Editing Mineral (section)

====Inosilicates====
[[File:Asbestos with muscovite.jpg|left|thumb|[[Asbestiform]] [[tremolite]], part of the amphibole group in the inosilicate subclass]]
Inosilicates consist of tetrahedra repeatedly bonded in chains. These chains can be single, where a tetrahedron is bound to two others to form a continuous chain; alternatively, two chains can be merged to create double-chain silicates. Single-chain silicates have a silicon:oxygen ratio of 1:3 (e.g. [Si<sub>2</sub>O<sub>6</sub>]<sup>4−</sup>), whereas the double-chain variety has a ratio of 4:11, e.g. [Si<sub>8</sub>O<sub>22</sub>]<sup>12−</sup>. Inosilicates contain two important rock-forming mineral groups; single-chain silicates are most commonly [[pyroxene]]s, while double-chain silicates are often [[amphibole]]s.<ref>{{harvnb|Chesterman|Lowe|2008}}, p. 537</ref> Higher-order chains exist (e.g. three-member, four-member, five-member chains, etc.) but they are rare.<ref>{{cite web|url=http://webmineral.com/strunz/strunz.php?class=09&subclass=09.D|title=09.D Inosilicates|publisher=Webmineral.com|access-date=2012-08-20|archive-date=2017-07-02|archive-url=https://web.archive.org/web/20170702022444/http://webmineral.com/strunz/strunz.php?class=09&subclass=09.D|url-status=live}}</ref>

The pyroxene group consists of 21 mineral species.<ref name="DG112" /> Pyroxenes have a general structure formula of XY(Si<sub>2</sub>O<sub>6</sub>), where X is an octahedral site, while Y can vary in coordination number from six to eight. Most varieties of pyroxene consist of permutations of Ca<sup>2+</sup>, Fe<sup>2+</sup> and Mg<sup>2+</sup> to balance the negative charge on the backbone. Pyroxenes are common in the Earth's crust (about 10%) and are a key constituent of mafic igneous rocks.<ref>{{harvnb|Dyar|Gunter|2008}} pp. 612–13</ref>

Amphiboles have great variability in chemistry, described variously as a "mineralogical garbage can" or a "mineralogical shark swimming a sea of elements". The backbone of the amphiboles is the [Si<sub>8</sub>O<sub>22</sub>]<sup>12−</sup>; it is balanced by cations in three possible positions, although the third position is not always used, and one element can occupy both remaining ones. Finally, the amphiboles are usually hydrated, that is, they have a hydroxyl group ([OH]<sup>−</sup>), although it can be replaced by a fluoride, a chloride, or an oxide ion.<ref>{{harvnb|Dyar|Gunter|2008}}, pp. 606–12</ref> Because of the variable chemistry, there are over 80 species of amphibole, although variations, as in the pyroxenes, most commonly involve mixtures of Ca<sup>2+</sup>, Fe<sup>2+</sup> and Mg<sup>2+</sup>.<ref name="DG112">{{harvnb|Dyar|Gunter|2008}}, p. 112</ref> Several amphibole mineral species can have an [[asbestiform]] crystal habit. These asbestos minerals form long, thin, flexible, and strong fibres, which are electrical insulators, chemically inert and heat-resistant; as such, they have several applications, especially in construction materials. However, asbestos are known carcinogens, and cause various other illnesses, such as [[asbestosis]]; amphibole asbestos ([[anthophyllite]], [[tremolite]], [[actinolite]], [[grunerite]], and [[riebeckite]]) are considered more dangerous than [[chrysotile]] serpentine asbestos.<ref>{{harvnb|Dyar|Gunter|2008}}, pp. 611–12</ref>