GEOLOGICAL TIME Flashcards

1
Q

o Absolute age dating

A

(radiometric dating)
 Decay products of radioactive elements in minerals to get absolute ages
* Igneous rocks, metamorphic rocks

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2
Q

o Relative age dating

A

(this is older than that)
 Steno’s principles

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3
Q

principle behind half-life

A

– isotopes are variants of the same parent atom, differing in #of neutrons,

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4
Q

o Formula- measured by ratio of parent to daughter

A

 N(t) = N0(1/2) ^t/t1/2

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5
Q

half-life

A

the time required for half of the radioactive nuclei in a sample to decay

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6
Q

o Nonconformity

A

 A boundary between non-sedimentary rocks (below) and sedimentary rocks (above)
* Occurs when time passes before deposition og the next layer
* Layer is eroded.

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7
Q

disconformity

A

 A boundary between two sequences of sedimentary rocks where the underlying nest have been eroded (no tilted) prior to the deposition of the younger ones

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8
Q

o Angular unconformity

A

 A boundary between two sequences of sedimentary rocks where the underlying ones have been tilted or folded and eroded prior to the deposition of the younger ones

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9
Q

o Para conformity

A

 A time gap in a sequence of sedimentary rocks that does not show up as an angular unconformity or a disconformity

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10
Q

different types of unconformities

A

nonconformity
disconformity
angular unconformity
para conformity

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11
Q

o What determines a time boundary (4)

A

 Appearance of new species
 Extinction events
 Shifts in ciliate
 Natural catastrophes

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12
Q

o Hadean eon (4.54-4.0 Ga)

A

 No evidence of life
 Differentiation of earths layers
 Development of atmosphere and oceans

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13
Q

o Archean eon (4.0-2.5 Ga)

A

 Oldest known fossils
 Free oxygen not available
 First continents form

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14
Q

o Proterozoic eon (2.5Ga- 451 Ma)

A

 Great oxygenation event
 Protocontinents accrete and form supercontinents
 Snowball earth ~700Ma
 First microscopic and macroscopic multicellular life ~550 Ma
 First eukaryotes
 Cambrain explosion

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15
Q

o Phanerozoic eon (541 Ma- present)

A

 Marked by the Cambrain explosion and the diversity of life forms
 Paleozoic, Mesozoic, and Cenozoic mean old, middle and new life

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16
Q
  • Order the 3 eras that make up our current eon
A

o Paleozoic, Mesozoic, cenozoic

17
Q

eons

A

haden, archean, proterzoic, phanerozoic

18
Q

mass extinctions

A

o End-ordovician
o End-devonian
o End-permian
o End-triassic
o End-cretaceous

19
Q

o End-ordovician

A

rapid melting of glacier

20
Q

o End-devonian

A

rapid climate change, O2 levels change and volcanic activity

21
Q

end- permian

A

extreme volcanic activity (siberian LIP)

22
Q

end triassic

A

splitting of pangea - CO2 volume

23
Q

end cretaceous

A

meterite impact

24
Q
A