The sequence of events leading to the preservation of dinosaur tracks is explained diagrammatically in this illustration. First of all a dinosaur traversed an area of soft sediment, leaving its footprints as it did so (diagrams a and b). It might, for example, have walked across the mudflats of an ancient estuary, leaving its tracks in the wet sediment exposed by the falling tide. The next rising tide might deposit more sand and mud over the newly formed footprints (diagram c), and once they were buried in this way they would be largely protected from the destructive effects of sun, wind and water. Continued accumulation of sediments would result in deeper burial of the footprints, and the consequent changes in pressure, temperature and water chemistry would bring about the complex process of lithification, or the transformation of soft wet sediment into harder and drier rock. The layers of sediment would be compressed and reduced in thickness; the water would be squeezed out from between the grains of sand and mud, which would be packed more tightly and, in many instances, cemented by mineral deposits. Ultimately, the lithified sediments would be raised by earth-movements and exposed by erosion. The layers of rock containing the footprints might then be exposed in hillsides, river beds, cliffs, quarries or roadside cuttings. Finally, those layers might be split open, by natural weathering or by an inquisitive fossil-hunter, to reveal the ancient footprints (diagram d).