While for many years zeolite crystallization has been assumed to proceed ma
inly through solution-mediated transformations, recent works point towards
the presence of heterogeneous events in both nucleation and crystal growth
steps. When the zeolite synthesis starts from a solid-containing gel, the p
articipation of the amorphous raw phase in the formation of the zeolite nuc
lei has been clearly established. Moreover, in some cases the zeolite cryst
als grow by reorganization of the hydrogel through solid-solid transformati
ons. In zeolite synthesis starting from clear solutions, the crystallizatio
n mechanism has been recently studied by in situ light scattering technique
s, showing the formation in the first stages of an X-ray amorphous gelatino
us phase, consisting of particles with sizes below 10 nm. These nanoparticl
es seem to be involved directly in the crystallization, as their aggregatio
n and subsequent densification have been proposed to lead to the formation
of the zeolite crystals. The crystallization of zeolites through heterogene
ous versus homogeneous pathways is favoured at high solid concentrations or
when the solubility of the silicate species is low, as occurs during zeoli
te synthesis through the fluoride route.