The crystal structure of amesite -2H(1) from the Postmasburg Mn ores o
f South Africa has been refined to R = 4.7% using Siemens P4 rotating-
anode MoK alpha X-ray data and SHELXL-93 software. Partial ordering of
tetrahedral Si,Al and especially of octahedral Mg,Al has reduced the
ideal P6(3)cm symmetry to triclinic PI (refined as CI). Tetrahedral ro
tation of 15 degrees moves the basal oxygens toward the octahedral cat
ions in the same layer but away from the OH H-donors of the next layer
s. The ordering pattern of Al-IV and Al-VI is unique in that the locus
of Al-rich sites consists of 2 intersecting sets of zigzag lines para
llel to X-2 and X-3, plus 2 Al-rich octahedra in layer 2 instead of th
e usual 1 site.