​STAUROLITE, a mineral consisting of basic aluminium and ferrous iron silicate with the formula HFeAl 5 Si 2 0i 3 . The material is, however, usually very impure, the crystals enclosing sometimes as much as 30 or 40% of quartz and other minerals as well as carbonaceous matter. Crystals are orthorhombic and have the form of six-sided prisms. Interpenetrating cruci- form twinned crystals are very common and characteristic; they were early known as pierres de croix or lapis crucifer, and the name staurolite, given by J. C. Delametherie in 1792, has the same meaning (Greek, aravpos, a cross, and Xi0os, a stone). In fig. 1 the twin-plane is (032) and the two prisms intercross

An image should appear at this position in the text. If you are able to provide it, see Wikisource:Image guidelines and Help:Adding images for guidance.

Fig. 1. 'Fig. 2.

Twinned Crystals of Staurolite.

at an angle of 91 22'; in fig. 2 the twin-plane is (232) and the prisms intercross at nearly 6o°. The mineral is translucent to opaque and dark reddish-brown in colour; it thus has a certain resemblance to garnet, and on this account has been called grenatite. Waterworn pebbles of material sufficiently trans- parent for cutting as gem-stones are occasionally found in the diamantiferous sands of Brazil. The hardness is 7^ and the specific gravity 3-75. Staurolite is a characteristic mineral of crystalline schists, and it is also a product of contact-meta- morphism. Large twinned crystals with rough surfaces a.re found in mica-schist in Brittany and at several places in the United States, e.g. in Fannin county, Georgia. Untwinned crystals, translucent and of a rich brown colour (grenatite), are abundant in the silvery white paragonite-schist of Monte Campione, St Gothard.  (L. J. S.)