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Dome |
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dome, a roof circular or (rarely) elliptical in plan and usually hemispherical in form, placed over a circular, square, oblong, or polygonal space. Domes have been built with a wide variety of outlines and of various materials.
Early DomesThe earliest domes were probably roofed primitive huts and consisted of bent-over branches plastered with mud. Another primitive form, called a beehive dome, is constructed of concentric rings of corbeled stones and has a conical shape. Ancient examples have been found in the tombs of Mycenae and can also still be seen in the folk architecture of Sicily. Although there is evidence of widespread knowledge of the dome, its early use was apparently restricted to small structures built of mud brick. Roman and Byzantine DomesIt was the Romans who first fully realized the architectural potentialities of the dome. The Roman development in dome construction culminated in the pantheon pantheon , term applied originally to a temple to all the gods. The Renaissance RefinementsBoth the influence of the Roman Pantheon and of the Byzantine pendentive came to bear on the designers of the Italian Renaissance, and the crossings of many churches of the period were covered by masonry domes on pendentives. Between pendentive and dome a circular drum usually was interposed, serving to give greater elevation and external importance as well as a space for the introduction of windows. By the addition of an outer shell, the exterior came to be independently designed for maximum effectiveness, and the placing of a lantern at the top of this outer shell provided an apex for the entire composition. Modern DomesThe dome in modern architecture utilizes such materials of construction as reinforced and thin-shell concrete, glass and steel, and plastic. An innovative contemporary approach to the form is the geodesic dome geodesic dome , structure that roughly approximates a hemisphere. Popular in recent years as economical, easily erected buildings, geodesic domes are geometrically determined from a model and may be constructed from limited materials. Outstanding DomesCelebrated examples are Brunelleschi's octagonal ribbed dome for the Cathedral of Florence (1420–36); St. Peter's, Rome, designed by Michelangelo, with two masonry shells (completed 1590), internal diameter 137 ft (42 m); the church of the Invalides, Paris, by J. H. Mansart (1706), 90 ft (27 m); St. Paul's Cathedral, London, by Sir Christopher Wren (1675–1710), 112 ft (34 m); and the Panthéon, Paris, by J. G. Soufflot (1775–81), 69 ft (21 m). The last three domes are built with triple shells, the middle shells serving to support the crowning lanterns. In the United States the dome of the Massachusetts state capitol, designed (1795) by Charles Bulfinch, established the dome as a distinctive feature for numerous later state capitols as well as for the national Capitol at Washington, D. C. The dome of the latter, however, is of cast iron instead of masonry. The design, by T. U. Walter, has an inner diameter of 90 ft (27 m) and possesses great external impressiveness. BibliographySee E. B. Smith, The Dome: A Study in the History of Ideas (1975). domeIn architecture, a hemispherical structure evolved from the arch, forming a ceiling or roof. Domes first appeared on round huts and tombs in the ancient Middle East, India, and the Mediterranean in forms, such as solid mounds, adaptable only to the smallest buildings. The Romans introduced the large-scale masonry hemisphere. A dome exerts thrust all around its perimeter, and the earliest monumental examples (see Pantheon) required heavy supporting walls. Byzantine architects invented a technique for raising domes on piers, making the transition from a cubic base to the hemisphere by four pendentives. Bulbous or pointed domes were widely used in Islamic architecture. The design spread to Russia, where it gained great popularity in the form of the onion dome, a pointed, domelike roof structure. The modern geodesic dome, developed by R. Buckminster Fuller, is fabricated of lightweight triangular framing that distributes stresses within the structure itself. dome 1. a hemispherical roof or vault or a structure of similar form 2. Crystallog a crystal form in which two planes intersect along an edge parallel to a lateral axis 3. Geology a. a structure in which rock layers slope away in all directions from a central point b. another name for pericline dome [dōm] (architecture) A hemispherical roof. (astronomy) A shallow raised structure on the moon's surface with a smooth convex cross section and a diameter anywhere from a few kilometers up to about 80 kilometers (50 miles). (crystallography) An open crystal form consisting of two faces astride a symmetry plane. (engineering) The portion of a cylindrical container used in a filament-winding process that forms an integral end of the container. (engineering acoustics) An enclosure for a sonar transducer, projector, or hydrophone and associated equipment; designed to have minimum effect on sound waves traveling underwater. (geology) A circular or elliptical, almost symmetrical upfold or anticlinal type of structural deformation. A large igneous intrusion whose surface is convex upward. (ordnance) The mound of water spray created in air when the shock wave from an underwater detonation of an atomic weapon reaches the surface. dome 1. A curved roof structure spanning an area; often spherical in shape. 2. A square prefabricated pan form; used in two-way joist (waffle) concrete floor construction. 3. A vault substantially hemispherical in shape, but sometimes slightly pointed or bulbous; a ceiling of similar form. also see geodesic dome and saucer dome. Dome a covering of buildings and structures, serving as a roof over spaces, normally those with a circular, polygonal, or elliptical floor plan. The shape of the dome follows a curve that is convex to the exterior of the building. Stresses existing in a dome consist not only of the basic compression loads, which transmit the weight of the roof to the supports, but also of horizontal thrusts. To accommodate the horizontal forces, special tension structures are sometimes provided, such as support rings at the base of the dome. Such structures were first introduced in the 15th century. It is possible that the first domes were parts of thatched huts made of pliable material (reeds, branches) and clay. In antiquity, domes were built of stone and fired brick. These domes were actually corbel vaults with horizontal circles of masonry that progressively diminished in diameter in such a way that no horizontal thrust was transmitted to the walls (buildings in the town of Eshnunna in Mesopotamia, dating back to the early third millennium B.C.; the Treasury of Atreus in Mycenae, 14th century B.C. [?]). Corbel vaults were widely used in the popular architecture of many countries, for example, the gvirgvini, the stepped roof of Georgian folk dwellings. In ancient Rome the true dome attained great importance after the introduction of squinches and particularly after the invention of concrete. In centrally planned buildings, domes with large spans enhanced the role of the covered spaces within the architectural composition and imparted to them spaciousness and solemn grandeur. The power and firmness of religious beliefs often found expression in such architecture (for example, the imposing dome of the Pantheon in Rome). In Byzantine architecture, pendentive domes and squinch domes were widely used. (Both had appeared earlier in the architecture of ancient Rome and of Iran during the age of the Sassa-nids.) Squinches and pendentives made it possible to erect a dome above a space with any type of floor plan (for example, Hagia Sophia in Constantinople). During the Middle Ages various types of domes were used in Europe and the Caucasus, predominantly in cruciform domed churches (for instance, Dzhvari Church near Mtskheta in Georgia; Ripsime Church in Echmiadzin in Armenia). In the feudal states of Middle Asia and the Middle East, buildings appeared with large central domes. As the role of the dome became understood in terms of its effect not only on the interior but also on the exterior of the building, the outer contour of the dome changed in its relation to the inner contour. Later the false dome appeared—an external shell with an outline differing from that of the dome proper. Such a shell usually consisted of curvilinear roofing supported by wooden rafters; an early example is the dome of St. Mark’s Church in Venice (ninth to 11th centuries). Domes with outer shells, which usually crowned the vertical space of religious buildings and were calculated to be in harmony with their architectural or natural surroundings, were particularly popular in the architecture of medieval Russia and of Middle Asia (for example, the mosque of Bibi Khanum in Samarkand, 1399–1401, which has an inner and an outer dome). During the Renaissance the treatment of the dome as a plastic shape in space and as a dominant feature of urban design became widespread in the architecture of Western Europe. An example is the dome of Santa Maria del Fiore in Florence (1420–36, architect F. Brunelleschi), where for the first time the two shells of the dome were connected by stiffening stone ribs and by wooden rings, thus forming a unified structure. Beginning at the end of the 18th century, domes were used in secular buildings. In the second half of the 19th century, domes of stone and brick were replaced by domes constructed of glass and metal frames or of wood or reinforced concrete. Masonry domes were at a disadvantage because of their great weight and the large amount of labor required for their construction. In the 20th century, with the development of monolithic and precast reinforced concrete, thin-walled shell vaults, and metal structures, the diversity of domical shapes and structures increased drastically. New types that appeared included ribbed domes, rib-and-ring domes, domes with rippled inner surfaces, geodesic domes (designed by B. Fuller, with diameters up to 150 m), and prefabricated domes creating the impression of a monolithic whole (designed by P. L. Nervi). Other innovative types include domes built of polymeric materials and those with an inflated double shell. REFERENCESKuznetsov, A. V. Svody i ikh dekor. Moscow, 1938.Kuznetsov, A. V. Tektonika i konstruktsiia tsentricheskikh zdanii. Moscow, 1951. Spravochnik proektirovshchika promyshlennykh, zhilykh i obshchestven-nykh zdanii i sooruzhenii: Rashchetno teoreticheskii. Moscow, 1960. Dereviannye konstruktsii, 3rd ed. Edited by G. G. Karlsen. Moscow, 1961. Zhelezobetonnye konstruktsii: Spetsial’nyi kurs. Edited by P. L. Pasternak. Moscow, 1961. Gokhar’-Kharmandarian, I. G. Bol’sheproletnye kupol’nye zdaniia. Moscow, 1972. Mukhanov, K. K. Metallicheskie konstruktsii. Moscow, 1963. Smith, E. B. The Dome. New York, 1950. V. F. MARKUZON Dome (geology), mode of occurrence of rock. (1) Volcanic (or magmatic) dome, a mode of occurrence of igneous rock in the form of a bun-shaped body. It forms on the earth’s surface when very viscous acid lava is extruded from a volcanic vent. It often has a characteristic radial and concentric jointing. (2) Granite-gneiss (or gneiss) dome, an uplift of layers of the earth’s crust; the central part of the uplift is composed of granite-gneisses and gneisses, sometimes cut by granites, occurring in relatively gently sloping beds. The periphery of the gneiss core is composed of crystalline schists of increasingly lower degrees of metamorphism, crushed into small folds that are often tilted toward the center of the dome. Granite-gneiss domes form as a result of the floating up of granite material during regional metamorphism and granitization or repeated heating of the ancient granite-gneiss base. These domes are found mainly in the shields of ancient platforms. They may be many dozens of kilometers in diameter. (3) Tectonic dome, a more or less rounded uplift of layers of the earth’s crust, which slopes down in all directions from the center of the dome. They may be dozens of kilometers (and sometimes up to 100) in diameter. Tectonic domes are found on platforms for the most part. (4) Salt dome, a rounded uplift of rock layers with a nucleus of rock salt or other kind of salt. It forms when, owing to its lower density and high plasticity as compared to other sedimentary rocks, salt rises and is intruded. These domes are common in areas of deep submersion of the crystalline crust in platform basins and in the foredeeps and intermontane areas of mountain belts. In the USSR they are found in the Caspian, Dnieper, Donets, Tadzhik, and other basins. V. E. KHAIN Want to thank TFD for its existence? Tell a friend about us, add a link to this page, add the site to iGoogle, or visit the webmaster's page for free fun content. |
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