worksheet 2 Flashcards

1
Q

what is relative dating

A

determining dates of geological units in relative sense (this comes before this… and this comes after this…)

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2
Q

what is absolute/numerical datng

A

provides actual date of how old rock/feature is

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3
Q

what is magnetic dating

A

dating of rock using reversals of Earth’s magnetic field to help determine age of rocks

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4
Q

what is radiometric dating

A

a strategy to determine the absolute age of rock using the ratios unstable isotopes in minerals and organic matter

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5
Q

what isotopes are good for absolate dating?

A

U-Pb (Uranium Lead), Rb-Sr (Rubidium-Strontium), Th-K (Thorium-Potassium) and K-Ar (Potassium-Argon)

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6
Q

can we use radiocarbon dating for old rocks?

A

no bc short half life so really only works for things ~<50,000 years old

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7
Q

what isotopes have really long half lives?

A

U-Pb or K-Ar

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8
Q

what is the equation for the number of remaining radioactive atoms when using radiocarbon dating?

A

N=N_0 e^(−λt)
N_0 is number of original radioactive atoms
λ is nuclide decay constant
λ= ln (2) / t^½
t^½ is the half life

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9
Q

what is the age equation and when is it used?

A

used for all dating when you do not have carbon
t= 1/λ * ln ( 1+ D / P )
D –> daughter isotopes
P –> parent isotopes
λ= ln (2) / t^½

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10
Q

what are possible assumptions made in radiometric dating?

A
  • no other factors altered amount of parent & daughter isotopes
  • no daughter isotopes existed at time zero
  • decay constant is actually a constant and doesn’t vary throughout time
  • parent and daughter isotopes can be accurately measured
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11
Q

what is the principle of superposition

A

in an undeformed sequence, the oldest rock is at the bottom and the youngest is at the top

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12
Q

what is the principle of originally horizontally

A

layers of sediment are deposited more or less horizontally

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13
Q

what is the principle of cross cutting relationships?

A

if a feature crosses multiple layers then it was formed after the features that it crosses

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14
Q

what is principle of faunal succession

A

fossil species succeed each other in a definitive recognizable order. one the species goes extinct, it will not appear as a fossil in a different time period

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15
Q

what are unconformities

A

surface that represents break in rock record due to deposition stopping and allowing erosion to occur and then deposition occurs again

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16
Q

what is an angular unconformity

A

when the underlying older rocks and the overlying younger rocks show angle to one another. the rocks below were tilted/folder and then there was weathering and then new rocks were deposited

17
Q

what is a disconformity

A

when the older rocks and the younger rocks are parallel but the contact plane (where they touch) is an erosional surface

18
Q

what is a nonconformity

A

when the underlying rocks are igneous or metamorphic (unstratified) and the overlying younger rocks are sedimentary (so they are stratified)

19
Q

what is biostratigraphy

A

using fauna and fossils to determine relative age of layer order and combine that with stratigraphic units

20
Q

how can biostratigraphy help us determine relative age

A

we can use the presence of absence of certain fossils and combine with the principle of faunal succession