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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.
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