By WILLIAM PHILLIPS, Esq.
member of the geological society.
The primitive crystal of quartz is considered to be an obtuse
rhomboid, of which the angles are given by Haüy in his “Tableau
comparatif,” &c. as being 94° 24′ and 85° S6′: that of the sulphate
of barytes is a quadrangular prism with rhombic terminations, the
angles of which according to the same authority are 101° 32′ 13″
and 78° 27′ 47″. The results of some attempts to verify these admeasurements
by subjecting the natural planes of the crystals of
both these substances, as well as some regular fragments of the latter,
to the reflecting goniometer, form the particular object of the present
communication.
The first attempts to ascertain by this means the angles of the rhomboid of quartz, were made upon some minute primitive crystals from Bristol: seven of these gave incidences on the one angle varying from 94° 12′ to 94° 17′, and on the other from 85° 44′ to 85° 52′; not more than two or three agreed. But the reflections
