The crystal structure of the high-pressure polymorph meyerhofferite, ideally Ca 2 B 6 O (OH) 10 ·2(H O), has been determined by means single-crystal synchrotron X-ray diffraction data. Meyerhofferite undergoes a first-order isosymmetric phase transition to meyerhofferite-II, bracketed between 3.15 and 3.75 GPa, with large volume discontinuity. is marked an increase in coordination number boron ...