Phenakite
Template:Short description Template:About Template:Infobox mineral
Phenakite or phenacite is a fairly rare nesosilicate mineral consisting of beryllium orthosilicate, Be2SiO4. Occasionally used as a gemstone, phenakite occurs as isolated crystals, which are rhombohedral with parallel-faced hemihedrism, and are either lenticular or prismatic in habit: the lenticular habit is determined by the development of faces of several obtuse rhombohedra and the absence of prism faces. There is no cleavage, and the fracture is conchoidal. The Mohs hardness is high, being 7.5–8; the specific gravity is 2.96. The crystals are sometimes perfectly colorless and transparent, but more often they are greyish or yellowish and only translucent; occasionally they are pale rose-red. In general appearance the mineral is not unlike quartz, for which indeed it has been mistaken.<ref name=EB1911>{{#if: |
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}}{{#ifeq: ||}}</ref> Its name comes from Template:Langx, meaning "deceiver" due to its close visual similarity to quartz,<ref>Firefly Guide to Gems By Cally Oldershaw p.94</ref> named by Nils Gustaf Nordenskiöld in 1833.<ref name=Mindat/><ref name=EB1911/>
Largest phenakiteEdit
A large phenakite gemstone has been found in Sri Lanka. Found on November 18, 2021, this gemstone weighs 616.9 carats which makes it the largest of its kind. It is owned by a gem dealer from Beruwala, Sri Lanka, and reported to be worth around Template:Nowrap (US $Template:To USD million).<ref name=sri>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
OccurrenceEdit
Phenakite is found in high-temperature pegmatite veins and in mica-schists associated with quartz, chrysoberyl, apatite and topaz. It has long been known from the emerald and chrysoberyl mine on the Takovaya stream, near Yekaterinburg in the Urals of Russia, where large crystals occur in mica-schist. It is also found with topaz and amazonite in the granite of the Ilmen Mountains in the southern Urals and of the Pikes Peak region in Colorado, US.<ref name=EB1911/> Additionally in Colorado, phenakite is found in the Mount Antero area with aquamarine, bertrandite, and fluorite.<ref>Template:Cite journal</ref><ref>Template:Cite journal</ref> Small, gem grade individual crystals of phenakite showing a prismatic habit are noted in beryl dissolution cavities at the Noumas II Pegmatite, part of the Orange River pegmatite belt in the Northern Cape of South Africa.<ref>Template:Cite book</ref> Large crystals of prismatic habit have been found in a feldspar quarry at Kragerø in Norway. Framont near Schirmeck in Alsace is another well-known locality. Still larger crystals, measuring Template:Convert in diameter and weighing Template:Convert. have been found at Greenwood in Maine, but these are pseudomorphs of quartz after phenakite.<ref name=EB1911/>
For gem purposes the stone is cut in the brilliant form, of which there are two fine examples, weighing 34 and 43 carats (6.8 and 8.6 g), in the British Museum. The indices of refraction are higher than those of quartz, beryl or topaz; a faceted phenakite is consequently rather brilliant and may sometimes be mistaken for diamond.<ref name=EB1911/>