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Chapter 5 Geologic History by: Natalie Bontrager

AB
UniformitarianismProcess today that are the same as they where along time ago
Law of superpositionyoungest rock layers on top; oldest rock layers on the bottom
Original HorizontalitySedimentary rocks are deposited in horizontal layers
Igneous IntrusionHot Liquid Rocks squeezes through all the other layers of rock
Igneous extrusionliquid rock squeezes through all the other layers of rock and out to the surface
FoldCrustal movement squeezes rock layers into curved layers
Recumbent FoldA fold Folds over on top of itself & puts younger layers under the older rock layers
Faulta break in the curst where movement occurs
Offset LayersLayers on opposite sides of a fault DO NOT line up
Contact MetamorphismRocks change from the heat of an igneous intrusion
eonLarge division of time
eraSubdivision of eon
epochSubdivision of a period
periodSubdivision of an era
Precambrian/PhanerozoicThe 2 major eons
Cenozoicmost recent era; means era of "most recent animals"
Mesozoic"age of reptiles"; middle era
Paleozoicera of the "ancient animals"
Correlationmatching
Index Fossilswide spread & short lived ( an animal lived all over the world but for a short amount of geologic time)
UnconformityBuried erosional surface; place where erosion has wiped out one or more layers
Submergence/DepostitionTime when land is under water & sediments are being left in horizontal layers
Uplift/ErosionTime when land is not covered by water & weathering agents are wearing away the land//creats unconformity
Radioactive DatingUsing radioactive istope half-lives to tell you how old something is
Carbon-14Used to date once living things less than 50,000 years old
Nitrogen-14A decay product of C-14


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