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Lecture Outlines PowerPoint. Chapter 11 Earth Science, 12e Tarbuck/Lutgens

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© 2009 Pearson Prentice Hall

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Lecture Outlines PowerPoint

Chapter 11

Earth Science, 12e

(2)

Earth Science,

Earth Science,

12e

12e

Geologic Time

Geologic Time

Chapter 11

Chapter 11

(3)

Historical notes

Historical notes

™

Catastrophism

• Landscape developed by catastrophes

• James Ussher, mid-1600s, concluded

Earth was only a few thousand years old

™

Modern geology

• Uniformitarianism

• Fundamental principle of geology

(4)

Historical notes

Historical notes

™

Modern geology

• James Hutton

Theory of the Earth

(5)

Relative dating

Relative dating

™

Placing rocks and events in sequence

™

Principles and rules of

• Law of superposition – oldest rocks are on the bottom

• Principle of original horizontality – sediment is deposited horizontally

• Principle of cross-cutting relationships – younger feature cuts through an older feature

(6)

Superposition is well illustrated

Superposition is well illustrated

in the Grand Canyon

in the Grand Canyon

(7)

Cross

Cross

-

-

cutting relationships

cutting relationships

(8)

Relative dating

Relative dating

™

Principles and rules of

• Inclusions – one rock contained within

another (rock containing the inclusions is younger)

• Unconformities

• An unconformity is a break in the rock record

• Types of unconformities

• Angular unconformity – tilted rocks are overlain by flat-lying rocks

• Disconformity – strata on either side are parallel

(9)

Figure 11.8

Formation of an

angular

(10)

Relative dating

Relative dating

™

Principles and rules of

• Unconformities

• Types of unconformities

• Nonconformity

• Metamorphic or igneous rocks below

(11)

Several unconformities are

Several unconformities are

present in the Grand Canyon

present in the Grand Canyon

(12)

Correlation of rock layers

Correlation of rock layers

™

Matching rocks of similar age in

different regions

(13)

Fossils: evidence of past life

Fossils: evidence of past life

™

Remains or traces of prehistoric life

™

Types of fossils

• Petrified – cavities and pores are filled with precipitated mineral matter

• Formed by replacement – cell material is removed and replaced with mineral matter • Mold – shell or other structure is buried

and then dissolved by underground water • Cast – hollow space of a mold is filled with

(14)

Fossils: evidence of past life

Fossils: evidence of past life

™

Types of fossils

• Carbonization – organic matter becomes a thin residue of carbon

• Impression – replica of the fossil’s surface preserved in fine-grained sediment

• Preservation in amber – hardened resin of ancient trees surrounds an organism

(15)

Cast and mold of a trilobite

Cast and mold of a trilobite

(16)

Fossils: evidence of past life

Fossils: evidence of past life

™

Types of fossils

• Indirect evidence includes

• Tracks

• Burrows

• Coprolites – fossil dung and stomach contents

• Gastroliths – stomach stones used to grind food by some extinct reptiles

(17)

Fossils: evidence of past life

Fossils: evidence of past life

™

Conditions favoring preservation

• Rapid burial

• Possession of hard parts

™

Fossils and correlation

• Principle of fossil succession

• Fossils succeed one another in a definite and determinable order

• Proposed by William Smith – late 1700s and early 1800s

(18)

Determining the ages of

Determining the ages of

rocks using fossils

rocks using fossils

(19)

Fossils: evidence of past life

Fossils: evidence of past life

™

Fossils and correlation

• Index fossils

• Widespread geographically

(20)

Radioactivity and

Radioactivity and

radiometric dating

radiometric dating

™

Atomic structure reviewed

• Nucleus

• Protons – positively charged

• Neutrons

• Neutral charge

• Protons and electrons combined

• Orbiting the nucleus are electrons – negative electrical charges

(21)

Radioactivity and

Radioactivity and

radiometric dating

radiometric dating

™

Atomic structure reviewed

• Atomic number

• An element’s identifying number

• Number of protons in the atom’s nucleus

• Mass number

• Number of protons plus (added to) the number of neutrons in an atom’s nucleus

• Isotope

• Variant of the same parent atom

• Different number of neutrons and mass number

(22)

Radioactivity and

Radioactivity and

radiometric dating

radiometric dating

™

Radioactivity

• Spontaneous breaking apart (decay) of atomic nuclei

• Radioactive decay

• Parent – an unstable isotope

• Daughter products – isotopes formed from the decay of a parent

(23)

Radioactivity and

Radioactivity and

radiometric dating

radiometric dating

™Radioactivity

• Radioactive decay

• Types of radioactive decay

• Alpha emission

• Beta emission

(24)

Types of radioactive decay

Types of radioactive decay

(25)

Radioactivity and

Radioactivity and

radiometric dating

radiometric dating

™

Radiometric dating

• Half-life – the time for one-half of the radioactive nuclei to decay

• Requires a closed system

• Cross-checks are used for accuracy

• Complex procedure

(26)

The radioactive decay curve

The radioactive decay curve

(27)

Dating sedimentary strata

Dating sedimentary strata

using radiometric dating

using radiometric dating

(28)

Radioactivity and

Radioactivity and

radiometric dating

radiometric dating

™

Carbon-14 dating

• Half-life of only 5,730 years

• Used to date very recent events

• Carbon-14 produced in upper atmosphere

• Incorporated into carbon dioxide

• Absorbed by living matter

• Useful tool for anthropologists,

archaeologists, historians, and geologists who study very recent Earth history

(29)

Geologic time scale

Geologic time scale

™

Divides geologic history into units

™

Originally created using relative dates

™

Subdivisions

• Eon

• Greatest expanse of time

• Four eons

• Phanerozoic (“visible life”) – the most recent eon

(30)

Geologic time scale

Geologic time scale

™

Subdivisions

• Eon

• Four eons

• Archean

• Hadean – the oldest eon

• Era

(31)

Geologic time scale

Geologic time scale

™

Subdivisions

• Era

• Eras of the Phanerozoic eon

• Cenozoic (“recent life”)

• Mesozoic (“middle life”)

• Paleozoic (“ancient life”)

• Eras are subdivided into periods

(32)

Figure 11.19

(33)

Geologic time scale

Geologic time scale

™

Difficulties in dating the time scale

• Not all rocks are datable (sedimentary ages are rarely reliable)

• Materials are often used to bracket events and arrive at ages

(34)

End of Chapter 11

End of Chapter 11

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