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Geologic Time

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Term
Definition
Law of superposition   undisturbed layers get younger as you go up  
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principle of original horizontality   all beds originally deposited in water form close to horizontally  
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principle of cross-cutting relationship   when a fault cuts through rock, the rock is younger  
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inclusions   pieces of one rock unit contained within another  
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conformable   strata sequence that is undisturbed  
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unconformities   gaps in geologic time that indicate erosion, deformation  
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disconformities   large gap in geologic time due to processes of erosion  
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angular unconformities   younger strata overlie an erosion surface on tilted or folded rock  
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nonconformities   igneous or metamorphic magma chamber intrudes, then erosion erodes  
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petrification   turn to stone (LOOKS LIKE WOOD)  
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replacement   cell membrane are removed and replaced with mineral matter  
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mold   reflects the shape and surface marking  
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cast   a mold that is filled in with mineral matter and solidified  
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carbonization   carbon film left behind after organism decay (PLANT)  
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impression   carbonization process, carbon lost and replica of surface  
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amber   resin from trees, insects are preserved (WHOLE ORGANISM)  
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tracks   animal footprints in sediment later solidified  
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coprolites   fossil poo and stomach contents that were preserved  
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gastroliths   polished stomach stones  
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burrows   tubes in sediment, wood, or rock made by an animal  
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rock and fossil correlation   matching of rock layers from one location at the same time to another location  
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principle of fossil succession   older rock contain fossils that are increasingly different from modern species  
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fossil assemblage   several different species found together in a specific rock unit  
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index fossil   well defend morphological characteristics (short-lived species and widespread distribution  
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radiometric dating   calculating the absolute ages of rock and minerals that contain radioactive isotoped  
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alpha emission   atomic #= -2 mass # -4  
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beta emission   atomic #= +1 mass # unchanged  
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electron capture   atomic # = -1 mass #= unchanged  
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half-life   time required for half of the nuclei in a sample to decay  
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radiocarbon dating   date recent events (carbon -14)  
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half life of carbon014   5730 yrs  
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half life of uranium-238   4.5billion years  
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numerical dating   actual number of yrs  
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how do geologists numerically date rocks   radioactive decay  
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relative dating   events in their proper sequence  
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biggest era   paleozoic  
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present era   cenozoic  
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present eon   phanerozoic  
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present epoch   holocene  
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present period   quaterary  
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what eon means visible life   phanerozoic  
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uniformitarianism   the physical chemical and biological laws that operate today have also operated in the geologic past (long history of earth)  
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catastrophism   earth's landscape has been developed by worldwide disasters (over a short span)(catastrophism does not require assumptions of long timelines)  
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Created by: miabegic2
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