GEOLOGIC TIME Flashcards
2 dating techniques geologists use to
- relative ages = geologic events placed in chronological order based on their position in the geologic record
- absolute ages = ages calculated for geologic events
examples of geologic events in earths history
- 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
principles used to determine the relative age of geologic events
- principle of uniformitarianism - physical processes observed today operated in the same way as geological past
- principle of superposition - in a sequence of layered rocks, the oldest lies on bottom and youngest on top
- principle of original horizontality - most sedimentary rocks were originally horizontal so if tilted its due to subsequent geological event
- principle of original lateral continuity - sedimentary beds originally laterally continuous so if in separate units its due to erosion
- principle of cross cutting relations - younger features cut across older ones
- principle of inclusions - an older rock fragment within another
- principle of baked contacts - thermal metamorphism occurs when country rock is invaded by a plutonic igneous intrusion - baked rock must be older
what 2 assumptions does fossil succession depend on
- no two species are exactly alike
- species never reappear once extinct
whats an index fossil
- distinctive
- wide geo distribution
- restricted to a narrow time interval
- provides reliable correlations between stratigraphic units
whats an unconformity
a time gap in the rock record
- non deposition or soil formation
- erosion
3 types of unconformities
- disconformity - parallel strata bracketing nondeposition - interruption in sediment
- nonconformity - sedimentary strata overlay metamorphic / igneous rocks
- angular unconformity - rocks below the unconformity were folded / tilted
2 types of stratigraphic correlation used by geologists
- lithologic correlation - based on rock type - limited to nearby regions
- fossil correlation - based on fossils within rocks - can apply to much broader areas
4 time blocks that the geologic column is divided into
- eons (largest subdivision of time)
- eras
- periods
- epochs
*each one is a subdivision of the one above it
what era makes up the majority of earths geological history
Precambrian (88%)
significant geological events on earth
- 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
names of the eons
- 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
names of the ears
- paleozoic - “ancient life”: life diversified rapidly
- mesozoic - “middle life”: age of dinosaurs
- cenozoic - “recent life”: age of mammals
relative vs absolute age
- 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)
isotopes
same protons, different neutrons
- unstable ones decay overtime
what is radiometric dating
measure amount of parent + daughter isotopes to determine age
what is half time when referring to isotopes
time it takes for half of unstable parent atom to decay to stable daughter atoms
- happens exponentially
how does radiometric dating vary with different rocks
- 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
other ways to determine numerical ages without radiometric dating
- growth rings - trees, shells
- rhythmic layering - annual layers in ice / sediment
- magnetostratigraphy - compare megnetic signitures in strata to global reference scale
3 oldest rocks on earth
- Acasta Gneisses
- Issua supracrustal belt
- Single zircon crystals
how was age of earth determined
4.57 Ga
- based on correlation with moon rocks + meteorites