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Types of Fossils

Fossils are evidence of past life. They are formed in many ways. After a plant or animal dies, its soft tissues usually decay or are eaten. Most fossils are formed when the hard parts are protected from decay by natural burial soon after the organism dies. For this reason, most fossils are found in sediments that were laid down by water - either ancient rivers, lakes, or oceans.

imprint of leaf


imprint of plant

small clam

therapod track

ammonite fossil

a claw


trilobite

hadrosaur leg bone




 


crocodile jaw

wasp in amber

giant mammoth (found in ice frozen for 10,000 years)


mammoth hair

tar pits
First the bones were saturated with asphalt, which stopped decay. Preservation of the fossils took place after the saturated bones had been buried beneath water-borne sediment. Unlike most fossils, the fossils from Rancho La Brea are unchanged, original material. 




 


shark teeth
coprolite
Links to great fossil pictures and information:

http://www.ammonite.ws/
http://www.envs.emory.edu/ichnology/dinotraces.html
http://www.coloradomtn.edu/campus_rfl/staff_rfl/kohls/eocene.html
http://tabla.geo.ucalgary.ca/~macrae/Burgess_Shale/
http://www.museum.vic.gov.au/dinosaurs/
http://www.uky.edu/KGS/coal/webfossl/pages/devonian.htm
Project Prosaurapod
Fossils of New Jersey