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Fossils and evolution
Rates of deposition of sediments
Cooling of the Earth from a molten state
Radiometric Dating
Methods for Estimating the Age of the Earth
Radiometric Dating of Rocks
1896-1898
Radioactivity discovered by:
Henri Becquerel and Marie and Pierre Curie.
Phenomenon of Radioactivity
Some elements, such as uranium (U) and thorium (Th), are unstable:
They decay spontaneously.
Age of the Earth
Geologic Time Scale
The Atom
NaCl
Na = silvery metalCl = poisonous gas
NaCl = Salt
2
1
8 7 8 2
11 protons 17 protons
Examples of Atomic Numbers
Element Number of Protons
Na 11
Cl 17
C 6
N 7
O 8
Fe 26
U 92
Phenomenon of Radioactivity
Some elements, such as uranium (U) and thorium (Th), are unstable:
They decay spontaneously.
Uranium Nucleus
spontaneously emits a particle from its nucleus called an alpha particle (2 protons + 2 neutrons).
Alpha Particle
emits a particle from its nucleus called an alpha particle (2 protons + 2 neutrons).
Uranium - Thorium Decay
U He + Th238
92
4
2
234
90
spontaneous
decay
“parent” “daughter product”
alpha particle =2 protons + 2 neutrons = positively charged ion of Helium
Thorium:90 protons + 144 neutrons
Beta Particle Emission
But, Th is also unstable, and it emits a beta particle …
234
90
Th + Pa234
90
234
91
Thorium - Protactinium Decay
beta particle
beta particle = an electron discharged from the nucleus when a neutron splits into a proton and an electron
Protactinium:91 protons + 143 neutrons
Title
beta particle = an electron discharged from the nucleus when a neutron splits into a proton and an electron
U PbSeries
This process is called radioactive decay, and eventually uranium (parent) decays to lead (daughter product).
U PbSeries
The rate at which this process occurs is measured in terms of the “half life”.
Half Life
Half Life = Number of years for 1/2 of the original number of atoms to decay from U to Pb
The phenomenon of radioactivity relates to our story about the age of the Earth in two ways:
(1) As radioactive elements decay in the Earth, they heat up the surrounding rocks.
(2) Radiometric Dating
As radioactive elements decay in the Earth, they heat up the surrounding rocks.
So, there is a source of heat inside the Earth that Kelvin didn't know about.
Thus: While the Earth was cooling off, it was also being heated up (due to radioactive decay in its interior), and the Earth took much longer to cool than Kelvin thought.
Radiometric Dating
Assume: Rate of decay (half life) of long-lived elements has not varied since the Earth was formed.
This is an example of uniformitarianism.
The Principle of Uniformitarianism
The physical, chemical and biological laws that operate today have also operated in the geologic past.
To estimate the age of a rock:
D = amount of daughter product. P = amount of parent.
For a particular radioactive element in a rock, determine the present ratio = D/P.
D
P
Rate of decay (from theory and measurement)
Make assumptions about original ratios (from theory of geochemistry).
As time passes, the amount of parent decreases, and the amount of daughter product increases. This provides a way of estimating the amount of time since the "clock" got started (i.e., since the rock solidified).
D
P
D
P
Title
Potassium - Argon Dating
Electron Capture
Title
Electron Capture
Potassium - Argon Dating
K/Ar clock begins when K bearing minerals crystallize in a rock.The new minerals will contain K40, but will not contain Ar40 (because Ar40 does not combine with other elements).
As time passes:K40 Ar40 (half-life = 1.3 billion years)
K40/Ar40 ratio can be measured to determine age
Uniformitarianism
Potassium - Argon Dating
K40/Ar40 ratio can be measured to determine age.
K40 Ar40 (half-life = 1.3 billion years)
K40/Ar40 > 1 less than 1.3 billion years oldK40/Ar40 = 1 1.3 billion years old
K40/Ar40 < 1 more than 1.3 billion years old
Half-Lives of Radioactive Isotpes
Examples of Very Old Rocks Found on Earth:
3.4 billion year old granites - South Africa.
3.7 billion year old granites - Greenland.
Oldest terrestrial rocks > 3.8 billion years.
Oldest terrestrial rocks (4.0 billion years?) are deep in the interiors of continents.
Oldest terrestrial rocks (4.0 billion years?) are deep in the interiors of continents.
But, rocks on the Earth have been weathered, metamorphosed and recycled through a very dynamic planet.
Thus, the Earth's earliest rocks have been recycled, and we need to look beyond Earth to find evidence of when the Earth solidified.
Plate Tectonics
Rock Cycle
Mountain Building
and Erosion
Oldest terrestrial rocks (4.0 billion years?) are deep in the interiors of continents.
Similar Rock Structures
The Earth's earliest rocks have been weathered, metamorphosed and recycled through a very dynamic planet.
We need to look beyond Earth to find evidence of when the Earth solidified.