Bone is one of the many biological tissues characterized by the still poorly defined process of mineralization, that is, by the deposition of inorganic substance in their organic matrix, and is one that, chiefly due to its important biological functions, but also because of its widespread presence in primates and its easy availability, has been investigated for hundred of years by thousand of investigators (see reviews by [1-3]). Its study, however, is a demanding task, because of the complexity and variability of the tissue-factors that derive mainly from differences in its histological types, biochemical composition, phases of maturation, and degree of mineralization (the terms 'mineralization', 'biomineralization', and 'calcification' are treated as equivalents in this paper; see Bonucci [2]). These differences, although recently emphasized [4-5], have not always received due recognition. In this connection, revealing indicative examples include, for instance, the differences between the compact, lamellar bone and spongy, woven bone [4], or between the dense rostrum bone of toothed whales [6] and the medullary bone of birds [7]. These differences may lead to incorrect interpretations of apparently contrasting results, but may also lead to new insights if they are recognized to derive from distinctive traits of tissues belonging to the same broad type, which is what they are. The concepts that follow, which chiefly focus on the local mechanism of matrix calcification, mainly refer to woven bone, which raises fewer technical issues than compact bone, but they are valid for, and can be extended to, all other types of bone and hard tissue. 2. Historical notes So much research has been carried out on bone mineralization that it is hard to provide an inclusive summary; moreover, research of this kind is often interlaced with that on other cal