earth time Flashcards

1
Q

principle of uniformitarianism

A

processes seen today are the same as those of the past

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2
Q

relative ages

A

based upon order of formation
qualitative method
older vs younger relationships

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3
Q

numerical ages

A

actual number of years since event
quantitative method

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4
Q

original horizontality

A

sediments settle out of a fluid by gravity
sediments accumulate horizontally, not favoured on slope

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5
Q

principle of superpositio

A

younger strata on top, older on bottom

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6
Q

principle of lateral continuity

A

strata form laterally extensive horizontal sheets
erosion dissects one-continuous layers
flat rocks unlikely to have been disturbed

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7
Q

principle of cross-cutting relations

A

faults, dikes, erosion must be younger than the material that is faulted, intruded, or eroded

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8
Q

principle of baked contacts

A

iegnous intrusion cooks invaded country rock
baked rock must have been there first (older)

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9
Q

principle of inclusions

A

rock fragment within another
inclusions older than enclosing material
fragments older than igneous intrusion

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10
Q

principle of fossil succession

A

fossils preserved in sedimentary rocks
they are time markers for relative age-dating
specific fossils found within limited time span
correlate strata locally regionally and globally

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11
Q

unconformities

A

time gap in rock record

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12
Q

angular unconformity

A

huge gap in time
horizontally parallel strata of sedimentary rock are deposited on tilted and eroded layers, producing an angular discordance with the overlying horizontal layers

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13
Q

nonconformity

A

igenous/metamorphic rocks capped by sedimentary rock
I or M rocks exposed by erosion then sediment deposited on eroded surface

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14
Q

disconformity

A

parallel strata bounding non deposition
interruption/pause in sedimentation

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15
Q

correlating formations

A

formations can be traced over long distances
lithologic (rock type) and fossil correlation

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16
Q

geologic maps

A

William Strata Smith noted that strata could be matched across distances. similar rock types in similar order

17
Q

geologic column

A

A geologic column is a record of the rock layers in a particular area across geologic time

18
Q

stratigraphic correlation

A

formations can be traced over long distances
overlap is sequences of rock types
overlapping rock columns used to build composite

19
Q

what is numerical age based on?

A

radioactive decay of atoms in minerals
decay proceeds at known fixed rate
radioactive elements act as internal clocks

20
Q

isotopes

A

elements that have varying number of neutrons.
stable: isotopes don’t change
radioactice: isotopes that spontaneously decay

21
Q

radioactive decay

A

progresses along decay chain. decay creates new unstable elements that also decay until reaching stable element endpoint

22
Q

parent and daughter isotope

A

parent: isotope that undergoes decay
daughter: product of this decay

23
Q

half life

A

time for half of unstable nuclei to decay
characteristic of each isotope
as parent disappears, daughter “grows in”

24
Q

isotopic dating

A

age of mineral determined by measuring ratio of parent to daughter isotopes. calculating time with known half life

25
Q

uranium lead dating

A

most trusted decay system for dating
determines the age of rocks and minerals by measuring the ratio of uranium to lead isotopes in a sample

26
Q

what does an isotope date mean?

A

gives time a mineral cooled below its closure temperature (when magma or lava cooled to become rock)
sedimentary rocks cannot be directly dated, but their minerals can

27
Q

other numerical ages

A

growth rings
rhythmic layering

28
Q

how old is oldest sandstone?

A

zircon
4.4 Ga