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Naturally preserved evidence of animal activity |
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| Examples include those found in amber, ice, tar/asphalt, and rocks or those made by petrifcation |
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| Fossil found only in a short geologic span of time. |
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| Remains of evidence of organisms preserved by geologic processes |
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| Is shaped inward or concave to a rock |
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| Examples include tracks, burrows, or coprolites. |
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| A cavity formed in a rock where a plant or animal was buried, usually by sediment. |
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| Fossilized marks showing movement of animals. |
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| Once an organism decayed, this would fill with sediment, eventually making a cast. |
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| Type of fossil used tro establish the age of rocks. |
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| Created when sediments or mineral sfill ahole left behind from a decaying organism. |
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| Naturally preserved evidence o flife. |
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| a rare fossil useful in matching age of rocks. |
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| this fossili useful in matching age of rocks. |
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| this fossil rock really looks like the outside of whatever was preserved |
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| determining the age of a rock in years |
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| typically involved radiometric dating, which uses knowledge of half-lives of elements in a rock sample. |
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| the idea that younger rock layers are above older rock layres, assuming they haven't been distrubed. |
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| since a geologic column is like a side view of layers of rocks, it is used for this scientific process. |
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| Law describing that older rocks are beneath the younger rocks in an undisturbed layer |
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| observing disturbed rock alyers, faults, magma intrusions, folding tiliting of rocks can all be usecd for this scientific process. |
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| the prinicple of superposition should be helpful with this scientific process. |
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| figuring out if a rock is older aor younder than other orcks or events taken place in a rock layer. |
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