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PHS ES Chp12
PHS ES Geologic Time Chapter 12
| Term | Definition |
|---|---|
| uniformitatianism | the concept that the processes that have shaped Earth in the geologic past are essentially the same as those operating today. |
| relative dating | process by which rocks are placed in their proper sequence or order, only the chronological order of events is determined, not the absolute age in years. |
| law of superposition | a law that states that in any undeformed sequence of sedimentary rocks, each bed is older than the layers above and younger than the layers below. |
| principle of original horizontality | a principle of relative dating; layers of sediments are generally deposited in a horizontal or nearly horizontal position. |
| principle of cross-cutting relationships | a principle of relative dating; a rock or fault is younger than any rock or fault through which it cuts. |
| unconformity | a surface that represents a break in the rock record, caused by erosion or lack of deposition |
| correlation | establishing the equivalence of rocks of similar age in different areas |
| extinct | term used to describe a type of organism that no longer exists anywhere on Earth |
| fossil | the remains or traces of an organism preserved from the geologic past. |
| principle of fossil succession | geologic principle stating that fossil organisms succeed one another in a definite order in the rock record. |
| theory of evolution | theory developed by Charles Darwin stating that all the different kinds of living things have changed over time. |
| natural selection | process by which characteristics that make an individual better suited to its environmnet become more common in a species. |
| adaptation | a trait that helps an organism survive and reproduce |
| index fossil | a fossil that is associated with a particular span of geologic time |
| radioactivity | the spontaneous decay of certain unstable atomic nuclei |
| half-life | the time required for one half of the atoms of a radioactive substance to decay |
| radiometric dating | the procedure of calculating the absolute ages of rocks and minerals that contain radioactive isotopes. |
| radiocarbon dating | method for determining age by comparing the amount of carbon-14 to the amount of carbon-12 in a sample. |
| geologic time scale | the division of Earth history into blocks of time - eons, eras, periods and epochs; the time scale was created using relative dating principles. |
| eon | the largest time unit on the geologic time scale, next in order of magnitude and above era. |
| precambrian time | the long time span from Earth's formation to the beginning of the Cambrian period; made up of the Hadean, Archaen, and Proterzoic eons. |
| era | a major division on the geologic time scale, Eras are divided into shorter units called periods. |
| period | a basic unit of the geologic time scale that is a subdivision of an era; periods may be divided into smaller units called epochs. |
| epoch | a unit of the geologic time scale that is a subdivision of a period. |