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{{Short description|Mineral}} {{about|the mineral|the community in Canada|Actinolite, Ontario}} {{redirect|Uralite|the rail stop|Uralite Halt railway station}} {{Infobox mineral |boxbgcolor=#987630| name = Actinolite | boxtextcolor = #fff | category = [[Inosilicates]] | image = Actinolite Portugal.jpg | imagesize = 260px | alt = | caption = Actinolite crystal from [[Portugal]] | formula = Ca<sub>2</sub>(Mg<sub>4.5-2.5</sub>Fe<sup>2+</sup><sub>0.5-2.5</sub>) <br/>Si<sub>8</sub>O<sub>22</sub>(OH)<sub>2</sub> |IMAsymbol=Act<ref>{{Cite journal|last=Warr|first=L.N.|date=2021|title=IMA–CNMNC approved mineral symbols|journal=Mineralogical Magazine|volume=85|issue=3|pages=291–320|doi=10.1180/mgm.2021.43|bibcode=2021MinM...85..291W|s2cid=235729616|doi-access=free}}</ref> | molweight = | strunz = 9.DE.10 | system = [[Monoclinic]] | class = Prismatic (2/m) <br/><small>(same [[H-M symbol]])</small> | symmetry = ''C2/m'' | color = pale to dark green, yellowish green, blue and black. White or grey when in asbestos | habit = bladed, fibrous, radial | twinning = simple or lamellar | cleavage = perfect along {110}. | fracture = uneven | mohs = 5–6 | luster = vitreous to dull | polish = vitreous | refractive = n<sub>α</sub> = 1.613–1.628<br/> n<sub>β</sub> = 1.627–1.644<br/> n<sub>γ</sub> = 1.638–1.655 | opticalprop = Biaxial (−) | 2V = 78–82° (calc), 84–73° (meas) | dispersion = r < v | birefringence = 0.0250–0.0270 | pleochroism = moderate, yellow to dark green (in stones that are transparent) | fluorescence= inert | absorption = faint line at 503 nm | streak = white | gravity = 3.00 (+0.10, -0.05) | density = | melt = | fusibility = | diagnostic = | solubility = | diaphaneity = translucent to transparent | other = |references = <ref>[http://www.mindat.org/min-18.html Actinolite]. Mindat.org</ref><ref name=wembmin>[http://www.webmineral.com/data/Actinolite.shtml Actinolite]. Webmineral.org</ref><ref>[http://rruff.geo.arizona.edu/doclib/hom/actinolite.pdf Actinolite]. Handbook of mineralogy</ref><ref name="GRG">Gem Reference Guide. City: [[Gemological Institute of America]] (GIA), 1988. {{ISBN|0-87311-019-6}}</ref><ref>[http://pubsites.uws.edu.au/ima-cnmnc/ IMA Master List]</ref> }} '''Actinolite''' is an [[amphibole]] [[silicate minerals|silicate mineral]] with the chemical formula {{nowrap|Ca<sub>2</sub>(Mg<sub>4.5–2.5</sub>Fe<sup>2+</sup><sub>0.5–2.5</sub>)Si<sub>8</sub>O<sub>22</sub>(OH)<sub>2</sub>}}. ==Etymology== The name ''actinolite'' is derived from the [[Greek language|Greek]] word ''aktis'' ({{lang|grc|ἀκτίς}}), meaning "beam" or "ray", because of the mineral's fibrous nature.<ref name=wembmin/> ==Mineralogy== Actinolite is an intermediate member in a [[Solid solution|solid-solution]] series between magnesium-rich [[tremolite]], {{nowrap|Ca<sub>2</sub>(Mg<sub>5.0-4.5</sub>Fe<sup>2+</sup><sub>0.0-0.5</sub>)Si<sub>8</sub>O<sub>22</sub>(OH)<sub>2</sub>}}, and iron-rich [[ferro-actinolite]], {{nowrap|☐Ca<sub>2</sub>(Mg<sub>2.5-0.0</sub>Fe<sup>2+</sup><sub>2.5-5.0</sub>)Si<sub>8</sub>O<sub>22</sub>(OH)<sub>2</sub>}}. Mg and Fe [[ion]]s can be freely exchanged in the [[crystal]] structure. Like tremolite, [[asbestiform]] actinolite is regulated as [[asbestos]]. ==Occurrence== Actinolite is commonly found in [[metamorphic rock]]s, such as [[Contact metamorphism|contact aureole]]s surrounding cooled [[Intrusive rock|intrusive]] [[igneous rock]]s. It also occurs as a product of [[metamorphism]] of magnesium-rich [[limestone]]s. The old mineral name ''uralite'' is at times applied to an alteration product of primary [[pyroxene]] by a mixture composed largely of actinolite. The metamorphosed [[gabbro]] or [[diabase]] [[Rock (geology)|rock]] bodies, referred to as [[epidiorite]], contain a considerable amount of this ''uralitic'' alteration. Fibrous actinolite is one of the six recognised types of [[asbestos]], the [[fibre]]s being so small that they can enter the [[lung]]s and damage the [[Pulmonary alveolus|alveoli]]. Actinolite asbestos was once mined along Jones Creek at [[Gundagai]], Australia. ==Gemology== Some forms of actinolite are used as [[gemstone]]s. One is [[nephrite]], one of the two types of [[jade]] (the other being [[jadeite]], a variety of pyroxene).<ref name="GRG"/> Another gem variety is the [[chatoyant]] form known as ''cat's-eye actinolite''. This stone is translucent to opaque, and green to yellowish green color. This variety has had the misnomer ''jade cat's-eye''. Transparent actinolite is rare and is faceted for gem collectors. Major sources for these forms of actinolite are [[Taiwan]] and [[Canada]]. Other sources are [[Madagascar]], [[Tanzania]], and the [[United States]].<ref name="GRG"/> ==See also== {{Portal|Earth sciences}} * [[Classification of minerals (disambiguation)|Classification of minerals]] * [[List of minerals]] ==References== {{Reflist}} * Hurlbut, Cornelius S.; Klein, Cornelis, 1985, Manual of Mineralogy, 20th ed., John Wiley and Sons, New York {{ISBN|0-471-80580-7}} {{Wiktionary}} {{Commons category}} [[Category:Inosilicates]] [[Category:Calcium minerals]] [[Category:Magnesium minerals]] [[Category:Iron(II) minerals]] [[Category:Asbestos]] [[Category:Amphibole group]] [[Category:Monoclinic minerals]] [[Category:Minerals in space group 12]] [[Category:Gemstones]]
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