The age of a fossil relative to other fossils can be determined by where in
relation to each other the fossils are found in rock strata. The absolute age of
a fossil can be found through radioactive dating.
Fossils are formed when a piece of bone or other material is buried by sediment.
Over long periods of time, chemicals from the surrounding rock leach into the
object until only a rock shaped like the original object is left.
The chemical make-up of rocks can tell us what environmental conditions may have
been like. They can tell us what kinds of gases may have been in the
atmosphere, how much moisture was in an area, or if any cataclysmic events
occurred, such as volcanic eruptions or meteor strikes.
Fossilization is a rare event. An object must remain in the right kind of
conditions undisturbed for a very long time for a fossil to form. Once formed
many fossils are lost to the crushing action of geological movements or to
erosion of rock faces.