The lanthanide silicate, La 9.33 Si 6 O 26 , which has the hexagonal apatite structure (P6 3 /m), was investigated at high pressure. A subtle phase transition was observed at ~13.3 GPa by in situ synchrotron x-ray diffraction (XRD) and confirmed by infrared absorption (IR) and Raman scattering measurements. The high-pressure phase has a structure similar to that of the initial hexagonal apatite structure, but the symmetry is reduced to P6 3 through the displacement of one oxygen site and tilting of the SiO 4 tetrahedra. Interestingly, the highpressure phase has an abnormally lower compressibility, which is caused by the change in symmetry that allows the tilting of the SiO 4 tetrahedra, and the bulk modulus of the highpressure phase is only half that of the apatite structure.2