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Introduction to Geology Phil Murphy [email protected]. ac.uk 1

Introduction to Geology Phil Murphy [email protected] 1

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Page 1: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

Introduction to Geology

Phil [email protected]

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Page 2: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

“Civilisations are what they dig from the Earth”

GibbonsDecline and fall of the Roman Empire, 1776

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Page 3: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

“If Kuwait had of grown carrots no one would have given a damn!”

Senior Source - NSA

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Page 4: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

Why is geology different from other sciences?•Often lacks experimental control• Incompleteness of data•Methodologies and procedures used to test

problems rather than the generation and testing of universal laws

•GEOLOGY WORKS• (everyone wants to drive to Sainsburys)

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Page 5: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

12_04c.jpg

5Principle of Superposition

Page 6: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

12_04e.jpg

6Principle of Original Horizontality

Page 7: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

Two kinds of ages•Relative - know order of events but not dates• Napoleonic wars happened before W.W.II • Bedrock in Scotland formed before the

glaciers came

•Absolute - know dates• Civil War 1803-1815• World War II 1939-1945 • Glaciers finally left Scotland About 11,000 Years

Ago

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Page 8: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

Two conceptions of Earth history •Catastrophism• Assumption: great effects require great causes • Earth history dominated by violent events

•Uniformitarianism• Assumption: we can use cause and effect to

determine causes of past events • Finding: Earth history dominated by small-scale

events typical of the present. • Catastrophes do happen but are uncommon

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Page 9: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

Principles of Relative Dating

•Law of superposition Undeformed section of sedimentary or

layered igneous rocks Oldest rocks are on the bottom

•Principle of original horizontality Layers of sediment are generally deposited in

a horizontal position Rock layers that are flat have not been

disturbed (deformed)•Principle of cross-cutting relationships

Younger features cut across older features

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Page 10: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

Superposition Strata in the Grand Canyon

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Page 11: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

Horizontality11

Page 12: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

Cross-cutting Relationship

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Page 13: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

Cross-cutting Relationship13

Which crater is youngest?

Page 14: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

Cross-cutting Relationships

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Page 15: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

Principles of Relative Dating• Inclusions• A piece of rock that is enclosed within

another rock• Rock containing the inclusion is

younger•Unconformity• Break in rock record produced by

erosion and/or non-deposition of rock• Represents period of geologic time

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Page 16: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

Principles of Relative Dating

•Types of unconformities Angular unconformity• tilted rocks (disturbed) are overlain by flat-lying

rocks

Disconformity • strata on either side of the unconformity are

parallel

Nonconformity• metamorphic or igneous rocks in contact with

sedimentary strata

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Page 17: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

Angular Unconformity17

Page 18: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

Angular Unconformity18

Page 19: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

Angular Unconformity19

Page 20: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

Uniformitarianism

•Continuity of Cause and Effect• Apply Cause and Effect to Future -

Prediction • Apply Cause and Effect to Present -

Technology • Apply Cause and Effect to Past –

Uniformitarianism

The present is the key to the past

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Page 21: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

Ripple Marks - Scarborough21

Page 22: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

Fossil Ripple Marks22

Page 23: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

Modern Mud Cracks23

Page 24: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

Fossil Mud Cracks24

Page 25: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

The makings of good Index Fossils

•Abundant •Widely-distributed (Global Preferred) •Short-lived or rapidly changing

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Page 26: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

Correlation26

Page 27: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

The Geologic Time ScaleQuaternary Latin, “fourth” 1822

Tertiary Latin, “third” 1760

Cretaceous Latin creta, “chalk” 1822

Jurassic Jura Mountains, Switzerland 1795

Triassic Latin, “three-fold” 1834

Permian Perm, Russia 1841

Carboniferous Carbon-bearing 1822

Devonian Devonshire, England 1840

Silurian Silures, a pre-Roman tribe 1835

Ordovician Ordovices, a pre-Roman tribe 1879

Cambrian Latin Cambria, “Wales” 1835

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Page 28: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

Absolute ages: early attempts

•The Bible

• Add up dates in Bible • Get an age of 4000-6000 B.C. for Earth • John Lightfoot and Bishop Ussher - 4004 B.C.,

October 26th 9 a.m (1584) • Too short!

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Page 29: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

Absolute ages: early attempts

•Salt in Ocean• If we know the rate salt is added, and how much salt

is in ocean, we can find the age of oceans. •Sediment thickness• Add up thickest sediments for each period and

estimate rate.•Both methods gave age of about 100 million

years• Problem: rates variable

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Page 30: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

Radiometric Dating: Half-Life

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Page 31: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

•Parent • an unstable radioactive isotope

•Daughter product• the isotopes resulting from the decay of a parent

•Half-life• the time required for one-half of the radioactive

nuclei in a sample to decay

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Radiometric Decay

Page 32: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

•Principle of radioactive dating

The percentage of radioactive toms that decay during one half-life is always the same (50%)

However, the actual number of atoms that decay continually decreases

Comparing the ratio of parent to daughter yields the age of the sample

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Radiometric Dating

Page 33: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

Radioactive Decay Curve33

Page 34: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

Radioactive Decay Curve

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Page 35: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

Present Radiometric Dating Methods

Cosmogenic•C-14 5700 Yr.

Primordial•K-Ar (K-40) 1.25 B.Y. •Rb-Sr (Rb-87) 48.8 B.Y •U-235 704 M.Y.

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Page 36: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

•Sources of error A closed system is required To avoid potential problems only fresh,

unweathered rock samples should be used

•Carbon-14 (radiocarbon) dating Half-life of only 5730 years Used to date very recent events C14 is produced in the upper atmosphere

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Radiometric Dating

Page 37: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

Some Geologic RatesCutting of Grand Canyon•2 km/3 m.y. = 1 cm/15 yr

Uplift of Alps•5 km/10 m.y. = 1 cm/20 yr.

Opening of Atlantic•5000 km/180 m.y. = 2.8 cm/yr.

Uplift of White Mtns. (N.H.) Granites•8 km/150 m.y. = 1 cm/190 yr.

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Page 38: Introduction to Geology Phil Murphy p.murphy@see.leeds.ac.uk 1

Some Geologic Rates

Movement of San Andreas Fault•5 cm/yr = 7 m/140 yr.

Growth of Mt. St. Helens•3 km/30,000 yr = 10 cm/yr.

Deposition of Niagara Dolomite•100 m/ 1 m.y.? = 1 cm/100 yr.

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