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Pyrophyllite
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{{short description|Aluminium silicate hydroxide phyllosilicate mineral}} {{Infobox mineral | name = Pyrophyllite | category = [[Silicate minerals]] | boxwidth = | boxbgcolor =#dfce9d | image = Pyrophyllite-118706.jpg | imagesize = 260px | caption = Pearly radial cluster of pyrophyllite from Hillsborough District, Orange County, North Carolina (Size: 11 × 7.3 × 6.6 cm) | formula = Al<sub>2</sub>Si<sub>4</sub>O<sub>10</sub>(OH)<sub>2</sub> | IMAsymbol = Prl<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 = 360.31 g/mol | system = [[Monoclinic]]<ref name=Mindat/> or [[triclinic]]<ref name=Webmin/> | class = Prismatic (2/m) <br/>or pinacoidal ({{overline|1}}) | symmetry = ''C2/c'' or ''C{{overline|1}}'' | unit cell = a = 5.16 Å, <br/>b = 8.966(3) Å, <br/>c = 9.347(6) Å; α = 91.18°, <br/>β = 100.46°, γ = 89.64°; Z = 2 | color = Brown green, brownish yellow, greenish, gray green, gray white | habit = Compact spherulitic aggregates of needlelike radiating crystals; as fine grained foliated laminae, granular, massive | cleavage = [001] Perfect | tenacity = Flexible inelastic | mohs = 1.5–2 | luster = Pearly to dull | refractive = n<sub>α</sub>=1.534–1.556, n<sub>β</sub>=1.586–1.589, n<sub>γ</sub>=1.596–1.601 | opticalprop = Biaxial (−) | 2V = 53–62 | birefringence = δ =0.0450–0.0620 | pleochroism = | streak = white | gravity = 2.65 – 2.9 | melt = | fusibility = Infusible, exfoliates | diagnostic = | solubility = | diaphaneity = Translucent to opaque | other = | references =<ref name=Mindat>[http://www.mindat.org/min-3323.html Mindat]</ref><ref name=Webmin>http://webmineral.com/data/Pyrophyllite.shtml Webmineral</ref><ref name=Handbook>[http://rruff.geo.arizona.edu/doclib/hom/pyrophyllite.pdf Handbook of Mineralogy]</ref><ref name=Klein>Hurlbut, Cornelius S.; Klein, Cornelis, 1985, ''Manual of Mineralogy,'' 20th ed., p. 430 {{ISBN|0-471-80580-7}}</ref><ref>{{cite journal |last1=Lee |first1=J.H. |last2=Guggenheim |first2=S. |journal=American Mineralogist |volume=66 |year=1981 |pages=350–357 |title=Single crystal X-ray refinement of pyrophyllite-1Tc |url=https://pubs.geoscienceworld.org/msa/ammin/article-abstract/66/3-4/350/41261/Single-crystal-X-ray-refinement-of-pyrophyllite?redirectedFrom=fulltext |access-date=30 December 2020}}</ref><ref>{{cite journal |last1=Gruner |first1=J.W. |journal=Zeitschrift für Kristallographie |volume=88 |year=1934 |pages=412–419 |title=The crystal structures of talc and pyrophyllite|issue=1–6 |doi=10.1524/zkri.1934.88.1.412 |s2cid=101680970 }}</ref> }} '''Pyrophyllite''' is a [[Silicate minerals|phyllosilicate]] [[mineral]] composed of [[aluminium]] [[silicate]] [[hydroxide]]: Al<sub>2</sub>Si<sub>4</sub>O<sub>10</sub>(OH)<sub>2</sub>. It occurs in two forms ([[Crystal habit|habit]]s): crystalline folia and compact masses; distinct [[crystal]]s are not known. The folia have a pronounced pearly [[Lustre (mineralogy)|luster]], owing to the presence of a perfect cleavage parallel to their surfaces: they are flexible but not elastic, and are usually arranged radially in fan-like or spherical groups. This variety, when heated, exfoliates and swells up to many times its original volume. The color of both varieties is white, pale green, greyish or yellowish; they are very soft ([[Mohs hardness|hardness]] of 1.0 to 1.5) and are greasy to the touch. The [[specific gravity]] is 2.65–2.85. The two varieties are thus very similar to [[talc]].
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