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1 Earth’s History
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1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

Mar 30, 2015

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Page 1: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Earth’s History

Page 2: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Earth’s History

• Planet Earth is approximately 4.5 X 109 years old–Rocks of the crust provide clues

to Earth’s past• By analyzing these clues we can infer events from the past

Page 3: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Earth’s History• Principle of Uniformitarianism

–Major assumption in geology–Events in the past occurred the same way

that they are occurring today. Examples Include:• Weathering/erosion• Deposition• Volcanism• Plate tectonics

Page 4: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Geologic Time

• Plate motions and mountain building events can be placed on the geologic time scale

Page 5: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Geologists have divided Earth’s history into time units based on the the fossil record

Geologic Time

Page 6: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Geologic Time• A study of the fossil record shows

–A great variety of plants, animals, and simpler life forms have lived on Earth in the past

–That life forms have evolved through time

–Most life forms of the geologic past have become extinct

Page 7: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Page 8: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Geologic DatingGeologic Dating

Page 9: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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There are two types of Geologic Dating

• AbsoluteAbsolute–Determines how many years old

something is

• RelativeRelative–Used to determine if one thing is

younger or older than another

Page 10: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Tools used to determine

• Using radiometric dating

• Law of superposition• Use of index fossils• Correlation of rock

layers

Absolute Age Relative Age

Page 11: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Relative Dating

Page 12: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Law of SuperpositionLaw of Superposition

• Sediments are laid down underwater in horizontal layers and form sedimentary rocks

Page 13: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Law of Superposition• In a series of sedimentary rocks the

bottom layer is the oldest and the top layer is the youngest– Lower layers must be in place before

younger rocks can be deposited on top of them

– Exception: when something occurs to overturn layers

Page 14: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Grand Canyon

Page 15: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

GRAND CANYON- LAW OF SUPERPOSITION

YOUNGEST ON TOP

OLDEST ON BOTTOM

Page 16: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Law of Superposition• Rock layers are older than folds found in them

– Layers were there before they were folded

Page 17: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Folds/Tilted

Page 18: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Law of Superposition

• Rock layers are older than faults found in them

• This is logical: you can’t break a rock if it does not exist; so rock containing a fault must be older than the fault

Page 19: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Law of Superposition• Fossils are generally the same

age as the rock layers in which they are found–Animal remains are deposited

along with the sediments that will turn into sedimentary rocks

Page 20: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Law of Superposition• Igneous intrusions are younger than the

rock that they cut through or flow out of

Page 21: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Igneous Intrusion - Cross Cutting

Page 22: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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UnconformityUnconformity• When a new rock layer is formed

atop an eroded surface

Page 23: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Page 24: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Upper Silurian Carbonates

Tilted Ordovician Shales and Sandstones

Taconic Unconformity

unconformity

Page 25: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Practice: what happened here?

Page 26: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.
Page 27: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Page 28: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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CorrelationCorrelation

• Matching similar rock layers in different locations to see if they formed at the same time

Page 29: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.
Page 30: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.
Page 31: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.
Page 32: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

Which fossil might be found in Devonian rock layers?

Page 33: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Volcanic Ash Falls• Can also be used to correlate rock layers

over a large area

• Ash is a good indicator because:– The ash from one explosion has distinct

characteristics

– ash can be deposited around the globe

– The event occurs at one, geologically brief, time

Page 34: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Fossils• Naturally occurring preserved remains

or impressions of living things

• Generally only hard parts get preserved – Bones, teeth, shells

• Hard parts are replaced by naturally occurring minerals

Page 35: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

Eurypterus

NY State Fossil

Silurian index

fossil

Page 36: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Fossils

• Can be a mold (impression)–Ex: footprint

• Or a cast–Ex: filled in footprint

Page 37: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Page 38: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Fossils (Cont)

• Other types– Ice– Tar– Carbonaceous film– Amber– Imprints– Petrified

Page 39: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.
Page 40: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.
Page 41: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Fossils• Generally found in

sedimentary rock layers

Why don’t fossils exist in most igneous or metamorphic rock?

Page 42: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Fossils• The living organism

that made the fossil lived during the time the rock layer was forming – i.e. when the sediment

was being deposited

Page 43: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Fossils• Fossils can provide

information about ancient environments– Marine fossils indicate

a marine environment, wooly mammoths indicate a cold environment, etc…

Page 44: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Fossils • A study of the fossil record shows:

–A great variety of plants, animals and simpler life forms have lived on Earth in the past

–That life forms have evolved through time

–Most life forms of the geologic past have become extinct

Page 45: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Index FossilsIndex Fossils• Index Fossils--used to date rock

layers (strata)–Fossils from creatures that existed for

a geologically short period of time• Ex. less than 2.0 x 107

–Fossils from creatures that had a wide geographic distribution

Page 46: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

Location A Location B Location C

Rock layer 1 W W W Z

Rock layer 2 W Z

Y Z

Rock layer 3 W X X X Z

Which letter would make a good index fossil?

Page 47: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Absolute Dating

Page 48: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Radioactive Decay• When an unstable radioactive

element changes into a stable element

Page 49: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Unstable Radioactive Isotope Stable Decay Product

Carbon 14 (C14)

Uranium 238 (U238)

Nitrogen 14 (N14)

Lead 206 (Pb206)

Parent Daughter

Example

Page 50: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Radiometric DatingHalf lifeHalf life: The time required for 1/2 of a parent

material to break down to daughter material

Page 51: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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• Another look

Page 52: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Radiometric Dating• The age of objects can be

determined by measuring the relative amounts of radioisotope and decay products

Page 53: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Radiometric Dating• The half lives of radioisotopes

vary depending upon the isotope–Examples:

• C14 = 5,770 years

• U238 = 4,500,000,000 years

• Rb87 = 47,000,000,000 years

Page 54: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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• Carbon 14 is used to date biological remains–Carbon is incorporated into the

cells of living organisms and begins to decay when the organism dies

• Uranium 238 is used to date rocks–Larger half life

Page 55: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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Half Life Practice

Problems

Page 56: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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• If half the K -40 of a rock has decayed into Ar-40, how old is the rock?

• How many years would it take for 75 % of a sample of K-40 to disintegrate?

Page 57: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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How old are:

• A sample that has ½ c-14 and ½ n-14?

• A sample that has ¼ K-40 and ¾ Ar-40?

• A sample that has ½ U-238 ½ Pb-206?

Page 58: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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How old are:

• A sample that has 1/8 Rb-87 and 7/8 Sr-87?

• A sample that has ¼ C-14 and ¾ N-14?

• A sample that has ¾ C-14 and ¼ N-14?

Page 59: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

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What fraction remains of:

• A 50 billion year old sample has ____ Rb-87 and ____ Sr-87.

• A 2.6 billion year old sample has____ K-40 and ____Ar-40.

Page 60: 1 Earths History. 2 Planet Earth is approximately 4.5 X 10 9 years old –Rocks of the crust provide clues to Earths past By analyzing these clues we can.

This is so boring

Stranz should take a break ;)

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