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Small scale permineralization can produce very detailed fossils.

Specimens are usually considered to be fossils if they are over 10,000 years old.

The observation in the 19th century that certain fossils were associated with certain rock strata led to the recognition of a geological timescale and the relative ages of different fossils.

to dinosaurs and trees, many meters long and weighing many tons.

A fossil normally preserves only a portion of the deceased organism, usually that portion that was partially mineralized during life, such as the bones and teeth of vertebrates, or the chitinous or calcareous exoskeletons of invertebrates.

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