Snow, Ice and Glaciers 1873:Pseudoscience: A Critical Encyclopedia 1834:, Henry George Liddell, Robert Scott, 1429:International Union of Crystallography 2433:, Department of Crystallography. 2010 1926:"The Magic of Crystals and Gemstones" 920:is responsible for its ability to be 111:material whose constituents (such as 7: 2032:G. Cressey and I. F. Mercer, (1999) 1446:for the discovery of quasicrystals. 1422:crystallographic restriction theorem 2753:The Chemical Basis of Morphogenesis 2329:"The Nobel Prize in Chemistry 2011" 1993:The surface science of metal oxides 872:. For example, water can also form 205:Examples of large crystals include 1892:Patti Wigington (31 August 2016). 1450:Special properties from anisotropy 1149:, because they help determine the 845:, but can also exist as the cubic 357: 131:are usually identifiable by their 25: 2431:Spanish National Research Council 2356:. Bob's Rock Shop. Archived from 1078:Defects, impurities, and twinning 517:atomic arrangement of the crystal 2575: 2211:Encyclopedia of the Solar System 2132:Hjorth-Hansen, E. (2017-10-19). 2046: 1695: 1661: 1649: 1626: 1614: 1599: 1584: 1565: 1543:is the science of measuring the 1313:found in many gemstones such as 1151:mechanical strength of materials 983:, perhaps with various possible 822:Polymorphism (materials science) 328: 300: 275:, are sometimes associated with 233:. A third category of solids is 2372:Krassmann, Thomas (2005–2008). 287:Crystal structure (microscopic) 1672:crystals partially encased in 1047:crystals in excess of 10  419:, but forming a crystal does. 1: 1038:solvent-based crystallization 903:are two crystalline forms of 629:Some crystals have formed by 440:crystallographic space groups 2314:10.1524/zkri.219.7.391.35643 2177:National Geographic Magazine 2171:Shea, Neil (November 2008). 1963:10.1107/97809553602060000001 1951:Welberry, T. R, ed. (2021), 1838:, on Perseus Digital Library 1822:, on Perseus Digital Library 1791:Ashcroft and Mermin (1976). 1522:stress-induced birefringence 507:The flat faces (also called 196: 174: 75:has atoms in a near-perfect 2376:. Krassmann. Archived from 2374:"The Giant Crystal Project" 2059:Flett, John Smith (1911). " 442:. These are grouped into 7 307:Microscopic structure of a 256:, and related products are 254:lead crystal, crystal glass 2838: 1553:crystallographic databases 1531: 1453: 1402: 1081: 1056: 941: 819: 816:Polymorphism and allotropy 341: 190: 168: 43: 36: 29: 2733:D'Arcy Wentworth Thompson 2573: 2264:10.1107/S0108767392008328 2200:. H.M. Stationery Office. 1327:solids (sometimes called 884:(an amorphous glass) and 760:) more often grow from a 681:and have never been in a 323:in the atoms' arrangement 2173:"Cave of Crystal Giants" 2008:Sinkankas, John (1964). 1440:Nobel Prize in Chemistry 1278:crystal, such as Type 2 1128:crystallographic defects 968:directly from gas; see: 960:in a beet sugar factory. 555:isometric crystal system 456:hexagonal crystal system 46:Crystal (disambiguation) 2070:Encyclopædia Britannica 2010:Mineralogy for amateurs 1836:A Greek-English Lexicon 1820:A Greek-English Lexicon 1486:electrical permittivity 1482:electrical conductivity 1397:pentagonal dodecahedron 1329:covalent network solids 1084:Crystallographic defect 641:. The vast majority of 87:" or "grains"); and an 1871:Regal, Brian. (2009). 1400: 1389:holmium–magnesium–zinc 1289:Widmanstatten patterns 1200: 1119: 1030:hydrothermal synthesis 961: 606: 588: 547:crystallographic forms 487: 356:are an exception, see 202:), "icy cold, frost". 96: 64: 2567:Widmanstätten pattern 2197:Report of the Council 1716:Atomic packing factor 1386: 1354:. Substances such as 1213:Semiconductor devices 1194: 1103: 955: 594: 583: 473: 435:symmetry of a crystal 417:latent heat of fusion 135:, consisting of flat 70: 56: 39:Xtal (disambiguation) 2393:"Teaching Pamphlets" 1875:. Greenwood. p. 51. 1812:Henry George Liddell 1577:grown in earth orbit 1508:that have been made 1474:piezoelectric effect 1344:van der Waals forces 1139:interstitial defects 1053:Cave of the Crystals 999:. Or, it can form a 958:cooling crystallizer 792:in the case of most 772:Organigenic crystals 576:Occurrence in nature 448:cubic crystal system 311:crystal. (Purple is 2801:Mathematics and art 2791:Pattern recognition 2761:Aristid Lindenmayer 2305:2004ZK....219..391S 2299:(7–2004): 391–446. 2287:Steurer W. (2004). 2252:Acta Crystallogr. A 1906:on 15 November 2016 1794:Solid State Physics 1685:Milwaukee Formation 1265:van der Waals bonds 1164:would only contain 1072:antifreeze proteins 1022:Czochralski process 454:shown at right) or 381:. Most macroscopic 71:Microscopically, a 2739:On Growth and Form 2639:Logarithmic spiral 2476:Patterns in nature 2111:. Voyageur Press. 1932:. 14 December 2011 1741:Crystal oscillator 1401: 1319:synthetic sapphire 1201: 1120: 1026:Bridgman technique 962: 716:in arid climates. 622:from Malakialina, 607: 589: 523:of relatively low 488: 460:ordinary water ice 271:, and, along with 267:practices such as 252:Despite the name, 97: 65: 32:Crystalline (song) 2809: 2808: 2766:Benoît Mandelbrot 2666:Self-organization 2602:Natural selection 2592:Pattern formation 2427:"Crystallography" 1997:google books link 1972:978-1-119-95235-0 1881:978-0-313-35507-3 1731:Colloidal crystal 1549:X-ray diffraction 1545:crystal structure 1415:x-ray diffraction 1391:(Ho–Mg–Zn) forms 1325:Covalently bonded 1147:materials science 1116:screw dislocation 1051:are found in the 570:crystal structure 350:crystal structure 344:Crystal structure 180:), meaning both " 162:derives from the 133:geometrical shape 105:crystalline solid 16:(Redirected from 2829: 2617:Sexual selection 2579: 2469: 2462: 2455: 2446: 2441: 2439: 2438: 2422: 2420: 2419: 2407: 2405: 2404: 2388: 2386: 2385: 2368: 2366: 2365: 2340: 2339: 2337: 2336: 2331:. Nobelprize.org 2325: 2319: 2318: 2316: 2284: 2278: 2277: 2275: 2243: 2237: 2231: 2225: 2220: 2214: 2208: 2202: 2201: 2191: 2185: 2184: 2183:on Dec 19, 2017. 2179:. Archived from 2168: 2162: 2156: 2150: 2149: 2129: 2123: 2122: 2102: 2096: 2081: 2075: 2074: 2052: 2050: 2049: 2043: 2037: 2030: 2024: 2023: 2005: 1999: 1990: 1984: 1983: 1948: 1942: 1941: 1939: 1937: 1922: 1916: 1915: 1913: 1911: 1902:. Archived from 1889: 1883: 1869: 1863: 1862: 1860: 1859: 1845: 1839: 1829: 1823: 1805: 1799: 1798: 1788: 1782: 1781: 1779: 1778: 1767: 1699: 1665: 1653: 1630: 1618: 1603: 1588: 1569: 1348:molecular solids 1109:edge dislocation 1092:Crystal twinning 1005:ambient pressure 909:amorphous carbon 782:aqueous solution 540:crystal symmetry 408:amorphous solids 379:grain boundaries 332: 304: 265:pseudoscientific 235:amorphous solids 201: 193: 192: 179: 171: 170: 21: 2837: 2836: 2832: 2831: 2830: 2828: 2827: 2826: 2812: 2811: 2810: 2805: 2779: 2672: 2580: 2571: 2478: 2473: 2436: 2434: 2425: 2417: 2415: 2410: 2402: 2400: 2391: 2383: 2381: 2371: 2363: 2361: 2351: 2348: 2346:Further reading 2343: 2334: 2332: 2327: 2326: 2322: 2286: 2285: 2281: 2245: 2244: 2240: 2232: 2228: 2221: 2217: 2209: 2205: 2193: 2192: 2188: 2170: 2169: 2165: 2157: 2153: 2146: 2131: 2130: 2126: 2119: 2104: 2103: 2099: 2095:, 9789048126415 2082: 2078: 2058: 2047: 2045: 2044: 2040: 2031: 2027: 2020: 2007: 2006: 2002: 1991: 1987: 1973: 1950: 1949: 1945: 1935: 1933: 1924: 1923: 1919: 1909: 1907: 1891: 1890: 1886: 1870: 1866: 1857: 1855: 1847: 1846: 1842: 1830: 1826: 1806: 1802: 1790: 1789: 1785: 1776: 1774: 1770:Stephen Lower. 1769: 1768: 1764: 1760: 1755: 1711: 1704: 1700: 1691: 1666: 1657: 1654: 1645: 1631: 1622: 1619: 1610: 1604: 1595: 1589: 1580: 1570: 1561: 1540:Crystallography 1536: 1534:Crystallography 1530: 1528:Crystallography 1490:Young's modulus 1458: 1452: 1442:was awarded to 1407: 1381: 1311:aluminium oxide 1295:Ionic compounds 1275:amorphous metal 1245: 1174:diamond's color 1135:vacancy defects 1098: 1082:Main articles: 1080: 989:stoichiometries 950: 944:Crystallization 942:Main articles: 940: 938:Crystallization 932:amorphous solid 895:. For example, 879: 850: 843: 828: 820:Main articles: 818: 800:in the case of 798:hydroxylapatite 774: 728:in the form of 722: 612: 578: 566:crystal's habit 536:crystallography 468: 444:crystal systems 366:polycrystalline 346: 340: 339: 338: 337: 336: 333: 325: 324: 319:ion). There is 305: 296: 295: 289: 269:crystal therapy 149:crystallization 141:crystallography 129:single crystals 125:crystal lattice 91:solid (such as 79:arrangement; a 49: 42: 35: 28: 23: 22: 15: 12: 11: 5: 2835: 2833: 2825: 2824: 2814: 2813: 2807: 2806: 2804: 2803: 2798: 2793: 2787: 2785: 2781: 2780: 2778: 2777: 2776: 2775: 2763: 2758: 2757: 2756: 2744: 2743: 2742: 2730: 2728:Wilson Bentley 2725: 2723:Joseph Plateau 2720: 2715: 2710: 2709: 2708: 2696: 2691: 2686: 2680: 2678: 2674: 2673: 2671: 2670: 2669: 2668: 2663: 2661:Plateau's laws 2658: 2656:Fluid dynamics 2653: 2643: 2642: 2641: 2636: 2631: 2621: 2620: 2619: 2614: 2609: 2604: 2594: 2588: 2586: 2582: 2581: 2574: 2572: 2570: 2569: 2564: 2559: 2554: 2549: 2548: 2547: 2542: 2537: 2532: 2522: 2517: 2512: 2507: 2502: 2497: 2492: 2486: 2484: 2480: 2479: 2474: 2472: 2471: 2464: 2457: 2449: 2443: 2442: 2423: 2408: 2389: 2369: 2347: 2344: 2342: 2341: 2320: 2293:Z. Kristallogr 2279: 2258:(6): 922–946. 2238: 2226: 2215: 2203: 2186: 2163: 2151: 2144: 2124: 2117: 2097: 2076: 2065:Chisholm, Hugh 2038: 2025: 2018: 2000: 1985: 1971: 1943: 1917: 1884: 1864: 1840: 1824: 1800: 1783: 1761: 1759: 1756: 1754: 1753: 1748: 1746:Liquid crystal 1743: 1738: 1736:Crystal growth 1733: 1728: 1723: 1718: 1712: 1710: 1707: 1706: 1705: 1701: 1694: 1692: 1667: 1660: 1658: 1655: 1648: 1646: 1642:single crystal 1632: 1625: 1623: 1620: 1613: 1611: 1605: 1598: 1596: 1590: 1583: 1581: 1571: 1564: 1560: 1557: 1532:Main article: 1529: 1526: 1520:—for example, 1456:Crystal optics 1451: 1448: 1403:Main article: 1380: 1377: 1339:respectively. 1261:covalent bonds 1253:metallic bonds 1249:chemical bonds 1244: 1243:Chemical bonds 1241: 1237:mosaic crystal 1227:grain boundary 1205:semiconductors 1199:crystal group. 1079: 1076: 1020:) include the 991:, impurities, 981:single crystal 948:Crystal growth 939: 936: 880:can form both 877: 848: 841: 817: 814: 784:, for example 773: 770: 762:supersaturated 721: 718: 611: 608: 577: 574: 529:surface energy 480:dangling bonds 467: 464: 411:, also called 342:Main article: 334: 327: 326: 321:cubic symmetry 315:ion, green is 306: 299: 298: 297: 293: 292: 291: 290: 288: 285: 153:solidification 145:crystal growth 73:single crystal 26: 24: 14: 13: 10: 9: 6: 4: 3: 2: 2834: 2823: 2820: 2819: 2817: 2802: 2799: 2797: 2794: 2792: 2789: 2788: 2786: 2782: 2774: 2773: 2769: 2768: 2767: 2764: 2762: 2759: 2755: 2754: 2750: 2749: 2748: 2745: 2741: 2740: 2736: 2735: 2734: 2731: 2729: 2726: 2724: 2721: 2719: 2718:Ernst Haeckel 2716: 2714: 2713:Adolf Zeising 2711: 2707: 2706: 2702: 2701: 2700: 2697: 2695: 2692: 2690: 2687: 2685: 2682: 2681: 2679: 2675: 2667: 2664: 2662: 2659: 2657: 2654: 2652: 2649: 2648: 2647: 2644: 2640: 2637: 2635: 2632: 2630: 2627: 2626: 2625: 2622: 2618: 2615: 2613: 2610: 2608: 2605: 2603: 2600: 2599: 2598: 2595: 2593: 2590: 2589: 2587: 2583: 2578: 2568: 2565: 2563: 2560: 2558: 2557:Vortex street 2555: 2553: 2550: 2546: 2543: 2541: 2538: 2536: 2535:Quasicrystals 2533: 2531: 2528: 2527: 2526: 2523: 2521: 2518: 2516: 2513: 2511: 2508: 2506: 2503: 2501: 2498: 2496: 2493: 2491: 2488: 2487: 2485: 2481: 2477: 2470: 2465: 2463: 2458: 2456: 2451: 2450: 2447: 2432: 2428: 2424: 2413: 2409: 2399:on 2008-04-17 2398: 2394: 2390: 2380:on 2008-04-26 2379: 2375: 2370: 2360:on 2006-08-26 2359: 2355: 2350: 2349: 2345: 2330: 2324: 2321: 2315: 2310: 2306: 2302: 2298: 2294: 2290: 2283: 2280: 2274: 2269: 2265: 2261: 2257: 2253: 2249: 2242: 2239: 2235: 2230: 2227: 2224: 2219: 2216: 2212: 2207: 2204: 2199: 2198: 2190: 2187: 2182: 2178: 2174: 2167: 2164: 2160: 2155: 2152: 2147: 2145:9781351416238 2141: 2138:. 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Retrieved 2416:. Retrieved 2401:. Retrieved 2397:the original 2382:. Retrieved 2378:the original 2362:. Retrieved 2358:the original 2333:. Retrieved 2323: 2296: 2292: 2282: 2255: 2251: 2241: 2233: 2229: 2218: 2210: 2206: 2196: 2189: 2181:the original 2176: 2166: 2158: 2154: 2134: 2127: 2107: 2100: 2084: 2079: 2068: 2041: 2033: 2028: 2009: 2003: 1992: 1988: 1953: 1946: 1934:. Retrieved 1929: 1920: 1908:. Retrieved 1904:the original 1897: 1887: 1872: 1867: 1856:. Retrieved 1852: 1843: 1835: 1827: 1819: 1816:Robert Scott 1803: 1792: 1786: 1775:. 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Index

Crystals
Crystalline (song)
Xtal (disambiguation)
Crystal (disambiguation)

amethyst
quartz

single crystal
periodic
polycrystal
crystallites
amorphous
glass
solid
atoms
molecules
ions
crystal lattice
single crystals
geometrical shape
faces
crystallography
crystal growth
crystallization
solidification
Ancient Greek
ice
rock crystal
snowflakes

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