“…during the calculus formation~Takeda & Ishikawa, 1983;Harrison et al, 1997;Riesco et al, 1999!. Calcification may then be further assisted by factors such as saliva composition~Westhofen et al, 1984;Grases et al, 2003! andretention in the ductal system~Harrison et al, 1997;Teymoortash et al, 2002Teymoortash et al, , 2003 A "silent" growth period following the core formation stage is thought to generate the multilayered structure observed in most sialoliths. After this growth stage, the process eventually culminates at an inflammatory episode that determines the clinical symptoms and leads to the detection and surgical removal of the calculus~Faure et al, 1986!. Laminated structures of bright and dark layers have been reported by several authors and, in fact, seem to constitute the major organization type during growth~Faure et al., 1986;Riesco et al, 1999!. The alternating heavily calcified and organic layers are thought to result either from a rhythmic deposition of minerals similar to a Liesegang phenomenon~Anneroth et al, 1975, 1978! or from a simpler and slow sequential deposition of layers during the course of the silent growth period~Faure et al, 1986!.…”