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Deep green isolated fluorite crystal shawin cubic an octahedral faces, set on a micaceous matrix, frae Erongo Mountain, Erongo Region, Namibie (overall size: 50 mm x 27 mm, crystal size: 19 mm wide, 30 g)
Category Halide meeneral
(repeatin unit)
Strunz clessification 03.AB.25
Creestal seestem Isometric, cF12, SpaceGroup Fm3m, No. 225
Space group Isometric H–M Symbol 4/m 3 2/m
Unit cell a = 5.4626 Å; Z=4
Colour Colourless, white, purpie, blae, green, yellae, orange, reid, pink, broun, blaeish black; commonly zoned; can be ony colour o the spectrum.
Creestal habit Occurs as weel-formed coarse sized crystals an nodular, botryoidal, rarely columnar or fibrous; granular, massive
Twinnin Common on {111}, interpenetrant, flattened
Cleavage Octahedral, perfect on {111}, pairtin on {011}
Fractur Subconchoidal tae uneven
Tenacity Brickle
Mohs scale haurdness 4 (definin meeneral)
Skinkle Vitreous
Streak White
Diaphaneity Skyre tae leamin
Speceefic gravity 3.175–3.184; tae 3.56 gif heich in rare-yird elements
Optical properties Isotropic; waik anomalous anisotropism
Refractive index 1.433–1.448
Fusibility 3
Ither chairacteristics whiles phosphoresces whan heatit or scartit. Ither varieties fluoresce
References [1][2][3][4]

Fluorite (forbye cried fluorspar) is a halide meeneral componed o calcium fluoride, CaF2. It is an isometric meeneral wi a cubic habit, tho octahedral an mair complex isometric furms arenae uncommon.

Fluorite is a colourful meeneral, baith in veesible an ultraviolet licht, an the stane haes ornamental an lapidary uses. Industrially, fluorite is uised as a flux for smeltin, an in the production o certaint glasses an enamels. The purest grades o fluorite is a soorce o fluoride for hydrofluoric acid manufactur, that is the intermediate soorce o maist fluorine-containin fine chemicals. Optically clear transparent fluorite lenses hae law dispersion, sae lenses made frae it exhibit less chromatic aberration, makkin thaim valuable in microscopes an telescopes. Fluorite optics can be uised in the far-ultraviolet range an aw, whaur conventional glesses is too absorbent tae uise.

References[eedit | eedit soorce]

  1. Anthony, John W.; Bideaux, Richard A.; Bladh, Kenneth W. and Nichols, Monte C. (ed.). "Fluorite". Handbook of Mineralogy (PDF). III (Halides, Hydroxides, Oxides). Chantilly, VA, US: Mineralogical Society of America. ISBN 0962209724. Retrieved December 5, 2011. 
  2. Fluorite. Mindat.org
  3. Fluorite. Webmineral.com
  4. Hurlbut, Cornelius S.; Klein, Cornelis, 1985, Manual of Mineralogy, pp. 324–325, 20th ed., ISBN 0-471-80580-7