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Hutton’s Unconformity

Siccar Point, Scotland

• During a time when many claimed the age of the Earth to be about 6,000 years, came a voice of reason:

– “We find no sign of a beginning-no prospect for an end”

– James

Hutton

(1788),

Scotland

Principles used to determine relative age

• Original Horizontality

– sedimentary beds deposited near horizontal

• Superposition

– layers young from bottom to top

• Lateral Continuity

– tapering, thinning near edges

• Cross-cutting Relationships

– disrupted pattern is older than disruption

– truncation of older rock bodies

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Unconformities

• Unconformity surface that represents a gap in the geologic record

– Disconformity - contact representing missing parallel beds

– Angular unconformity - younger strata overlie an erosion surface on tilted or folded layers

– Nonconformity - erosion surface on plutonic or metamorphic rock

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Great Unconformity: The Grand Canyon

• In detail a nonconformity with Cambrian (ca.

530 Ma) Tapeats sandstone deposited on 1.7 Ga

Vishnu schist)

Reading the rock record:

Timing of events on the local scale

What is the relative age of granite ?

When did tilting take place ?

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Timing of event on the regional scale:

Correlation

• Physical continuity

• Similarity of rock types

• Superposition

• Correlation by fossils

– Principle of faunal succession

– Concept of index fossil

– Fossil assemblage

• Radioisotopic dating-comparisons

Correlation of strata: Colorado Plateau

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Correlation

• Physical continuity

• Similarity of rock types

• Superposition

• Correlation by fossils

– Principle of faunal succession

– Concept of index fossil (short lived, widespread)

– Fossil assemblage

• Radioisotopic dating-comparisons

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Henri Becquerel b. 1852 / d. 1908

Becquerel (1896) Sur les radiations emises par phosphorescence. Comptes Rendues Acad. Sci. Paris, v. 122,

420-21.

• Discovered natural radioactivity (x-rays fog photographic plate)

• Nobel Prize in Physics 1903 (with Pierre and Marie Curie)

Ernest Rutherford b. 1871 / d. 1937

Rutherford & Soddy (1903) Radioactive Change. Phil Mag ser 6, v 576-91.

• Atomic "disintegration" theory of radioactivity

• Nobel Prize in Chemistry 1908

Numerical Age

• Isotopic Dating (or radioisotopic dating)

• Isotopes and Radioactive Decay

–Isotopes

• Atoms of an element with differing number of neutrons, but same number of protons

–Radioactive Decay

• Spontaneous nuclear disintegration of unstable isotopes

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Radioactive decay of Uranium to Lead

Helium atoms neutron > proton

Numerical Age

• Radioactive Decay

–Parent isotope decays to daughter product

• rate of decay measured by physicists

• decay process is “exponential”, not linear

• half-life

– Time it takes for half the parent isotope to decay

– After one half-life, equal amounts of parent and daughter isotopes are present in a mineral

• decay constant

– Portion of isotope that decays per unit time

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Exponential

Decay of parent isotope and

Increase of daughter isotope

Linear

Decay of burning candle

Calculating the age of a Mineral

• Relationship between time and radioactive decay

Constant = 2.718

Number of atoms of isotope at time “t”

N = N o e λ t

Decay constant: portion of isotope that decays per unit time

Number of atoms of isotope when clock was set

• How do we measure λ ? Half-life concept:

λ = ln 2/t half-life

= 0.693/t half-life

• Age of mineral: t = (1/ λ )*ln(N/N o

) we measure N (# atoms parent isotope) we measure D (# atoms daughter) to get N o

[N o

= N + D]

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Numerical Ages

• Uses of Isotopic Dating

– Age of eruption of lava, ash

• ash can allow dating of sediments in many cases

– Age of intrusion

– Age of metamorphism

• Reliability of Isotopic Dating ?

– Multiple methods: U-Pb, Rb-Sr, K-Ar, etc.

– Combine with Relative Dating Principles

– Powerful means to understand time scales and rates of geological processes

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• Arthur Holmes b. 1890 / d. 1965

Holmes (1913) The Age of the Earth, Harper & Brothers

• First geologist to apply radioactivity to dating rocks

• First numerical timescale (counters Lord Kelvin)

• Combined U-Pb date from Norway with Boltwood's results

• Phanerozoic >400 myr long

• Earth is >4 billion yrs old

Holmes (1928) Radioactivity and Earth movements.

Transactions Geological Society of Glasgow, v. 18, 559-

606.

•Suggested that mantle flows due to radioactive heating, supporting Wegner's theory of continental drift, 30 years before plate tectonic theory !

K-Ar dating of the Green River Formation, Wyoming

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K-Ar dating feldspar crystals in volcanic ash beds

Evolving Geologic Time Scale

• Based on Fossil Assemblages & Radioisotopic dating

• Eras, Periods, and Epochs

– Cenozoic Era

• Tertiary & Quaternary Periods

– Recent (Holocene) Epoch

– Mesozoic Era

– Paleozoic Era

• Precambrian - All time before Paleozoic Era

– 88% of Earth History

– no megascopic fauna (bacteria)

– radioisotopic dating essential

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Age of the Earth

• Early speculation

• Dating of meteorites

• U-Pb dating of zircon crystals

– 4.4 billion year old crust

• The Earth is 4.56

billion years old

4,560,000,000

• Comprehending Geologic Time

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Geologic Time Scale

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