Lecture 5 Flashcards

1
Q

Cultural Views of time

A
  • Greek and Hindu ancient philosophers rejected finite time
  • proposed that time is cyclic with universe regenerated in cycles. Things that happen to day is part of the current cycle and one day in a new cycle the same things will happen again
  • Europ thought time was linear and finite history was drawn from the bible. Provided the first such time frame for science
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2
Q

Concept of human history

A
  • dates to Herodotus 6.484 BC
  • first attempt to research the past
  • used a list of pharaohs to do so
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3
Q

Biblical time line

A

CreationEnd of World

-importance was the production of a linear view with unique historical events on the finite time line

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4
Q

James Ussher

A
  • Bishop to Armagh in 1650
  • calculated biblical chronologies
  • calculated biblical record of births and deaths
  • result was dating the creation making Earth 6000 years old
  • Creation October 23, 4004 BC)
  • first no qualms with scientists, fossils only then being recognized as former living creatures
  • new explanation was that shells and bones found in rocks on mountains were from the flood
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5
Q

New Sciences of Earth

A
  • 18th Century
  • study of past life-paleontology
  • study of Earth physical nature and origin-geology and cosmology
  • both quickly outgrow Biblical time scale
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6
Q

Benoit de Maillet

A
  • wrote about mythical philosopher Telliamed who claimed to be telling about what Eastern philosophers thought
  • pointed out that places in sea level was going down
  • Telliamed calculated how long it would have taken for the mountains to rise from the sea=2mry
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7
Q

de Buffon

A
  • mid 1700s astronomers begun to realize that the sun and its planets had condensed from a swirling mass of hot gas-how long would it take a planet to cool?
  • Buffon tested with hot iron balls and extrapolated getting about 100,000 years
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8
Q

Relative time

A
  • time line that represents when something happened in relationship to something else
  • measure by relative position, before, after, same time
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9
Q

Absolute time

A
  • real time dates
  • how long ago something happened
  • measured in time units like years
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10
Q

Nicholas Steno

A
  • helped with understanding relative time
  • recognized and showed that fossils were remains of past life buried before mud became rock (tongue stones=shark teeth)
  • came up with general theory of how sediments accumulated
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11
Q

Principle of superposition

A
  • gives relative age of rocks
  • sediments accumulate on horizontal surface
  • later different sediments deposited
  • ultimately rocks form in layers going from oldest at the bottom and younger above
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12
Q

Superposition applied to relative dating of rocks

A
  • only a few kinds of sedimentary rocks

- sandstone, limestone, shale so it will occur in different ages

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13
Q

How to tell ages of rocks

A
  • take information from one location and fuse with information from another and come up with a rock section that you don’t see in any one place, but the order would be correct on earth
  • confined to individual strata
  • William Smith did this by carefully observing rocks and their fossils
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14
Q

Superposition and strata correlation

A
  • by use of index fossils in the 19th century used to map strata over wide regions of Europe and America
  • also developed relative scale that’s still in use
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15
Q

James Hutton

A
  • figured out from key geological observation how ancient the world would have to be to account for observation
  • saw tilted rock layers below and contact with overlying horizontal layers
  • since all rocks are deposited horizontally the rocks were shifted to have new rocks deposited on top
  • shifted rocks back to how they would be deposited and makes an order out of it showing oldest to youngest
  • saw infinite amount of time
  • eventually new horizontal segments will too be bent into mountains and cycle of erosion will begin again
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16
Q

Historical data showing age of Earth

A
  • buried forest sequences
  • Green River formation, remains a huge lake-2000 feet total lake deposited rock
  • rates of sediment deposition
  • evidence from geology shows sediments deposited over long time scale-no single flood accounts for deposition of Earth’s rocks
17
Q

Absolute time scale methods

A
  • 19th C: Lord Kelvin-calculation of life of sun (30-100 million years)
  • rate of sedimentation/thickness of rocks (75 million years)
  • rate of salt delivery to sea/salinity (100 million years)
  • present method: decay of radioactive isotopes
18
Q

Decay of Radioactive isotopes

A
  • elements are unstable and decay into radioactive isotopes
  • U235 will one day decay into Pb207 and He4
  • gives you way to date earth
  • half life: always takes same amount of time to decay by half and can be measured
  • Pb204 is non radiogenic
  • Pb is stable end product
19
Q

Radioactive decay date what?

A
  • only igneous rock

- because only sample where you know the age of all the parts because of measurable parent and daughter isotopes

20
Q

Rate law for radioactive decay

A

λ=log_eP_0/P_t

  • λ=decay constant
  • t=time elapsed
  • P_0=amount isotope in time t_0
  • P_t=amount isotope at time t
21
Q

Radiometric Age Equation

A
  • P_0=P_t+D_t
  • D=daughter isotope
  • substitute P_t+D_t for P_0 in P_t=P_0e^- λt so you can solve for t=1/ λ*log_e((D_t/P_t)+1)
  • all quantities on right hand of equation can be measured in the lab
22
Q

Assumptions for radioactive decay dating

A
  • igneous rock
  • rock contains measurable parent and daughter isotopes
  • half life comparable to age of rock being measured
  • closed system
  • must be able to estimate amount of daughter isotope at t=0
  • assume constant rate of decay over geological time
23
Q

isochron method

A
  • done in cases where some daugher isotope might already be present at =0.
  • some like Pb 206 and 207 existed when rocks formed
  • way of normalizing isotope content against isotopes of same element not part of the decay chain, e.g. Pb 204
  • from that the initial content of the decay product can be calculated with great accuracy
24
Q

Simple accumulation clock

A

40K——->40Ar

  • done with igneous rocks
  • as rock starts molten, no Ar gas present when it hardens and it starts to accumulate at that point
  • method useful for rocks of ages from a few to 100,000 years to a few billion
25
Q

Dating a sedimentary rock

A
  • Lava is 435 MY layer (top)
  • shale with fossil layer (middle)
  • lava 495 MY layer (bottom)
  • so the fossil must be between 495 MY and 435 MY old because of the dating of the lava
26
Q

Carbon 14 dating

A
  • special case
  • different than radioactive decay dating
  • When an individual dies, the C14 is still contained in the bones, however the organism is not still accumulating new C14 and what is there is decaying away
  • importance is that it can be applied directly to the subject, not just the surrounding rock layers
  • limitation: only young less than about 40,000 year-old specimens can be dated this way
27
Q

Age of earth

A
  • oldest existing rocks dated by radioisotopes go back 4 BY
  • meteors are fragments of material left over from formation of planets all dat 4.6 BY=the age of formation of the earth
  • geology has destroyed oldest rocks on earth but we do find rocks of that age on the moon