People can identify fossils by their shape, size, and texture. Fossils might closely resemble the bones or shells of modern organisms, but also exhibit distinctive features that indicate they are ancient. Additionally, the location where a fossil is found can provide clues about the type of organism it belonged to.
You can identify them by what IS the fossil. The 3 fossils are prints, coprolite, or smooth rocks corroded by gizzards.
Fossils can form by: Freezing Amber Asphalt Carbonization
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Fossils can form in various ways, including through petrification (minerals replace organic material), carbonization (leaving a carbon impression), molds and casts (where an organism leaves an imprint in sediment that hardens), and freezing or desiccation (preserving the organism in ice or dried conditions). Each method results in a unique type of fossil that provides valuable information about ancient life forms.
Body fossils are any fossil that comes from the animal itself. Examples of body fossils are fossilized skin, bone, teeth, claws, eggs, embryos etc. Trace fossils are any fossil connected to ancient life but not the animal itself. Examples include footprints, teethmarks, nests, gizzard stones, coprolites, burrows etc. In a lot of ways trace fossils are as important as body fossils. The give us insight into how the animal lived, how fast it walked, what ate what etc.
You can identify them by what IS the fossil. The 3 fossils are prints, coprolite, or smooth rocks corroded by gizzards.
In what ways are fossils useful to geologist?
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Fossils can form by: Freezing Amber Asphalt Carbonization
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1.) Low precipitation2.) Limited plant life 3.) Temperature extremes
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