BOSTONITE  , in

petrology, a fine-grained, pale-coloured, grey or pinkish rock, which consists essentially of alkali-felspar (orthoclase, microperthite, &c.) . Some of them contain a small amount of interstitial quartz (quartz-bostonites); others have a small percentage of lime, which occasions the presence of a plagioclase felspar (maenite, gauteite, lime-bostonite) . Other minerals, except apatite, zircon and magnetite, are typically absent . They have very much the same composition as the trachytes; and many rocks of this series have been grouped with these or with the orthop,hyres . Typically they occur as dikes or as thin sills, often in association with nepheline-syenite; and they seem to bear a complementary relationship to certain types of lamprophyre, such as camptonite and monchiquite . Though nowhere very common they have a wide distribution, being known from Scotland, Wales, Massachusetts, Montreal, Portugal, Bohemia, &c . The lindoites and quartz-lindoites of Norway are closely allied to the bostonites .