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Barnett - Fossils and Stratigraphy

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Question
Answer
fossil   evidence or remains of once-living plants or animals  
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unaltered hard part   a bone or shell that has not undergone change since the organism's death  
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altered hard part   organic material is replaced with minerals  
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petrified   turned to stone  
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mold   impression left by an organism - a leaf or shell for example  
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cast   mold is filled with minerals  
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index fossil   used to correlate rock layers; easily recognized, abundant, and widespread geographically  
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trace fossil   indirect evidence of life, like a footprint  
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stratigraphy   the study of rock layers and the fossils they contain  
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uniformitarianism   forces and processes that we observe today have been at work for a very long time  
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original horizontality   sediments are laid down in horizontal layers  
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superposition   in undisturbed bedrock, the oldest rocks are at the bottom and the youngest rocks are on the top  
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cross-cutting relationship   intrusion, folding, or fault is younger than the rock it cuts across  
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unconformity   buried surface of erosion  
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relative age   puts the age of materials in order; puts events in a sequence  
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absolute age   gives the actual age of a material  
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isotope   atom that has a different number of neutrons in its nucleus than normal  
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half life   the amount of time it takes for half the parent material to decay to daughter material  
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parent material   the original, unstable isotope  
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daughter material   the stable isotope that results from radioactive decay  
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radioactive decay   spontaneous breakdown of nuclei of unstable isotopes  
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radiometric dating   using the process of radioactive decay to find the absolute date of a material  
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radiocarbon dating   finding the absolute age of a once-living organism using the carbon 14 decay process  
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dendrochronology   tree ring dating  
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Created by: ebarnett
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