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Continuum mechanics. Charles's law (also known as the law of volumes) is an experimental gas law that describes how gases tend to expand when heated. A modern statement of Charles's law is: When the pressure on a sample of a dry gas is held constant, the Kelvin temperature and the volume will be in direct proportion.
Jarndyce and Jarndyce (or Jarndyce v Jarndyce) is a fictional probate case in Bleak House (1852–53) by Charles Dickens, progressing in the English Court of Chancery. The case is a central plot device in the novel and has become a byword for seemingly interminable legal proceedings. Dickens refers to the case as "Jarndyce and Jarndyce", the ...
Marble is a metamorphic rock consisting of carbonate minerals (most commonly calcite (CaCO 3) or dolomite (CaMg (CO 3) 2) that have recrystallized under the influence of heat and pressure. [1] It has a crystalline texture, and is typically not foliated (layered), although there are exceptions. In geology, the term marble refers to metamorphosed ...
Terrazzo is a composite material, poured in place or precast, which is used for floor and wall treatments. It consists of chips of marble, quartz, granite, glass, or other suitable material, poured with a cementitious binder (for chemical binding), polymeric (for physical binding), or a combination of both. Metal strips often divide sections ...
Louis XIV style. The Louis XIV style or Louis Quatorze (/ ˌluːi kæˈtɔːrz, - kəˈ -/ LOO-ee ka-TORZ, - kə-, French: [lwi katɔʁz] ⓘ), also called French classicism, was the style of architecture and decorative arts intended to glorify King Louis XIV and his reign. It featured majesty, harmony and regularity. It became the official ...
Quartz. Quartz is a hard, crystalline mineral composed of silica (silicon dioxide). The atoms are linked in a continuous framework of SiO 4 silicon–oxygen tetrahedra, with each oxygen being shared between two tetrahedra, giving an overall chemical formula of SiO 2. Quartz is, therefore, classified structurally as a framework silicate mineral ...
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The Mohs scale (/ moʊz / MOHZ) of mineral hardness is a qualitative ordinal scale, from 1 to 10, characterizing scratch resistance of minerals through the ability of harder material to scratch softer material. The scale was introduced in 1812 by the German geologist and mineralogist Friedrich Mohs, in his book Versuch einer Elementar-Methode ...
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