Lecture11_PlateTectonics.pdf

    Plate Tectonics

    Lecture 11

    What Are the Earth’s Major Geological Hazards?

    ´ Dynamic processes move matter within the earth and on its surface´ Cause volcanic eruptions,

    earthquakes, tsunamis, erosion, and landslides

    Plate Tectonics

    ´ Unified theory: Study the dynamic creation, movement, and destruction processes of plates

    ´ Plates: lithosphere fragments

    ´ Plates move in relation to each other at varied rates

    ´ No major tectonic movements within plates

    ´ Dynamic actions concentrated along plate boundaries

    3 major types of plate boundaries

     Divergent: plates moving apart and new lithosphere produced in mid-oceanic ridge

     Convergent: plates collide, subduction and mountain building

     Transform: two plates slide past one another

    The Earth Beneath Your Feet Is Moving

    Divergent Margins and the Red Sea

    Figure 2.21Seafloor Spreading

    Convergent Margins When plates collide

    ´Continent-Continent

    ´Ocean-Ocean

    ´Ocean-Continent

    Transform Faults

    Transform Margins along the Seafloor

    San Andreas fault

    Driving Mechanism´ What drives plate motion?

    ´ Old idea: plates are dragged atop a convectingmantle.

    ´Convection does occur; not the prime driving mechanism.

    ´ Modern thinking: two other forces drive plate motions. ´ Ridge-push—elevated MOR pushes lithosphere away.

    ´ Slab-pull—gravity pulls a subducting plate downward.

    Volcanoes Release Molten Rock from the Earth’s Interior

    ´ Volcano´Magma rising through the

    lithosphere reaches the earth’s surface through a crack (fissure)

    ´Eruption–release of lava, hot ash, and gases into the environment

    • ~1500 active volcanoes on Earth

    • 400 erupted in the last century

    • ~50 eruptions per year

    • Most activity concentrated along major plate boundaries

    • Impact risks depend on the type of volcano

    Introduction

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    Viscosity of Magma and Explosiveness

    Silicon-oxygen tetrahedron

    Hot Spots

    ´ Volcanic centers with magma source from deep mantle, perhaps near the core-mantle boundary

    ´ A chain of volcanoes over a stationary hot spot

    ´ The bend of a seamount chain over a hot spot representing the change of plate motion

    What are Earthquakes?

    Faulting

    ´Occurs when rock breaks accompanied by displacement

    ´Occurs along zones of weakness in the crust, fault zones

    ´Fault lines´Begin as sudden ruptures, but

    can result in large (hundreds of km) faults over millions of year

    21© 2011 Pearson Education, Inc.

    Faulting

    ´Earthquakes´Vibration in Earth resulting from

    sudden displacement along a fault

    ´Earthquake waves´Energy released by earthquakes

    moves in several types of seismic waves that originate at the center of fault motion, the origin

    ´Ground above origin experiences strongest jolt, the epicenter

    © 2011 Pearson Education, Inc.

    Body Waves: P and S waves

    ´ Body waves´ P or primary waves

    ´fastest waves´travel through solids, liquids, or gases´compressional wave, material

    movement is in the same direction as wave movement

    ´ S or secondary waves´slower than P waves´travel through solids only´shear waves – move material

    perpendicular to wave movement

    Surface Waves: R and L waves

    ´ Surface Waves´ Travel just below or along the ground’s surface´ Slower than body waves; rolling and side-to-side

    movement´ Especially damaging to buildings

    Surface Waves: R and L waves

    ´ L-waves (Love waves)´Waves that intersect the land surface´Move the ground back and forth like a

    writhing snake

    ´ R-waves (Rayleigh waves)´ Waves that intersect the land surface´ Particles underground follow a circular

    path as the wave passes´ Cause the ground to ripple up and down

    Where Do Earthquakes Occur and How Often?~80% of all earthquakes occur along the “Ring of Fire”

    Earthquakes Are Geological Rock-and-Roll Events

    ´ Richter scale ´Insignificant: <4.0´Minor: 4.0–4.9´Damaging: 5.0–5.9´Destructive: 6.0–6.9´Major: 7.0–7.9´Great: >8.0

    ´ Largest recorded: 9.5 in Chile, 1960

    Tsunamis

    Earthquakes on the Ocean Floor Can Cause Tsunamis

    ´ Tsunami´Series of huge waves generated when ocean floor

    suddenly rises or drops´Travels several hundred miles per hour

    ´Slows down as it approaches coastline´ December 2004–Indian Ocean tsunami

    ´Magnitude 9.15 earthquake´Over 230,000 people lost their lives

    ´No warning system in place

    Earthquakes on the Ocean Floor Can Cause Tsunamis

    Where they Occur

    (Setake and Atwater, 2007)

    • Plate Tectonics
    • What Are the Earth’s Major Geological Hazards?
    • Plate Tectonics
    • 3 major types of plate boundaries�
    • The Earth Beneath Your Feet Is Moving
    • Slide Number 6
    • Figure 2.21
    • Convergent Margins �When plates collide
    • Transform Faults
    • Slide Number 10
    • Slide Number 11
    • Driving Mechanism
    • Volcanoes Release Molten Rock from the Earth’s Interior
    • Introduction
    • Slide Number 15
    • Viscosity of Magma and Explosiveness
    • Slide Number 17
    • Hot Spots
    • Slide Number 19
    • What are Earthquakes?
    • Faulting
    • Faulting
    • Body Waves: P and S waves
    • Surface Waves: R and L waves
    • Surface Waves: R and L waves
    • Where Do Earthquakes Occur and How Often?
    • Earthquakes Are Geological Rock-and-Roll Events
    • Tsunamis
    • Earthquakes on the Ocean Floor Can Cause Tsunamis
    • Earthquakes on the Ocean Floor Can Cause Tsunamis
    • Slide Number 31
    • Where they Occur

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