One of the methods of bone dating. Fluorine-containing groundwater percolates through deposits, its fluorine becoming absorbed onto the crystal lattice of the mineral component of buried bones (in the same way that fluorine is adsorbed into the surface layers of teeth from repeated brushing with fluoride toothpaste). Given a constant rate of groundwater percolation, the concentration of fluorine in the bone should be proportional to its age. Bones from the same stratigraphical context can be dated relatively by comparison of their fluorine content. The Piltdown forgery was finally exposed by this method.
The Macmillan dictionary of archaeology, Ruth D. Whitehouse, 1983Copied