EARTH SCIENCE MONDAY Flashcards
chronological measurement that relates stratigraphy to time.
GEOLOGIC TIME SCALE
glaciation in northern hemisphere
PLEISTOSCENE
100 million years
PERIOD
billions of years
EON
several 100 million years
ERA
millions of years
AGE
mammals and birds begin to replace dinosaurs
PALEOSCENE
humans dominate Earth
HOLOCENE
tens of millions of years
EPOCH
flowering plants begin their domiance
CRETACEOUS
age of dinosaurs and ammonites
JURASSIC
abundant swamps that created coal deposits
PEENSYLVANIAN
abundant land plants and animals
MISSISSIPIANS
age of fishes and brachiopods
DEVONIAN
age of trilobites
CAMBRIAN
1.3 billions years ago first rocks found at sterling hill formed. A majority of life invisible to the naked eye
PROTEROZOIC EON
age of prokaryotes. aLL life invisible to the naked eye
ARCHEAN EON
extraterrestrial information indicates a high - temperature earth adverse to life.
HADEAN EON
earliest part of earth . newly formed planet beginning to cool
HADEAN ERA (4.6 - 4.0 BYA )
plate tectonics allowed crystal building and the formation of volcanic belts and sedimentary basins
ARCHAEAN ERA ( 4.0 - 2.5 BYA )
means early life
PROTEROZOIC
the rifitng of the continental crust and its subsequent filling with sedimentary volacanics rocks occured
PROTEROZOIC ERA ( 2500 MYA - 540 MYA )
means old life
PALEOZOIC
means middle life
MESOZOIC
means new life
CENOZOIC
beginning of life
PALEOZOIC (540 MYA - 260 MYA )
indicated the sudden abundance of complex organisms with hard parts in the fossil record . also known as cambrian explosion
PALEOZOIC ERA
age of dinosaurs . various dinosaur species dominated the planet. New trees and conifers appeared and mammals began to emerge
MESOZOIC ERA ( 245 MYA - 66 MYA )
known as age of recent life. Youngest era and has the most complete geological record of rocks. Life forms continued to become more complex
CENOZOIC ERA ( 66 MYA TO PRESENT TIME )
protons plus neutrons
MASS NUMBER
protons
ATOMIC NUMBER
2 protons / neutrons are emitted and new eleemnt were formed
ATOMIC DECAY
time needed for half of a sample of a radioactive substance to undergo changes
HALF LIFE
eleemnts with same protons but different neutron
ISOTOPES
positively charge
PROTONS
parent isotopes that are unstable
RADIOACTIVE ISOTOPES
unstable and decays
PARENT
stable and doesnt decay
DAUGHTER
determining numerical age of rocks using radioactive decay
ABSOLUTE DATING
radioactive isotopes found in fossil or rocks are used
RADIOMETRIC DATING
used for fossils
CARBON 14
used for rocks
URANIUM 238
isotopes are?
10 NATURAL 19 ARTIFICIAL
potassium argon dating
POTASSIUM 40 / 100 K YEARS
uranium lead dating
URANIUM 238 / 10 MIL YEARS
rubidium strontium
RUBIDIUM 87/ 10 MIL YEARS
carbon 14 dating
CARBON 12 - 14 / 50 K YEARS