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EARTH HISTORY

YOU WILL LEARN HOW THE EARTH HAS CHANGED AND LEARN A THEORY THAT EXPLAINS MANY OF THESE CHANGES.

AB
PANGAEASUPERCONTINENT FORMED AT THE END OF THE PALEOZOIC ERA
FOSSILSRECORDS OF ANCIENT LIFE
ABSOLUTE AGEACTUAL AGE OF A ROCK
GEOLOGIC TIME SCALESEQUENCE OF EVENTS ON EARTH BASED ON THE ROCK RECORD
PLATE TECTONICSPRESENT THEORY OF CONTINENTAL MOVEMENT
SUPERPOSITIONPRINCIPLE THAT YOUNGER ROCK LAYERS ARE DEPOSITED OVER OLDER LAYERS
INDEX FOSSILSFOSSILS OF ORGANISMS THAT LIVED ONLY AT A PARTICULAR TIME BUT IN MANY PLACES
UNCONFORMITYA BURIED EROSION SURFACE
RELATIVE AGEA ROCK'S AGE COMPARED TO OTHER ROCKS
PALEOMAGNETIC DATINGDETERMINING ROCKS' AGES BY STUDYING THE ALIGNMENT OF MAGNETITE GRAINS
SEAFLOOR SPREADINGPROCESS THAT CREATES NEW OCEAN PLATE MATERIAL AT MID-OCEAN RIDGES
UNIFORMITARIANISMIDEA OF CONTINUOUS CHANGES CREATING THE EARTH'S GEOLOGIC FEATURES
RADIOMETRIC DATINGMETHOD FOR FINDING THE ABSOLUTE AGE OF A ROCK USING RADIOACTIVITY
CORRELATIONFINDING OUT HOW ROCKS AT DIFFERENT LOCATIONS COMPARE IN AGE
FORMATIONROCK UNIT USED FOR CORRELATION
ERALARGEST DIVISION OF THE GEOLOGIC TIME SCALE
TRILOBITESIMPORTANT INDEX FOSSIL OF THE PALEOZOIC ERA
MESOZOIC ERAPANGAEA BEGAN TO BREAK APART
CENOZOIC ERAEVIDENCE OF HUMAN LIFE


Ms. Shryock

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