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Fossils
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What is a Fossil? Traces or remains of living things from long ago. There are 2 main types of fossils: Original remains Rock fossils
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Original Remains
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Original Remains Fossils that are the actual bodies or body parts of organisms. There are 3 modes of preservation: Ice Amber Tar
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Ice Ice is one of the best preservers of the remains of prehistoric life. Huge ice fields in Siberia and Alaska contain 10,000 year-old mammoths.
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Amber Amber forms from resin, a sticky substance inside trees that flows like syrup and protects the tree by trapping insects.
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Tar Original remains of animals have also been found in places where there are pools of tar – a thick, oily substance.
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Rock Fossils
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Rock Fossils If an organism is covered by or buried in sediment, it may become a fossil as the sediments become rock. There are 4 main types of fossils that we find in rocks: molds and casts, petrified wood, carbon films and trace fossils
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Molds & Casts A mold is a visible shape that has left after an animal or plant was buried in sediment and then decayed away. A cast fossil is a solid model in the shape of the organism.
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Petrified Wood The stone fossil of a tree is called petrified wood.
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Carbon Films Carbon is an element that is found in every living thing. Sometimes when a dead plant or animal decays, its carbon is left behind as a visible layer.
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Trace Fossils Trace fossils are not parts of an animal or impressions of it, but rather evidence of an animal’s presence in a given location. Trace fossils include: footprints, trails, animal holes, and even feces.
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Fossil Formation
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How Do Fossils Form? Conditions have to be just right for a fossil to form in rock – the organism must be preserved before it decomposes or disappears. Rock fossils form in sedimentary rock. Why not in igneous rocks?
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