29.3 a bsolute t ime. h istorical m ethods counting rigs in trees – more accurate, but cannot...

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29.3 ABSOLUTE TIME

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Page 1: 29.3 A BSOLUTE T IME. H ISTORICAL M ETHODS Counting rigs in trees – more accurate, but cannot calculate very old material

29.3 ABSOLUTE TIME

Page 2: 29.3 A BSOLUTE T IME. H ISTORICAL M ETHODS Counting rigs in trees – more accurate, but cannot calculate very old material

HISTORICAL METHODS

Counting rigs in trees – more accurate, but cannot calculate very old material.

Page 3: 29.3 A BSOLUTE T IME. H ISTORICAL M ETHODS Counting rigs in trees – more accurate, but cannot calculate very old material

HISTORICAL METHODS

Estimating rates of erosion and sedimentation – Only useful for younger geologic features.

Page 4: 29.3 A BSOLUTE T IME. H ISTORICAL M ETHODS Counting rigs in trees – more accurate, but cannot calculate very old material

HISTORICAL METHODS

Counting Varves – The sediments that form in bodies of water annually. (Optional) Ex. The glacial lakes deposit a like thin layer in the summer and a dark layer in the winter.

Page 5: 29.3 A BSOLUTE T IME. H ISTORICAL M ETHODS Counting rigs in trees – more accurate, but cannot calculate very old material

RADIOACTIVITY

Radioactive Decay – the process of an atomic nucleus losses E by emitting ionizing particles and radiation.

(Alpha, Beta & e- capture)

Page 6: 29.3 A BSOLUTE T IME. H ISTORICAL M ETHODS Counting rigs in trees – more accurate, but cannot calculate very old material

RADIOACTIVITY

Radioactive Decay Alpha Decay : An

alpha particle (2 e+ and 2 e-) are emitted.

Page 7: 29.3 A BSOLUTE T IME. H ISTORICAL M ETHODS Counting rigs in trees – more accurate, but cannot calculate very old material

RADIOACTIVITY

Radioactive Decay Beta Decay: A

neutron disintegrates into a e+ and a e- (beta particle)

Page 8: 29.3 A BSOLUTE T IME. H ISTORICAL M ETHODS Counting rigs in trees – more accurate, but cannot calculate very old material

RADIOACTIVITY

Radioactive Decay e- capture: A e+

captures an e- and becomes a neutron.

Page 9: 29.3 A BSOLUTE T IME. H ISTORICAL M ETHODS Counting rigs in trees – more accurate, but cannot calculate very old material

RADIOACTIVITY

Radioactive DecayAs decay continues

the atom becomes an isotope of a different element. Continues until it becomes a stable (non radioactive isotope).

Page 10: 29.3 A BSOLUTE T IME. H ISTORICAL M ETHODS Counting rigs in trees – more accurate, but cannot calculate very old material

RADIOACTIVITY

Radioactive Decay Parent Isotope –

Original element/atom

Daughter Isotope – product of the original.

Ex. C14->N14

Page 11: 29.3 A BSOLUTE T IME. H ISTORICAL M ETHODS Counting rigs in trees – more accurate, but cannot calculate very old material

HALF LIFE

The time it takes half an atoms radioactive material to decay to a stable product.

U 238 has a half life of 4.5 b.y.

Page 12: 29.3 A BSOLUTE T IME. H ISTORICAL M ETHODS Counting rigs in trees – more accurate, but cannot calculate very old material

RADIOMETRIC DATING

Radiometric DatingThe process of measuring the amount of parent and daughter material and using the ratio to find the age of the material. (Rocks, minerals and organic material)

Page 13: 29.3 A BSOLUTE T IME. H ISTORICAL M ETHODS Counting rigs in trees – more accurate, but cannot calculate very old material

RADIOMETRIC DATING

Radiocarbon Dating Using C12 and

C14 to date dead organisms. (not useful for organisms older than 70,000 y.o.)

Page 14: 29.3 A BSOLUTE T IME. H ISTORICAL M ETHODS Counting rigs in trees – more accurate, but cannot calculate very old material

RADIOMETRIC DATING

Radiometric Dating U-Pb Dating: Used

to date rocks that contain U and Pb. Not acurate for rocks less than 10 myo.

Page 15: 29.3 A BSOLUTE T IME. H ISTORICAL M ETHODS Counting rigs in trees – more accurate, but cannot calculate very old material

RADIOMETRIC DATING

Radiometric Dating Rubidium/

Strontium dating, Used to date rocks that contain Rb and Sr. Used for extremely old rocks.

Page 16: 29.3 A BSOLUTE T IME. H ISTORICAL M ETHODS Counting rigs in trees – more accurate, but cannot calculate very old material

RADIOMETRIC DATING

Radiometric Dating Potassium/Argon

dating, Used to date rocks that contain K and Ar. Can be used to date rocks as young as 50000 y.o. Met/Sed/Ig Rocks