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How old is it

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Title: How old is it


1
How old is it?
2
4.5 Billion years old
  • 4,500,000,000 years

3
But - how do we
know that?
4
Archbishop Ussher of Ireland1664
  • Heaven and Earth, Centre and substance were made
    in the same instant of time and clouds full of
    water and man were created by the Trinity on the
    26th day of October, 4004 B.C at 900 in the
    morning.

5
1750 -Molten Earth modelGeorges de Buffon
  • Earth was originally molten and cooled to present
    surface temperature
  • 75,000 years.

6
This seemed too young
  • Darwin - Beagle voyage in 1830s
  • Hutton - Uniformitarianism
  • The present is the Key to the past.

7
Late 1800sLord Kelvin
  • Reworked the cooling model using rock properties
    instead of iron.
  • 20-40 million years

8
1893 - sedimentary rock recordCharles Walcott.
USGS
  • Used typical sedimentation rates
  • Tried to calculate thickness of all rocks
  • 75 million years

9
1899 - ocean salinityJohn Joly, physicist
  • Assumed all oceans were originally pure
  • How long would it take to get to present
    salinity?
  • 100 million years

10
1900s - radioactive elements discovered
  • Uranium - Henri Becquerel
  • Marie and Pierre Curie - radium

11
Radioactivity
A radioactive isotope is one with an unstable
nuclear configuration
12
The structure of an Atom
  • All atoms are built from the same basic
    components.
  • Protons and neutrons are found in the nucleus.
  • Electrons are found in orbits around the nucleus.

13
Radioactive decay involves the emission of
radiation.
  • Alpha decay - loss of 2 protons and 2 neutrons
  • Beta decay - loss of electrons or positrons
  • Gamma decay - electromagnetic radiation - similar
    to X-rays

14
The unstable parent nucleus decays to a stable
daughter nucleus
  • This decay is not random, but is a statistical
    phenomenon that follows the laws of probability.
  • (like a coin toss)

15
Half Life
  • The length of time required for half of a certain
    number of parent atoms to decay to daughter
    atoms.

16
Half life
17
Ratio of parent / daughter
  • Uranium 235 decays to Lead 207
  • Half life is 704 million years.
  • If the ratio of U235 Pb 207 is 13
  • Age 2 704 ma 1408 ma

18
  • Uranium 238 to Lead 206. 4.5 billion years
  • Uranium235 to Lead 207 704 million years
  • Potassium 40 to Argon 40 1.3 billion
    years
  • Carbon 14 to Nitrogen 14 5730 years

19
Potassium-Argon Dating
  • Potassium-Argon dating is the only viable
    technique for dating very old archaeological
    materials.
  • Why?
  • Geologists have used this method to date rocks as
    much as 4 billion years old.

20
Problems with Potassium-Argon Dating
  • Argon 14 is a gas
  • When rocks are heated to the melting point, any
    Ar-40 contained in them is released into the
    atmosphere.
  • When the rock re-crystallizes it becomes
    impermeable to gasses again.
  • As the remaining K-40 in the rock decays into
    Ar-40, the gas is again trapped in the rock.
  • Which age are we recording?

21
Other methods typically used for working out dates
  • Dendrochronology
  • Magnetic Dating
  • Thermoluminescence
  • Fission Track Dating

22
Dendrochronology
  • Tree Ring Dating

23
  • Trees show annual growth rings that can be easily
    counted.
  • This technique can give dates to around 10,000
    years ago.

24
Bristle Cone Pines
  • The oldest Bristle Cone discovered so far was
    4,900 years old
  • Many are 4,000 years old.
  • These trees were already 2000 years old during
    the time of the Cesars.

25
Magnetic Dating
  • The direction and strength of the Earths
    magnetic field is constantly changing.
  • Field fixed in molten stone or fired clay.

26
Paleomagnetism
  • Correspondence between the locked magnetic
    polarities of different layers of lava flows and
    the magnetic-reveral time scale

27
Fission Track Dating
  • fission track analysis is widely used as a means
    of dating minerals
  • Observing the tracks made in objects by the
    fission fragments of the uranium nuclei that they
    contain.
  • Objects are irradiated with neutrons to induce
    fission then the density and number of the tracks
    before and after irradiation is noted to estimate
    the time that has elapsed since the object
    solidified.
  • Objects can be dated to 10,000,000 years old

28
Fission Track Dating
29
Carbon 14 in the Atmosphere
  • Carbon 14 undergoes constant decay.
  • C14 ratios remain relatively stable in the
    atmosphere.
  • C14 is constantly formed in the upper atmosphere.

30
Carbon 14 Decay to Nitrogen 14
  • Carbon 14, an unstable isotope of Carbon, loses
    an electron and decays into Nitrogen.

31
Carbon 14 and Living Things
  • Organisms are constantly replenishing their
    carbon and so while living maintain the same C14
    ratios as found in the atmosphere.

32
Exponential Decay of Carbon 14
  • ½ of the Carbon 14 decays every 5730 years

33
Practical use of Carbon 14
  • Bison from Ornee Caves in Niaux, France
  • Dated by Carbon 14 technique to be 13,000 years
    old
  • Objects can be dated as old as 70,000 years old

34
Cited Figures
  • Magnetic dating and spreading plates
    http//www.kie.berkeley.edu/ned/data/E01-971212-00
    8/E01-971212-008.html
  • Bristle Cone Pine http//web.utk.edu/grissino/i
    mages/bcp.jpg
  • Growth Rings http//emuseum.mnsu.edu/archaeology/
    dating/images/tree_ring.gif
  • Magnetic dating by period http//geomag.gly.fsu.e
    du/parker/1000/seis/1000seis.htm
  • Exponential Decay of C14 http//carbon14.univ-lyo
    n1.fr/courb2.gif
  • C14 in the atmosphere http//www.cnde.iastate.edu
    /ncce/RT_CC/Sec.2.4/c-14b.gif
  • Carbon 14 Decay to Nitrogen 14
    http//sol.sci.uop.edu/jfalward/nuclearphysics/ca
    rbon14decay.JPG
  • Bison from Ornee Caves in Niaux, France
    http//www.laradioactivite.com/pages/05_laboratoir
    e/01_methodes_d.htm
  • Thermoluminescence test http//www.yang-guifei.co
    m/Welcome.html
  • Fission Track Dating http//bullard.esc.cam.ac.uk
    /hobro/fission_image_hires.gif
  • Potassium-Argon Dating http//anthro.palomar.edu/
    time/images/potassium_argon_dating.gif
  • Radioactivity http//www.wps.com/archives/FilmStr
    ips/Effects-of-Fallout/atoms-are-unstable.GIF
  • The structure of an Atom http//info.fuw.edu.pl/f
    estiwal/2001/struny/czastki/atom.gif
  • Radioactive decay http//earth.leeds.ac.uk/dynami
    cearth/dating/decay.gif
  • Carbon 14 and Living Things http//jan.ucc.nau.ed
    u/wittke/GLG100/Carbon14.jpg
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