Tectonic Hazards (AQA GCSE Geography)

Revision Note

Bridgette Barrett

Written by: Bridgette Barrett

Reviewed by: Jenna Quinn

Plate Tectonics Theory

The structure of the Earth

  • The Earth is composed of four main layers:

    • Inner core: About 1400km in diameter, a solid and dense layer composed of iron and nickel with temperatures of about 5500°C

    • Outer core: About 2100km thick, a semi-molten metal layer with temperatures between about 5000-5500°C

    • Mantle: About 2900km thick, a semi-molten layer which is less dense than the outer core 

    • Crust: The thickness varies, and is made up of two types of crust 

Cross-section diagram of Earth showing labeled layers: crust, mantle, outer core, and inner core. The outer layer is the crust, followed by the mantle and cores.
Structure of the Earth

Crust

  • There are two types of crust:

    • The oceanic crust is thinner (5-10km) but heavier and denser

    • The continental crust is thicker (25-90km) but is older and lighter

  • Oceanic crust is continually being created and destroyed as a result of plate movement, where it is denser and so subducts under the continental crust

  • This is why continental crust is much older than oceanic crust, as it isn't destroyed

Plate tectonics

  • The crust is broken into a number of tectonic plates

Map illustrating global tectonic plates including the Pacific, North American, Eurasian, Australian, African, South American, Antarctic, Juan de Fuca, and others.
Distribution of the major tectonic plates
  • These plates move on top of the semi-molten mantle below.

  • Tectonic theory once stated the movement of the plates was the result of convection currents in the mantle

    • Current theory is called slab pull theory which suggests that the movement is the result of the weight of the denser oceanic plates subducting and dragging the rest of the plate along

  • A plate boundary or margin is where two plates meet

Distribution of Earthquakes & Volcanoes

Earthquake distribution

  • Earthquakes occur at all types of plate boundaries

    • Most occur along the Pacific 'Ring of Fire' (approximately 90%)

World map showing earthquake frequency, with clusters of red dots around the Pacific Rim, along Western coasts of Americas, Japan, Southeast Asia, and some parts of Europe.
Global earthquake distribution

Volcano distribution

  • Most volcanoes occur at constructive and destructive plate boundaries

  • The majority of active volcanoes (approximately 75%) are located around the rim of the Pacific Ocean called the 'Ring of Fire'

  • Hotspots occur away from plate boundaries and are plumes/columns of magma which escape through the Earth's crust

World map showing tectonic plate boundaries with red dots indicating significant volcanic and earthquake activity along the edges of continents and oceans.
Active volcano distribution

Worked Example

Study Figure 1, a world map showing plate margins and active volcanoes.

Diagram showing oceanic plates moving apart at an ocean ridge, with magma rising from below the lithosphere, erupting as lava to form new crust.
Constructive plate boundary

Using Figure 1, which one of the following statements is true? 

[1 mark]

A. All active volcanoes occur in lines along plate margins

B. There are more active volcanoes along constructive margins than destructive margins

C. There are many active volcanoes around the edge of the Pacific Ocean

D. Active volcanoes are found along the eastern side of North and South America

Answer: 

  • C. There are many active volcanoes around the edge of the Pacific Ocean [1]

Examiner Tips and Tricks

When describing the distribution of hazards from a map ask yourself the following questions:

  • What is the general pattern?

  • Does the pattern relate to anything else for example the location of plate boundaries?

  • Are they close to the equator or further away?

  • Are they inland or coastal?

Use map features to help with your description - place names, compass rose, latitude and longitude.

Plate Boundaries

Types of plate boundary

  • Volcanic eruptions and earthquakes most commonly occur at or near plate boundaries

  • There are three main types of plate boundaries:

    • Constructive

    • Destructive

    • Conservative (transform)

Constructive plate boundary

  • At a constructive boundary the plates are moving apart

  • The Mid Atlantic Ridge is an example of a constructive plate boundary

  • Both volcanic eruptions and earthquakes can occur at this type of plate boundary

Constructive plate boundary
Constructive plate boundary

Destructive plate boundary

  • At a destructive plate boundary the plates are moving together

  • The denser, heavier oceanic plate subducts under the lighter, less dense continental plate

  • The boundary between the Nazca plate and the South American plate is one example

  • Both volcanic eruptions and earthquakes occur at this type of plate boundary

Diagram illustrating subduction zone: An oceanic plate moves towards a continental plate, causing friction, heating, and melting rock. Magma rises, forming a volcano.
Destructive plate boundary

Conservative (transform) boundary

  • At a conservative (transform)boundary the plates move passed each other in opposite directions or in the same direction at different speeds

  • Earthquakes are the only hazard at this type of boundary

Diagram of tectonic plates moving past each other, with one plate shown moving left and the other right, accompanied by a label "PLATES MOVE PASSED EACH OTHER".
Conservative (transform) boundary

Worked Example

Study Figure 1, a map showing the tectonic plates in and around North and South America 

Map showing tectonic plates (North American, Eurasian, Pacific, South American, Nazca) and earthquake zones. Arrows indicate the direction of plate movement. Key included.

Using Figure 1, name the type of plate margin at X

[1 mark]

Answer: 

  • Conservative (transform) - at X the plates are moving past each other in opposite directions [1]

Examiner Tips and Tricks

When describing the processes which lead to an earthquake or volcanic eruption, it is helpful to write the formation down as a sequence of steps. This will make the process easier to remember.

Primary and secondary hazards

  • When earthquakes and volcanic eruptions occur, there are primary and secondary hazards

The Primary and Secondary Hazards of Tectonic Activity

 

Primary Hazards

Secondary Hazards

Volcanic Eruption

  • Ash

  • Pyroclastic flow

  • Lava flow

  • Gas emissions

  • Volcanic bombs

  • Lahars

  • Acidification

  • Landslides

  • Climate change

  • Fires

  • Floods

Earthquake

  • Ground shaking

  • Gas emissions

  • Building collapse

  • Landslides

  • Gas leaks

  • Fires 

  • Soil liquefaction

  • Subsidence

  • Mudflows

  • Tsunami

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Bridgette Barrett

Author: Bridgette Barrett

Expertise: Geography Lead

After graduating with a degree in Geography, Bridgette completed a PGCE over 25 years ago. She later gained an MA Learning, Technology and Education from the University of Nottingham focussing on online learning. At a time when the study of geography has never been more important, Bridgette is passionate about creating content which supports students in achieving their potential in geography and builds their confidence.

Jenna Quinn

Author: Jenna Quinn

Expertise: Head of New Subjects

Jenna studied at Cardiff University before training to become a science teacher at the University of Bath specialising in Biology (although she loves teaching all three sciences at GCSE level!). Teaching is her passion, and with 10 years experience teaching across a wide range of specifications – from GCSE and A Level Biology in the UK to IGCSE and IB Biology internationally – she knows what is required to pass those Biology exams.