We examined human pineal concretions and found them to exhibit a multi
-layered concentric structure consisting of irregularly spaced dense a
nd sparse zones containing fine crystals. The hydroxyapatite crystalli
tes were shown to be irregularly outlined plate forms (measuring 11 si
milar to 70 nm in their longest dimension and 2 similar to 10 nm in th
ickness). At the center of each crystallite a central dark line was ob
served by means of high resolution electron microscopy. The structure
and size of the crystals were similar to those of dentin and bone. The
ground surface of the concretions was observed metallurgically by mea
ns of an electron probe microanalyzer (EPMA). The surface zones of the
concretions contained a higher concentration of zinc, which seems to
play an important role during the mineralization process, whereas calc
ium and phosphorus exhibited higher concentrations at the center.