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The Rock and Fossil Record

This actvity will help you learn the vocabulary for this chapter

AB
uniformitarianisma principle that states that the same geologic processes shaping the Earth today have been at work throughout Earth's history
catastrophisma principle that states that all geologic change occurs suddenly
relative datingdetermining whether an object or event is older or younger than other objects or events
superpositiona principle that states that younger rocks lie above older rocks in undisturbed sequences
geologic columnan ideal sequence of rock layers that contains all the known fossils and rock formations on Earth arranged from oldest to youngest
unconformitya surface that represents a missing part of the geologic column
absolute datingthe process of establishing the age of an object, such as a fossil or rock layer, by determining the number of years it has existed
isotopesatoms of the same element that have the same number of protons but have a different numbers of neutrons
radioactive decaya process in which radioactive isotopes tend to break down into stable isotopes of other elements
radiometric datingdetermining the absolute age of a sample based on the ratio of parent material to daughter material
half-lifefor a particular radioactive sample, the time it takes for one-half of the sample to decay
fossilany naturally preserved evidence of life
permineralizationa process in which minerals fill in pore spaces of an organism's tissues
petrificationa process in which an organism's tissues are completely replaced by minerals
trace fossilsany naturally preserved evidence of an aminal's activity
coprolitespreserved feces, or dung, from animals
molda cavity in the ground or rock where a plant or animal was buried
castan object created when sediment fills a mold and becomes rock
index fossila fossil of an organism that lived during a relatively short, well-defined time span; a fossil that is used to date the rock layers in which it is found
geologic time scalea scale that divides Earth's 4.6-billion-year history into distinct intervals of time
eonthe largest division of geologic time
erathe second-largest division of geologic time
periodthe third-largest division of geologic time
epochthe fourth-largest division of geologic time


Mrs. Belair

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