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Understanding Tectonic Hazards and Risks

May 11, 2025

Tectonic Processes and Hazards - EQ1: Why Are Some Locations More at Risk?

Introduction

  • Aim: Understand why some locations are more at risk from tectonic hazards.
  • Reminder: This is an overview, not a replacement for detailed lessons.
  • Tectonics and Hazards is a small part of the AEV course (16 marks).
  • Importance of having a broad understanding to apply case studies in exams.

Tectonic Hazards

  • Definition: Threats to human life/infrastructure due to plate boundaries and movements.
  • Distribution:
    • Most earthquakes occur on plate boundaries.
    • Powerful earthquakes at conservative boundaries.
    • Ocean Fracture Zone (OFZ) - earthquake activity along mid-ocean ridges (e.g., Mid-Atlantic Ridge).
    • Continental Fracture Zone (CFZ) - earthquake activity along mountain ranges.
    • Pacific Ring of Fire - active volcanic/earthquake area.
    • Intraplate earthquakes and volcanic hotspots (e.g., Hawaii, Iceland).

Plate Margins

  • Constructive Margins:
    • Plates move apart; magma rises, forming volcanoes.
    • Oceanic-oceanic or continental-continental plates.
    • Eruptions are effusive, low gas content, high viscosity.
  • Destructive Margins:
    • Plates move towards each other; forms earthquakes, volcanic eruptions.
    • Oceanic-continental, oceanic-oceanic, continental-continental interactions.
    • Subduction zones create the most dangerous hazards.
  • Conservative Margins:
    • Plates slide past each other (e.g., San Andreas Fault).
    • Frequent, shallow earthquakes; no volcanic activity.

Earth's Structure

  • Layers: Crust, lithosphere, asthenosphere, mantle, outer core, inner core.
  • Mantle Convection: Drives plate movements; internal heat engine of Earth.

Key Theories and Discoveries

  • Continental Drift: Alfred Wegener (1912) - Pangaea supercontinent.
  • Convection Currents: Arthur Holmes (1930s) - driving force of plate movements.
  • Seafloor Spreading: Harry Hess (1960s) - mid-ocean ridges.
  • Paleomagnetism: Earth's magnetic field creates patterns on seafloor.
  • Subduction, Gravitational Sliding, Slab Pull:
    • Subduction: Dense plates sink under lighter plates.
    • Gravitational Sliding: Constructive margins, rising magma creates slopes.
    • Slab Pull: Dense oceanic plate pulled into mantle.

Hazard Characteristics by Plate Margin

  • Constructive Margin:
    • Shallow, low-magnitude earthquakes; small, low gas content volcanoes.
    • Example: Mid-Atlantic Ridge.
  • Destructive Margin (Oceanic-Continental):
    • Large earthquakes, violent volcanic eruptions.
    • Example: Nazca and South American Plate Boundary.
  • Destructive Margin (Oceanic-Oceanic):
    • Frequent earthquakes, volcanic islands (e.g., Hawaii).
  • Collisional Margin (Continental-Continental):
    • Large fault lines, high magnitude earthquakes; no volcanic eruptions.
    • Example: The Andes.
  • Conservative Margin:
    • High magnitude earthquakes, shallow focus, no volcanic activity.
    • Example: San Andreas Fault.

Earthquake Hazards

  • Primary Waves (P-waves): Fastest, least destructive.
  • Secondary Waves (S-waves): Cause ground shaking, more destructive.
  • Love Waves (L-waves): Cause significant damage, travel horizontally.

Earthquake-Induced Hazards

  • Crustal Fracturing: Primary hazard; fractures and cracks in Earth's surface.
  • Liquefaction: Secondary hazard; waterlogged ground destabilized.
  • Landslides: Secondary hazard; soil dislodged on slopes.

Volcanic Hazards

  • Primary Hazards:
    • Pyroclastic Flows: Fast, hot, dense ash and gas clouds.
    • Ashfall: Damages vegetation, buildings, water sources.
    • Lava Flows: Destroys anything in path.
    • Gas Eruptions: Poisonous gases emitted.
  • Secondary Hazards:
    • Lahars: Volcanic mudflows.
    • Jökulhlaups: Flooding from glacial meltwater.

Tsunamis

  • Causes: Submarine earthquakes, volcanic eruptions, landslides.
  • Characteristics:
    • Disruption of seabed rock causes waves.
    • Waves increase in height as they approach shore.
    • Speeds between 250 and 950 km/h.

Conclusion

  • Overview of EQ1 - tectonic processes and hazards.
  • Importance of understanding risk factors and hazard development.
  • Next session will cover EQ2.