EUCLASE, a very rare mineral, occasionally cut as a gem-stone for the cabinet. It bears some relation to beryl in that it is a silicate containing beryllium and aluminium, but hydrogen is also present, and the analyses of euclase lead to the formula HBeAlSiOs or Be(A10H)SiO4. It crystallizes in the monoclinic system, the crystals being generally of prismatic habit, striated vertically, and terminated by acute pyramids. Cleavage is perfect, parallel to the clinopinacoid, and this suggested to R. J. Haiiy the name euclase, from the Greek eB, easily, and xXiiais, fracture. The ready cleavage renders the stone fragile with a tendency to chip, and thus detracts from its use for personal ornament. The colour is generally pale-blue or green, though sometimes the mineral is colourless. When cut it resembles EUCLID certain kinds of beryl (aquamarine) and topaz, from which it may be distinguished by its specific gravity (3-1). Its hardness (7-5) is rather less than that of topaz. Eudase occurs with topaz at Boa Vista, near Ouro Preto (Villa Rica) in the province of Minas Geraes, Brazil. It is found also with topaz and chrysoberyl in the gold-bearing gravels of the R.
\nSanarka in the South Urals; and is met with as a rarity in the mica-schist of the Kauris in the Austrian Alps.
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