absolute vs. relative dating. what is geology? geology is the study of the earth’s form and...
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Absolute vs. Relative Dating
What is Geology?
Geology is the study of the Earth’s form and composition and the changes it has undergone.
Why do we care?1. Rock record provides evidence of
geological events and life forms of the past.
2. Processes observed on Earth in the present also acted in the past.
3. Earth is very old and has changed over time.
Is the Earth changing now?Yes! Although many features of the Earth
may seem to be unchanging over our lifetime, they are still changing, but on time scales of hundreds, thousands or even millions of years.
This image shows Mount Hood in Oregon USA at the same time in late summer in 1985 and 2002.
How old is the Earth?
How old is the Earth?The universe is
13.7 billion years old
The sun is 5 billion years old.
The Earth is 4.6 billion years old.
The moon is 4.5 billion years old.
How do we know? Relative Dating
Absolute Dating
Relative DatingRelative Dating identifies which rock units
formed first, second, third and so on.
Relative dating determines the sequence in which events occurred, but not how long ago they occurred.
Relative DatingLaw of Superposition – each rock layer is
older than the one above it and younger than the one below it.
Usually applies to sedimentary rock, but can also be applied to lava flows and layers of ash from volcanic rock.
Relative DatingPrinciple of Original Horizontality – layers of
sediments are generally deposited in horizontal position.
Relative DatingPrinciple of Cross-Cutting – when a fault
cuts through rock layers, or when magma intrudes other rocks and hardens, then the fault or intrusion is younger than the rocks around it.
Absolute DatingAbsolute Dating identifies the exact age of
a rock.
Scientists use radioactive decay to determine the age of the rock.
Atom ReviewWhat are the subatomic particles of an
atom? ProtonElectronNeutron
Which subatomic particles make up the mass of the atom?ProtonsNeutrons
Radioactive DecayDuring radioactive decay, unstable atomic
nuclei spontaneously break apart, or decay, releasing energy.
Radioactive Decay
What is an isotope?Atoms of the same element can have
different numbers of neutrons; the different possible versions of each element are called isotopes.
For example, the most common isotope of hydrogen has no neutrons at all; there's also a hydrogen isotope called deuterium, with one neutron, and another, tritium, with two neutrons. Hydrogen TritiumDeuterium
Carbon Dating• Carbon-14 dating, is based on
the ratio of C-14 to C-12 in an organic sample less than 70,000 years old
• As long as the organism was alive, the ratio of carbon-12 to carbon-14 was in equilibrium with its environment.
• When the organism dies, the "clock" starts as the carbon-14 decays, changing the ratio
Radioactive DecayRadioactive isotopes decay until they are
stable.
Ex. Uranium-238 decays over time to form lead-206
Half LifeHalf life is the amount of time necessary for
one half of the nuclei in a sample to decay to its stable isotope.
Radiometric DatingRadiometric dating, also called radioactive
decay dating, is a way of calculating the absolute ages of rock that contain radioactive isotopes.
Practice Problems1. The half life of nickel is 100 years. If you
had 94 grams of nickel, how much would be left after 200 years?
1 half life = 100 years = 47 grams2 half lives = 200 years = 23.5 grams
Practice Problems2. Sodium-24 has a half life of 15 hours. How much
of a 440 gram sample of sodum-24 remains after 60 hours?
1 half life = 15 hours = 220 grams2 half lives = 30 hours = 110 grams3 half lives = 45 hours = 55 grams4 half lives = 60 hours = 27.5 grams
Practice Problems3. Iron-59 has a half life of 45 days. A murder
weapon was found in a lake and the original weapon was reported to have contained 1,200 grams of iron. After 6 months (180 days), the original sample decayed. How much iron-59 was left?
1 half life = 45 days = 600 grams2 half lives = 90 days = 300 grams3 half lives = 135 days = 150 grams4 half lives = 180 days = 75 grams
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