Chimiquement, la rhodolite est un silicate de fer, de magnésium et d'aluminium, qui fait partie de la série de solutions solides pyrope-almandin, et elle a une composition approximative en grenat de Py70Al30. In yttrium iron garnet (YIG), Y3Fe2(FeO4)3, the five iron(III) ions occupy two octahedral and three tetrahedral sites, with the yttrium(III) ions coordinated by eight oxygen ions in an irregular cube. The garnets from mantle-derived rocks, peridotites, and eclogites commonly contain a pyrope variety. This type of garnet is produced in America, China and western India. pp. , Rock garnet is perhaps the garnet type used for the longest period of time. The curious lore of precious stones. Being freshly crushed, this garnet has the sharpest edges and therefore performs far better than other kinds of garnet. In daylight, their color ranges from shades of green, beige, brown, gray, and blue, but in incandescent light, they appear a reddish or purplish/pink color. Because the chemical composition of garnet varies, the atomic bonds in some species are stronger than in others. Other varieties of gem-quality corundum are called sapphires. Almandine, sometimes incorrectly called almandite, is the modern gem known as carbuncle (though originally almost any red gemstone was known by this name). rhodochrosite, rhodonite).  . Garnets can be chemically altered and most often alter to serpentine, talc, and chlorite. En effet, sa couleur comporte des tons de rose, de rouge et de violet. The mineral spessartine should not be confused with a type of igneous rock (a lamprophyre) called spessartite. The word garnet comes from the 14th‑century Middle English word gernet, meaning 'dark red'.It is borrowed from Old French grenate from Latin granatus, from granum ('grain, seed'). Son nom est un dérivé du terme grec rhodon signifiant “semblable à la rose”. All species of garnets possess similar physical properties and crystal forms, but differ in chemical composition. Lippincott. For gem identification purposes, a pick-up response to a strong neodymium magnet separates garnet from all other natural transparent gemstones commonly used in the jewelry trade. The color of pyrope varies from deep red to black. Spinel is the magnesium/aluminium member of the larger spinel group of minerals. Spessartine of an orange-yellow is found in Madagascar. In mineralogy, an inclusion is any material that is trapped inside a mineral during its formation. In chemical composition it may be considered as essentially an isomorphous mixture of pyrope and almandine, in the proportion of two parts pyrope to one part almandine. Most natural garnets are compositionally zoned and contain inclusions. 319-320. The gemstone varieties occur in shades of green, red, yellow, and orange.  Its crystal lattice structure is stable at high pressures and temperatures and is thus found in green-schist facies metamorphic rocks including gneiss, hornblende schist, and mica schist. Its county seat is Franklin. , This material is particularly popular due to its consistent supplies, huge quantities and clean material. Il ne faut pas confondre le poids en carat d’une pierre avec le carat d’or, qui est l’unité utilisée pour définir la pureté du précieux métal. Vous pouvez partager vos connaissances en l’améliorant (comment ?) Ces inclusions sont des caractéristiques naturelles, et permettent de vérifier l’authenticité et l’origine de la pierre.  The harder species like almandine are often used for abrasive purposes. Rhodolite. , Pure crystals of garnet are still used as gemstones. Tsavorite was first described in the 1960s in the Tsavo area of Kenya, from which the gem takes its name. The common problems with this material are the presence of ilmenite and chloride compounds. , The color of rhodolites, combined with their brilliance, durability, and the accessibility of stones with no visible inclusions have brought about some demand for the stone in the jewelry industry. Rhodolite: Vierge, taureau, scorpion. New York has garnet as its state gemstone, Connecticut has almandine garnet as its state gemstone, Idaho has star garnet as its state gemstone, and Vermont has grossular garnet as its state gemstone. On peut le tailler selon de nombreuses formes car c’est une pierre assez solide. 2. Rhodolites from different occurrences around the world have been characterized by crystal chemical and absorption spectral analysis showing that besides iron such elements as manganese, chromium and vanadium may effect the colour of rhodolites. Sapphirine has also been synthesized for experimental purposes via a hydrothermal process. The remaining garnet pieces that are finer than 200 mesh (74 micrometers) are used for glass polishing and lapping. Garnets are used as an index mineral in the delineation of isograds in metamorphic rocks. Another intriguing find is the blue color-changing garnets from Madagascar, a pyrope-spessartine mix. Yttrium aluminium garnet (YAG), Y3Al2(AlO4)3, is used for synthetic gemstones. The color of these blue garnets is not like sapphire blue in subdued daylight but more reminiscent of the grayish blues and greenish blues sometimes seen in spinel. It occurs most often in granite pegmatite and allied rock types and in certain low grade metamorphic phyllites. This is a rather rare garnet, bright green in color, usually found as small crystals associated with chromite in peridotite, serpentinite, and kimberlites. Mineralogically and chemically, rhodolite garnets are members of the pyrope-almandine solid-solution series, with an approximate bulk garnet composition of Py70Al30. However, certain rocks and occasionally organic materials that are not minerals are also used for jewelry and are therefore often considered to be gemstones as well. It is borrowed from Old French grenate from Latin granatus, from granum ('grain, seed'). The name is a corruption of alabandicus, which is the name applied by Pliny the Elder to a stone found or worked at Alabanda, a town in Caria in Asia Minor. Knorringite is a magnesium-chromium garnet species with the formula Mg3Cr2(SiO4)3. A cabochon is a gemstone which has been shaped and polished as opposed to faceted. Viewed through the spectroscope in a strong light, it generally shows three characteristic absorption bands.
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