Silicate minerals
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▪ TableSilicate mineralsname colour lustre Mohs hardness specific gravityTectosilicates (three-dimensional networks)feldspar (for other examples, see feldspar)orthoclase flesh-red, white to pale yellow, red, green vitreous 6–6½ 2.6feldspathoid (for other examples, see feldspathoid)nepheline light-coloured; reddish, greenish, brownish vitreous to greasy 5½–6 2.6–2.7silica (for other examples, see silica mineral)quartz variable vitreous to greasy (coarse-grained); waxy to dull (fine-grained) 7 (a hardness standard) 2.65zeolite (for other examples, see zeolite)chabazite white; flesh-red vitreous 4½ 2.0–2.1Phyllosilicates (sheet structures)clay (for other examples, see clay mineral)chlorite green vitreous or pearly 2–3 2.6–3.0smectite 2.2–2.7mica (for other examples, see mica)apophyllite colourless, white, pink, pale yellow, or green pearly iridescent 4½–5 2.3–2.4muscovite commonly white or colourless; light shades of green, red, or brown vitreous to silky or pearly 2–2½ 2.8–3.0prehnite pale green to gray, white, or yellow vitreous 6–6½ 2.9–3.0pyrophyllite white and various pale colours dull and glistening 1–2 2.6–2.9talc colourless; white; pale or dark green; brown pearly 1 (a hardness standard) 2.6–2.8Inosilicates (chain structures)amphibole (for other examples, see amphibole)common hornblende pale to dark green glassy 5–6 3.0–3.4mullite white 3.0pyroxene (for other examples, see pyroxene)augite brown, green, black vitreous 5½–6 3.2–3.5rhodonite pink to brownish red vitreous 5½–6½ 3.6–3.8wollastonite white; also colourless, gray, or very pale green vitreous 4½–5 2.9–3.1Cyclosilicates (ring structures)axinite clove- or lilac-brown; pearl-gray; yellowish highly glassy 6½–7 3.3–3.4beryl various greens; variable, including deep-green (emerald), blue-green (aquamarine), pink (morganite), yellow (heliodore) vitreous 7½–8 2.7–2.8cordierite various blues vitreous 7 2.5–2.8tourmaline extremely variable vitreous to resinous 7–7½ 3.0–3.2Sorosilicates (double tetrahedral structures)hemimorphite white, sometimes tinted bluish or greenish; yellow to brown vitreous 5 3.4–3.5melilite colourless; grayish green; brown vitreous to resinous 5–6gehlenite 3.1åkermanite 2.9Nesosilicates (independent tetrahedral structures)andalusite pink, white, or rose-red; also variable vitreous 6½–7½ 3.1–3.2chrysocolla green, bluish green vitreous 2–4 2.0–2.8datolite colourless or white; also various pale tints vitreous 5–5½ 2.9–3.0epidote yellowish green to dark green vitreous 6–7 3.3–3.5garnet variable vitreous to resinous 6–7½almandine 4.3andradite 3.9grossularite 3.6pyrope 3.6spessartite 4.2uvarovite 3.9kyanite blue; white; also variable vitreous to pearly 4–7 (variable) 3.5–3.7olivine (for other examples, see olivines)forsterite-fayalite series various greens and yellows vitreous 6½–7 3.2 (forsterite) to 4.4 (fayalite)phenacite colourless; also wine-yellow, pale rose, brown vitreous 7½–8 3.0sillimanite colourless or white; also various browns and greens vitreous to subadamantine 6½–7½ 3.2–3.3sphene colourless, yellow, green, brown, black adamantine to resinous 5 3.4–3.6staurolite dark red-brown; yellow-brown; brown-black subvitreous to resinous 7–7½ 3.7–3.8thorite black; also orange-yellow (orangite) 4½–5 4.5–5.0; 5.2–5.4 (orangite)topaz straw- or wine-yellow; white; grayish, greenish, bluish, reddish vitreous 8 (a hardness standard) 3.5–3.6vesuvianite yellow, green, brown vitreous 6–7 3.3–3.4willemite white or greenish yellow vitreous to resinous 5½ 3.9–4.2zircon reddish brown, yellow, gray, green, or colourless adamantine 7½ 4.6–4.7zoisite white; gray; green-brown; pink (thulite) vitreous 6–6½ 3.2–3.4name habit fracture or cleavage refractive indices crystal systemTectosilicates (three-dimensional networks)feldspar (for other examples, see feldspar)orthoclase twinned crystals two good cleavages of 90 degrees alpha = 1.518–1.529beta = 1.522–1.533gamma = 1.522–1.539 monoclinicfeldspathoid (for other examples, see feldspathoid)nepheline small glassy crystals or grains poor cleavage omega = 1.529–1.546epsilon = 1.526–1.542 hexagonalsilica (for other examples, see silica mineral)quartz prismatic and rhombohedral crystals; massive conchoidal fracture omega = 1.544epsilon = 1.553 hexagonalzeolite (for other examples, see zeolite)chabazite single, cubelike rhombohedrons poor cleavage omega = 1.470–1.494epsilon = 1.470–1.494 hexagonalPhyllosilicates (sheet structures)clay (for other examples, see clay mineral)chlorite large crystalline blocks; fine-grained, flaky aggregates platy cleavage alpha = 1.57–1.64gamma = 1.575–1.645 monoclinic or triclinicsmectite broad undulating mosaic sheets that break into irregular fluffy masses of minute particles alpha = 1.480–1.590gamma = 1.515–1.630mica (for other examples, see mica)apophyllite tabular, prismatic, or granular crystals; prisms and bipyramids when well-formed one perfect, one poor cleavage omega = 1.534–1.535epsilon = 1.535–1.537 tetragonalmuscovite large tabular blocks (called books); pseudohexagonal crystals; fine-grained aggregates one perfect, platy cleavage alpha = 1.552–1.574beta = 1.582–1.610gamma = 1.587–1.616prehnite rosettes of small radiating crystals; tabular or prismatic crystals; lamellar or botryoidal massive one good cleavage alpha = 1.611–1.632beta = 1.615–1.642gamma = 1.632–1.665 orthorhombicpyrophyllite lamellar massive; granular to compact massive one perfect cleavage alpha = 1.534–1.556beta = 1.586–1.589gamma = 1.596–1.601 monoclinictalc compact foliated masses one perfect cleavage alpha = 1.539–1.553beta = 1.589–1.594gamma = 1.589–1.600 monoclinicInosilicates (chain structures)amphibole (for other examples, see amphibole)common hornblende massive one good cleavage of 56 degrees alpha = 1.615–1.705beta = 1.618–1.714gamma = 1.632–1.730 monoclinicmullite elongated prismatic crystals; melts one distinct cleavage alpha = 1.642–1.653beta = 1.644gamma = 1.654–1.679 orthorhombicpyroxene (for other examples, see pyroxene)augite short, thick, tabular crystals one good cleavage of 87 degrees alpha = 1.671–1.735beta = 1.672–1.741gamma = 1.703–1.761 monoclinicrhodonite rounded tabular crystals; cleavable to compact massive; embedded grains two perfect cleavages alpha = 1.711–1.738beta = 1.715–1.741gamma = 1.724–1.751 triclinicwollastonite cleavable, fibrous, or compact massive; tabular crystals one perfect, two good cleavages alpha = 1.616–1.640beta = 1.628–1.650gamma = 1.631–1.653 triclinicCyclosilicates (ring structures)axinite broad, sharp-edged, wedge-shaped crystals; lamellar massive one good cleavage alpha = 1.674–1.693beta = 1.681–1.701gamma = 1.684–1.704 triclinicberyl long hexagonal crystals conchoidal to uneven fracture omega = 1.569–1.598epsilon = 1.565–1.590 hexagonalcordierite short prismatic crystals; embedded grains; compact massive one distinct cleavage alpha = 1.522–1.558beta = 1.524–1.574gamma = 1.527–1.578 orthorhombictourmaline parallel or radiating groups of striated, elongated hexagonal prisms, often rounded or barrel-shaped; massive subconchoidal to uneven fracture omega = 1.635–1.675epsilon = 1.610–1.650 hexagonalSorosilicates (double tetrahedral structures)hemimorphite sheaflike crystal aggregates one perfect cleavage alpha = 1.614beta = 1.617gamma = 1.636 orthorhombicmelilite short prismatic crystals; tablets one distinct cleavage tetragonalgehlenite omega = 1.669epsilon = 1.658åkermanite omega = 1.632epsilon = 1.640Nesosilicates (independent tetrahedral structures)andalusite coarse prisms; massive one good cleavage of 89 degrees alpha = 1.629–1.640beta = 1.633–1.644gamma = 1.638–1.650 orthorhombicchrysocolla crusts; botryoidal masses conchoidal fracture omega = 1.46epsilon = 1.54 orthorhombic?datolite tabular or short prismatic crystals; botryoidal and globular or divergent and radiating massive conchoidal to uneven fracture alpha = 1.622–1.626beta = 1.649–1.654gamma = 1.666–1.670 monoclinicepidote striated elongated crystals; fibrous or granular massive; disseminated one perfect cleavage alpha = 1.712–1.756beta = 1.720–1.789gamma = 1.723–1.829 monoclinicgarnet crystals; irregular embedded grains; compact, granular, or lamellar massive subconchoidal fracture isometricalmandine n = 1.830andradite n = 1.887grossularite n = 1.734pyrope n = 1.714spessartite n = 1.800uvarovite n = 1.86kyanite elongated tabular, bladed crystals one good, one perfect cleavage alpha = 1.712–1.718beta = 1.719–1.723gamma = 1.727–1.734 triclinicolivine (for other examples, see olivines)forsterite-fayalite series flattened crystals; compact or granular massive; embedded grains one indistinct cleavage alpha = 1.631–1.827beta = 1.651–1.869gamma = 1.670–1.879 orthorhombicphenacite rhombohedral crystals one distinct cleavage omega = 1.654epsilon = 1.670 hexagonalsillimanite vertically striated, square prisms; long, slender parallel crystal groups to fibrous or columnar massive one perfect cleavage alpha = 1.654–1.661beta = 1.658–1.670gamma = 1.673–1.684 orthorhombicsphene wedge-shaped crystals, often twinned; compact massive one good cleavage alpha = 1.843–1.950beta = 1.870–2.034gamma = 1.943–2.110 monoclinicstaurolite cruciform twins one distinct cleavage alpha = 1.739–1.747beta = 1.744–1.754gamma = 1.750–1.762 monoclinicthorite square prismatic crystals; small masses one distinct cleavage omega = 1.8 tetragonaltopaz prismatic crystals one perfect cleavage alpha = 1.606–1.629beta = 1.609–1.631gamma = 1.616–1.638 orthorhombicvesuvianite prismatic crystals; massive subconchoidal to uneven fracture omega = 1.703–1.752epsilon = 1.700–1.746 tetragonalwillemite hexagonal prismatic crystals; disseminated grains; fibrous massive one easy cleavage omega = 1.691–1.714epsilon = 1.719–1.732 hexagonalzircon square prismatic crystals; irregular forms; grains conchoidal fracture omega = 1.923–1.960epsilon = 1.968–2.015 tetragonalzoisite striated prismatic crystals; columnar to compact massive one perfect cleavage alpha = 1.685–1.705beta = 1.688–1.710gamma = 1.697–1.725 orthorhombicSee as table:
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Universalium. 2010.
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Silicate minerals — The silicate minerals make up the largest and most important class of rock forming minerals, constituting approximately 90 percent of the crust of the Earth. They are classified based on the structure of their silicate group. Silicate minerals… … Wikipedia
silicate mineral — Any of a large group of silicon oxygen compounds that are widely distributed throughout much of the solar system. The silicates make up about 95% of the Earth s crust and upper mantle, occurring as the major constituents of most igneous rocks and … Universalium
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Silicate — Häufige natürliche Erscheinungsform der Silikate: Feldspat … Deutsch Wikipedia
silicate — noun Etymology: silicic (acid) Date: 1811 a salt or ester derived from a silicic acid; especially any of numerous insoluble often complex metal salts that contain silicon and oxygen in the anion, constitute the largest class of minerals, and are… … New Collegiate Dictionary
silicate — silication /sil i kay sheuhn/, n. /sil i kit, kayt /, n. 1. Mineral. any of the largest group of mineral compounds, as quartz, beryl, garnet, feldspar, mica, and various kinds of clay, consisting of SiO2 or SiO4 groupings and one or more metallic … Universalium
silicate — 1. A salt of silicic acid. 2. The term sometimes applied to dental restorations of synthetic porcelain. * * * sil·i·cate sil ə .kāt, sil i kət n a salt or ester derived from a silicic acid esp any of numerous insoluble often complex metal salts… … Medical dictionary
silicate — sil·i·cate || sɪlɪkÉ™t / keɪt n. any of a large number of mineral compounds which form over 90 percent of the rock forming minerals of the earth s crust (Mineralogy); salt of silicic acid (Chemistry) … English contemporary dictionary
silicate — sil•i•cate [[t]ˈsɪl ɪ kɪt, ˌkeɪt[/t]] n. 1) mir any of the largest group of minerals, as quartz, olivine, pyroxene, amphibole, mica, clay, and feldspar, consisting of silicon and oxygen with one or more metals: the basic building block is the… … From formal English to slang