absolute time benefits: –tell you how old something is. –if two ages are known for different...
TRANSCRIPT
Absolute Time How do you measure time? How do geologists measure time? Requirements
Process that occurs at aconstant rate
Method of keeping acumulative record of thatprocess
Absolute Time• Benefits:
– Tell you how old something is.– If two ages are known for different events
then you can calculate the time between to see how long the process took for the rocks to form.
• Difficulties– Dates are difficult to obtain due to type of
testing.– Testing is expensive ( $400 / hr for lab
work)
TREE RINGS
Each year is usually represented by a single ring.
This method is good to about 5000 years ago. (bristle cone pines of the Sierra Nevadas in California are among the oldest trees.
TREE RINGS
By starting with trees today and working backwards a record in tree rings can be made- this has proven very successful with the dating of Southwestern Indian ruins.
•The cultures would use trees in their roof beams.
•By taking a core out of these roof beams and matching them to a record of tree rings, scientists can tell when the tree was cut.
Tree Rings
• Annual growth rings are a function of their environment, i.e. temperature, humidity, precipitation, insects, fires, etc.
• Limited to recent geologic past (furthest back 8000 years)
Rings also give a record to weather patterns. This will also tell you years of drought.
•Wide distance between rings is a wet, good growing year.•Short distance between rings is a dry, poor growing year.
Varves deposited in a glacial-age lake in southern Connecticut. Each pair of layers in a sequence of varves represents an annual deposit. Light-colored silty layers were deposited in summer, and the dark-colored clayey layers accumulated in winter.
A section of gypsum "varves" from the Permian Castile Formation near Carlsbad New Mexico
Ice Layers
• Ice Sheets in Greenland and Antarctica record annual changes in accumulation and snowmelt
• Records up to 65,000 years
• Ice also traps volcanic ash which can be radiometrically dated
• Record climatic conditions of the Earth
Ash Layers
• Ash Layers from major volcanic eruptions create KEY BEDS – a distinct layers of known age
Absolute Dating
Determining the exact age of a rock or
fossil through radiometric dating
Radioactive atoms are like clocks
All minerals contain some radioactive atoms
Only works for IGNEOUS rocks
Radiometric Dating
• Radioactive decay – naturally-occurring radioactive materials break down into stable materials at known rates(parent material to daughter material)
• Determining absolute age based on ratio of parent to daughter material
Half-Life•The time it takes for half of
the parent material to decay into the daughter material.
•Each radioactive isotope has its own unique half-life.
•Amount of parent material decreases by one half each half-life.
Half-LifeParent
(radioactive)Daughter (stable)
# of half-lives that have passed
20 atoms 0 atoms 0
10 atoms 10 atoms
5 atoms
2.5 atoms
Determining # Half-Lives
Half-life Example #1
• You start with $1000 in your bank account
• Every week your spouse or boyfriend/girlfriend removes half of the money
• The half-life of your account = 1 week
• Questions to think about:– When is the most money taken out?– Will the amount in your bank account ever go to
zero?
Your Bank Account
• Start: $1000• Week 1: $500• Week 2: $250• Week 3: $125• Week 4: $62.50• Week 5: $31.25• Week 6: $15.63• Week 7: $7.81• Week 8: $3.90• Week 9: $1.95
• Week 10: $0.98• Week 11: $0.49• Week 12: $0.24• Week 13: $0.12• Week 14: $0.06• Week 15: $0.03• Week: 16: One and a
half cents left in your bank account
How radiometric dating works
1. Measure the amount of radioactive parent material.
2. Measure the amount of stable daughter material.
3. Determine the number of half lives that have passed.
4. Multiply half lives by rate of decay (given).
Radiometric Dating Limitations• Sedimentary Rocks
– Weathered material of other rocks– Radiometric clock has been altered
• Metamorphic Rocks– Radiometric clock has been altered?
• Igneous Rocks– Minerals form when rock forms – No Problem – best source for radiometric dating
Try these1. 30 parent atoms, 10 daughter
atoms, h-l = 5,000 years. How old is it?
2. 15 parent atoms, 45 daughter atoms,h-l = 1.3 billion years. How old is it?
3. 1 parent atom, 15daughter atoms,h-l = 100,000 years. How old is it?
Types of Radiometric DatingCarbon-14
• Carbon-14 found in humans, plants, animals
• Constantly decays to C-12, but is replaced
• When object dies, no new C-14, ration unbalanced
• Used for “younger” items - <50,000yrs
Types of Radiometric Dating
Uranium-Lead Method• Uranium-238 decays to Lead-206• Half-life is 4.5 billions years• Used on objects older than 10
million years
Types of Radiometric Dating
Potassium-Argon• K-40 decays to Ar-40• Half-life of K-40 is 1.3 billion years• Used for rocks older than 100,000
years
Types of Radiometric Dating
Fission Track Dating• Charged particles are given off
during radioactive decay• Leave a trail of damage known as
fission tracks• The number of tracks is a function
of age
Carbon 14 Only useful in finding the age of ORGANIC materials up to 75,000
years old.
How Carbon-14 Is Produced
Cosmic Rays (radiation)
Collision with atmosphere (N14)
Forms C-14 C-14 combines with oxygen to form carbon dioxide (CO2)
Carbon-14 Life Cycle
14
6
14
7
14
7
Cosmic radiation
Carbon-14 is produced in the atmosphere
Carbon-14 decays into Nitrogen-14
Starting the Carbon Dating ClockOnce a plant or animal dies the
clock starts
Organism dies
No more C-14 intake
Organism dies
No more C-14 intake
C-14 continues to decay
C-14 continues to decay
Determining the Starting Amount• There are two types of carbon used in the dating
process: C-12 and C-14• C-12 is a stable isotope (it does not decay)
• When an organism is alive it has the same ratio (C-12 to C-14) that is found in the atmosphere (1-trillion to 1)
Same ratio
I’m alive
Different ratio
I’m a fossil
Amount of stable C-12
Amount of unstable C-14
Ratio Years Dead
# Half-lives
100 Trillion 100 1-T to 1 0 0
100 Trillion 50 2-T to 1 5,730 1
100 Trillion 25 4-T to 1 11,460 2
100 Trillion 12 8-T to 1 17,190 3
100 Trillion 6 16-T to 1 22,920 4
100 Trillion 3 32-T to 1 28,650 5
How the C-12 / C-14 Ratio Works