Hazardous Earth - Tectonics Notes

Earth's Cross Section and Layers

  • Crust: Continental (granitic, thicker, older, less dense) and Oceanic (basaltic, thinner, younger, more dense).
  • Mantle: Upper (solid, silica-based), Lower (liquid).
  • Core: Outer (liquid, iron/nickel), Inner (solid).

Plate Boundaries

  • Divergent: Plates move apart, magma rises, forming new land or shield volcanoes (e.g., Mid-Atlantic Ridge). Earthquakes can occur.
  • Conservative: Plates slide past each other, no crust created/destroyed. Earthquakes occur (e.g., San Andreas Fault).
  • Convergent: Plates collide. Oceanic plate subducts under continental, creating trenches and composite volcanoes. Earthquakes occur. Collision of two equal density plates forms fold mountains.

Plate Movement

  • Residual heat and radioactive decay in the core generate heat.
  • Convection currents in the mantle cause plates to collide, slide, or be pulled apart.

Tectonic Hazards

  • Volcanoes: Mainly along plate margins. Measured using the Volcanic Explosivity Index (VEI).
  • Earthquakes: Occur on conservative plate margins. Focus (below surface), Epicentre (above surface).
  • Tsunamis: Oceanic waves caused by undersea earthquakes/volcanic eruptions.

Volcano Types

  • Shield (Divergent): Low, flat, gentle slopes. Basaltic magma, fluid, frequent gentle eruptions (e.g., Mauna Loa).
  • Composite (Convergent): Steep sided, layers of ash and lava. Granitic/andesitic magma, viscous, infrequent explosive eruptions (e.g. Montserrat).
  • Hotspots (Divergent): Low, flat, gentle slopes. Basaltic magma, fluid, frequent gentle eruptions (e.g., Kilauea, Hawaii).

Case Studies

  • Volcanic Eruption (Emerging Country): Mount Pinatubo, Philippines, 1991
    • Primary impacts: Deaths, homes destroyed, power cuts.
    • Secondary impacts: Disease, crop destruction, economic devastation.
    • Responses: Prediction, warnings, evacuation, long-term dykes and dams.
  • Earthquake (Developed Country): Tohoku, Japan, 2011 (9.0 Richter scale)
    • Primary Impacts: Deaths, building destruction, infrastructure collapse
    • Secondary Impacts: Tsunami, nuclear meltdown, homelessness, cost of rebuilding = £300 billion.
    • Responses: Tsunami warning, rescue efforts, evacuation.
  • Earthquake (Developing Country): Port-au-Prince, Haiti, 2010 (7.0 Richter scale)
    • Primary impacts: Shanty towns crumbled, business collapse, damaged infrastructure.
    • Secondary impacts: Long-term displacement, job loss, transport disruption, disease.
    • Responses: Rescue teams, international aid, debt relief.
  • Volcanic Eruption (Developed Country): Hawaii, USA (Kilauea since 1983)
    • Primary impacts: Land destroyed, homes destroyed, utilities damaged.
    • Secondary impacts: Air pollution, acid rain, respiratory disease, increased tourism.

Earthquake Location and Measurement

  • Most earthquakes occur at convergent boundaries due to stress build-up.
  • Measured using seismometers and the Richter scale (1-10, logarithmic).

Mantle Layers

  • Lithosphere: Crust and upper mantle (80-100km thick), broken into plates.
  • Asthenosphere: Denser upper mantle (100-300km deep).