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Scientist who studies the Earths’ processes and history that have shaped it. |
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Geologic Time Scale
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A record of the geologic events and life forms in Earth’s history. |
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Divisions of Geologic Time Scale |
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Based on large, profound geologic changes to life forms Ex. eons, eras, and periods |
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Four main divisions of Geologic Time Ex. Precambrian, Paleozoic, Mesozoic, Cenozoic |
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Earliest era of Earth's history where single cell organisms (like bacteria) and simple multicellular organisms lived. |
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"Middle Life", often known as Age of Dinosaurs |
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"Ancient Life", when organisms started in water but transitioned into amphibians where they lived on land and in water; dense trees |
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"Recent Life", often known as Age of Mammals and first evidence of humans |
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Preserved remains or traces of living things |
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Hollow area in sediment that is in the shape of an organism |
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Solid copy of an organism |
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Minerals replace all or part of a once living organism Ex. petrified wood |
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Carbon Film Fossil
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Extremely thin carbon layer leaving the picture of a bug or leaf |
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Perserved Remains
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All of organism is trapped Ex. bug in amber, frozen mammoth |
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Fossil showing activity or evidence of a living organism |
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Method where geologists compare different layers of rock to determine an age |
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Rule that the oldest layer of rock will always be on the bottom layer |
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Rock that forms from lava that cools; younger than the rocks it is on top |
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Rock formed from cooling lava; always younger than any layer other rock layers |
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Crust, Mantle, Outer Core, Inner |
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Method of relative dating that compares ice layers to determine the age and atmosphere existing when ice froze |
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Method where geologists use radioactive dating to put dates on rock layers |
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Isotope used to determine the age of younger or once living materials |
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Isotope to date older materials; half life is 4.3 billion years |
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Amount of time it takes for an isotope to decay 50% |
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When a radioactive atom loses particles and gives off energy |
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Original isotope before material decays |
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Isotope remaining whenever the parent element experiences decay |
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When an element has the same number of protons and electrons, but a different number of neutrons |
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