A study of apatite crystals from the Asio mine, Japan, showed sectoral
texture related to the growth of the crystal, and with optically biax
ial properties within the sectors. Wet chemical analysis gave a compos
ition Ca5(PO4)3(F0.64,OH0.38,Cl0.01)1.03 for the specimen. Additional
diffraction spots were not observed in precession and oscillation X-ra
y photographs and electron diffraction photographs. Since the internal
textures correlate with the surface growth features, it is suggested
that the internal textures and the unusual optical properties were pro
duced during nonequilibrium crystal growth. The fluorine/hydroxyl site
s in hexagonal apatite are symmetrically equivalent in the solid cryst
al but, at a growth surface, this equivalence may be lost, resulting i
n a reduction of crystal symmetry. Heating of the apatite to about 850
-degrees-C results in the almost complete disappearance of the optical
anomalies due to disordering, which may be related to the loss of hyd
roxyl from the crystal.