GEOLOGIC TIME Flashcards

1
Q

2 dating techniques geologists use to

A
  • relative ages = geologic events placed in chronological order based on their position in the geologic record
  • absolute ages = ages calculated for geologic events
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2
Q

examples of geologic events in earths history

A
  • deposition of sediment and formation of rock strata
  • erosion of crust such that a gap is formed in the record of past events
  • intrusion of igneous rocks
  • faulting of crust rocks
  • deformation of crust rocks
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3
Q

principles used to determine the relative age of geologic events

A
  1. principle of uniformitarianism - physical processes observed today operated in the same way as geological past
  2. principle of superposition - in a sequence of layered rocks, the oldest lies on bottom and youngest on top
  3. principle of original horizontality - most sedimentary rocks were originally horizontal so if tilted its due to subsequent geological event
  4. principle of original lateral continuity - sedimentary beds originally laterally continuous so if in separate units its due to erosion
  5. principle of cross cutting relations - younger features cut across older ones
  6. principle of inclusions - an older rock fragment within another
  7. principle of baked contacts - thermal metamorphism occurs when country rock is invaded by a plutonic igneous intrusion - baked rock must be older
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4
Q

what 2 assumptions does fossil succession depend on

A
  1. no two species are exactly alike
  2. species never reappear once extinct
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5
Q

whats an index fossil

A
  • distinctive
  • wide geo distribution
  • restricted to a narrow time interval
  • provides reliable correlations between stratigraphic units
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6
Q

whats an unconformity

A

a time gap in the rock record
- non deposition or soil formation
- erosion

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7
Q

3 types of unconformities

A
  • disconformity - parallel strata bracketing nondeposition - interruption in sediment
  • nonconformity - sedimentary strata overlay metamorphic / igneous rocks
  • angular unconformity - rocks below the unconformity were folded / tilted
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8
Q

2 types of stratigraphic correlation used by geologists

A
  • lithologic correlation - based on rock type - limited to nearby regions
  • fossil correlation - based on fossils within rocks - can apply to much broader areas
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9
Q

4 time blocks that the geologic column is divided into

A
  • eons (largest subdivision of time)
  • eras
  • periods
  • epochs
    *each one is a subdivision of the one above it
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10
Q

what era makes up the majority of earths geological history

A

Precambrian (88%)

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11
Q

significant geological events on earth

A
  • 3.8 Ga : life first appear on earth - anaerobic single celled orgs
  • 2 Ga : oxygen from cyanobacteria
  • 700 Ma : evolution of multicellular life
  • 542 Ma : hard shells
    ___precambrian - Cambrian boundary___
  • cambrian explosion
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12
Q

names of the eons

A
  • Hadean - “hell” (oldest): formation of ocean + second atmos
  • Archean - “ancient”: continents + early life formed
  • Proterozoic - “ealrier life” : tectonic plates + atmospheric O2 for multicellular life
  • Phanerozoic - “visible life”: Cambrian boundary + hard shells
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13
Q

names of the ears

A
  • paleozoic - “ancient life”: life diversified rapidly
  • mesozoic - “middle life”: age of dinosaurs
  • cenozoic - “recent life”: age of mammals
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14
Q

relative vs absolute age

A
  • relative = chronostratigraphic (but doesn’t tell us how long ago they occured)
  • absolute = numerical age before present - most common used is radiometric age dating (use of radioactive decay to date rock)
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15
Q

isotopes

A

same protons, different neutrons
- unstable ones decay overtime

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16
Q

what is radiometric dating

A

measure amount of parent + daughter isotopes to determine age

17
Q

what is half time when referring to isotopes

A

time it takes for half of unstable parent atom to decay to stable daughter atoms
- happens exponentially

18
Q

how does radiometric dating vary with different rocks

A
  • best rock type for radiometric dating = igneous rocks - contains both parent and daughter isotopes
  • metamorphic rocks = can be tricky - drives daughter isotopes out as it recrystalizes
  • ## sedimentary rocks = not possible - its grains derive from weathering of pre existing rocks, not the sedimentary rock itself
19
Q

other ways to determine numerical ages without radiometric dating

A
  • growth rings - trees, shells
  • rhythmic layering - annual layers in ice / sediment
  • magnetostratigraphy - compare megnetic signitures in strata to global reference scale
20
Q

3 oldest rocks on earth

A
  • Acasta Gneisses
  • Issua supracrustal belt
  • Single zircon crystals
21
Q

how was age of earth determined

A

4.57 Ga
- based on correlation with moon rocks + meteorites