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7E6.4 A Earth’s Evolution

AB
PangaeaA "super-continent" that was a single landmass about 260 million years ago
Geologic Time Scalechronological model of the geologic history of Earth using the divisions of time- eon, eras, periods and epochs
Law of SuperpositionPrinciple that States that the youngest layers or rock lay above the older layers of rocks if they have not been distrubed
intrusive igneous rockMolten rock from the earth's interior that pressed to the existing rock and cools.
FaultA crack in the earth's crust along which blocks of crust slide in relation to each other.
Plate TectonicsExplains how the large pieces of the outermost layer of the earth(continents), called plates, move and change shape.
Mold FossilIs formed when sediment becomes rock leaving a cavity in the shape of the body
Cast FossilForms when a mold is filled with sand or mud which hardens in the shape of the body
Petrified FossilWhere minerals replace the buried remains, and change them in rock
Preserved FossilForms when entire organisms or parts of organisms are prevented from decaying due to be trapped in rock, ice, tar, or amber
Trace FossilForms when mud or sand hardens in stone where a fingerprint, trail, or burrow of a body had been left behind cylinders
Ice CoreIce cylinders that are drilled of polar glaciers and ice sheets. They provide information on how the climate of the earth and the atmosphere has changed over time.
eons, eras, periods, epochsthe order of time divisions from large to small
Eonsthe largest division of geologic time
Foldingthe bending of rock layers due to stress



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