25 
Greenland.—The pyrope^ or Bohemian garnet, 
in rounded grains, &c.—The common garnet^ the 
predominant colours of which are brown and 
green: among these may be mentioned the 
variety which, from its resemblance to resin, is 
'called colophonite. To this also belongs the 
elegant variety from Kamschatka, denominated 
grossidar^ on account of the resemblance which 
its separate crystals bear to a gooseberry.—Tra¬ 
pezoidal and emarginated crystals of the black 
garnets, called melanile^ found particularly in the 
neighbourhood of Frascati.—The allochroite^ also 
called splintery garnet, from Drammen in Nor¬ 
way.—The aplome^ whose dodecahedral crystals 
differ from those of the garnet in being streaked 
in the direction of the short diagonal of their 
rhomboidal planes.—The cmnamon-stone from 
Ceylon, a mineral which was supposed to contain 
zirconia, till a more accurate analysis proved it 
to be a substance nearly allied to garnet and 
vesuvian; some polished pieces of the same, being 
the true hyacinth.—Among the specimens of 
vesuvian or idocrased^Q more conspicuous are the 
large beautiful crystals (the unibinaire of Haiiy) 
discovered by Laxmann on the banks of the Vilui 
in Kamschatka, imbedded in a steatitic rock; 
those from Vesuvius, where this substance occurs 
accompanied by other volcanic ejections, have, 
in Italy, obtained the appellation of volcanic 
gems, hyacinths, and chrysolites.— Gehlenite ,— 
In this case, though not very closely allied to 
the garnet tribe, is also deposited the stauroUte 
(called 
SALOON. 
Nat, Hist. 
