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    PowerLecturePowerLectureA Microsoft PowerPoint Link Tool

    forfor

    academic.cengage.com/earthsci

    Changing EarthChanging EarthExploring Geology

    and EvolutionExploring Geologyand Evolution

    55thth EditionEdition

    James S. MonroeJames S. Monroe || Reed WicanderReed Wicander

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    Chapter 1

    UnderstandingEarth

    A Dynamic andEvolving Planet

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    Introduction

    Geology

    Geology is a complex, integratedsystem of related

    parts, components, or sub-systems that interactin an organized fashion, affecting one another in

    various ways.

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    Introduction

    The principal subsystemsof theearth are the:

    Atmosphere

    BiosphereHydrosphere

    Lithosphere

    Mantle

    Core

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    The interaction of these subsystems has resulted in a

    dynamically changing planet in which matter andenergy are continuously recycled into different forms.

    Introduction

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    Geology is the study of the Earth.

    Physical geology is concerned with the

    materials and processes which compose andoperate on the surface of, and within, Earth.

    Historical geology is concerned with the

    origin andevolution of Earth's continents,oceans, atmosphere, and life.

    What is geology?

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    What is geology?

    Geologists areemployed indiverse occupations.

    Principle occupationsinclude:

    Mineral and

    energy resource

    exploration

    Solvingenvironmental

    problems

    Predicting

    natural disasters

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    Geology and theFormulation of Theories

    What is a theory?

    It is arrived at through thescientific method, which

    involvesgathering and analyzing facts

    formulating hypotheses to explain the phenomenon

    testing the hypotheses

    and finally proposing a theory.

    Thehypotheses is a tentative explanation.

    Ascientific theory is a testable explanation for some

    natural phenomenon, that is supported by a large body

    ofevidence.

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    How Does Geology Relateto theHuman Experience?

    Geology pervades oureveryday lives

    and is a part of many aspects of

    human experience, including the artsand literature.

    The range ofenvironmental problems

    and issues of concern to society

    require a basic understanding ofgeology.

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    How does geology affectour daily lives?

    Natural Events

    Economics andPoliticsOur Role as Decision

    makers

    Consumers andCitizens

    Sustainable Development

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    Global Geologic and EnvironmentalIssues Facing Humankind

    Most scientists would argue

    that overpopulation is thegreatest problem facing the

    world today.

    Increasingly large numbers of

    people must be fed, housed,

    and clothed, with a minimal

    impact on theenvironment.

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    Global Geologic and EnvironmentalIssues Facing Humankind

    The greenhouseeffect is the retention of heat in the

    atmosphere, which results in an increase in thetemperature of Earths surface and atmosphere, thus

    producing global warming.

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    Origin ofthe Universe

    Did it begin with a Big Bang?

    In theBig Bang theory, the

    universe began approximately15 billion years ago.

    An extremely dense, hot body

    of matterexpanded and

    cooled

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    Origin ofthe Universe

    How do we know? Evidence for theBig Bang:

    the universe is expanding

    from a central point.Theentire universe has a

    pervasive and constant

    background radiation,

    thought to be the faintafterglow of theBig Bang.

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    Our Solar System

    Its Origin and Evolution

    The Solar System formed from a rotating cloud ofinterstellar matter about 4.6 billion years ago.

    This cloud, upon condensing, collapsed under theinfluence of gravity and flattened into a rotating disk.

    The sun, planets, and moons formed within this disk.

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    Earth

    Its Place in Our Solar System

    Earth formed from a swirling eddy of nebular

    material 4.6 billion years ago, accreting as a solid

    body and soon thereafterdifferentiated into a

    layered planet during a period of internal heating.

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    Why Earth is a Dynamic

    and Evolving Planet

    Earthhas continuously changed during its 4.6

    billion year existenceas aresultof

    interactions between its various subsystems

    and cycles.

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    Earth is composed of 3 concentric layers.

    Core

    Mantle

    Crust.

    Why Earth is a Dynamicand Evolving Planet

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    The core consists of

    a small, solid innerregion

    a larger,liquid, outerportion

    Composed ofiron and a small amount ofnickel.

    TheCore

    Why Earth is a Dynamicand Evolving Planet

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    Why Earth is a Dynamicand Evolving Planet

    The mantle surrounds the core and

    is divided into: a solid lower mantle

    an asthenosphere that behavesplastically and flows slowly

    a solid upper mantle.

    Composed primarily ofperidotite, an igneous rockmade of olivine.

    TheMantle

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    Why Earth is a Dynamicand Evolving Planet

    The outermost layer, the crust,

    is divided into:

    thick continental crust

    thin oceanic crust

    TheCrust

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    Why Earth is a Dynamicand Evolving Planet

    TheAsthenosphere

    Surrounds the lower mantle

    Behaves plastically and slowlyflows

    Partial melting in the

    asthenospheregenerates magma

    (molten rock) that rises to theearths surface.

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    Why Earth is a Dynamicand Evolving Planet

    TheLithosphere

    The crust and upper mantle make

    up the lithosphere which forms thesolid outer layers of the Earth.

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    Why Earth is a Dynamicand Evolving Planet

    PlateTectonic Theory

    The lithosphere is composed of rigid plates that

    diverge, converge, or slide sideways past oneanother as they move over the asthenosphere

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    Why Earth is a Dynamicand Evolving Planet

    PlateTectonic Theory

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    Why Earth is a Dynamicand Evolving Planet

    PlateTectonic Theory

    Volcanoes andearthquakes occur at the

    boundaries between the plates.

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    Why Earth is a Dynamicand Evolving Planet

    PlateTectonic Theory

    Plate tectonic theory isa unifying explanation

    for many geologicfeatures andevents,helping us understandthe composition andinternal processes of

    Earth on a global scale.

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    The Rock Cycle

    Arock is a solid aggregate of one or more minerals, as

    well as non-crystalline matter such as natural glass ororganic material like coal.

    There are three major groups of rocks

    Igneous

    Sedimentary

    Metamorphic

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    The Rock CycleIgneous Rocks form from the crystallization

    of magma as it cools or the consolidation ofvolcanic ejecta.

    Intrusive igneous rock

    crystallizes beneath theearths surface.

    Extrusive igneous rock

    crystallizes and cools at the

    earths surface. At times it

    cools so fast that it forms a

    glass or ash.

    GraniteGranite

    Intrusive Igneous RockIntrusive Igneous Rock

    BasaltBasalt

    Extrusive Igneous RockExtrusive Igneous Rock

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    The Rock Cycle

    Sedimentary Rocks are typically depositedin layers formed from:

    rock/mineral fragments

    precipitation of minerals from solution

    the compaction of plant and animal remains.

    LimestoneLimestone

    Precipitation from seawaterPrecipitation from seawater

    ConglomerateConglomerate

    Forms from river gravelsForms from river gravels

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    The Rock Cycle

    Metamorphic Rocks form from alteration of

    other rocks, usually by:

    Heat

    PressureChemically active fluids

    QuartziteQuartziteGneissGneiss

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    The Rock Cycle

    The rock cycle illustrates the interactions between

    Earths internal andexternal processes and how thethree rock groups are interrelated.

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    The Rock Cycle

    How are the rock cycle and plate tectonics

    related?

    Plate movement is the

    driving mechanism of therock cycle. Plate inter-

    action determines, to

    someextent, which of the

    three rock groups will form.

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    Organic Evolution andtheHistory of Life

    The theory oforganic evolution states:

    that all living things are related and

    havedescended with modification from organismsliving in the past.

    Charles Darwin proposed that the mechanism of

    natural selection results in survival reproductive age

    of those organisms best suited to theirenvironment.

    Fossils, the remains of once-living organisms provide

    theevidence forevolution and a history of life before

    humans.

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    Organic Evolution

    and Plate Tectonics

    Together the theories of platetectonics and organic evolution

    have changed the way we view

    our planet.

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    Geologic Time

    An appreciation of the immensity of geologic time is

    central to understanding theevolution of the Earthand its life.

    Geologic timediffers from the humanperspective of time

    Earth goes through cycles of muchlongerduration than the humanperspective of time

    The immense span of timeencompassed by the Earth's

    existence and geological processessets geology apart

    Thegeologic time scale is thecalendar that geologists use to datepast events in Earths history.

    G l i Ti d

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    Geologic TimeandUniformitarianism

    Uniformitarianism forms a cornerstone of geology. It is

    a fundamental tenet of geology.

    This principle states that the laws of nature have

    remained unchanged through time and thus, thatthe processes observed today have also operated in

    the past, though possibly at different rates.

    Therefore, to understand and interpret geologic

    events from evidence preserved in rocks,geologists

    must first understand present-day processes in

    rocks.

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    How does the study of geology

    benefitus?

    Understanding how the Earths subsystems

    work will help ensure the survival of thehuman species.

    It will help us to understand how our

    actions affect thedelicate balance betweenthese systems.

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    Endof Chapter 1