Balearic PAU Geology & Env Sci study materials
Balearic PAU Geology & Env Sci study resources

Balearic PAU Geology & Env Sci: Environmental Geology and Natural Hazards: Volcanic, Seismic, Slope, Coastal and Fluvial Risks

Balearic PAU Geology & Env Sci · Work through your exam, one topic at a time.

All guide sections

Environmental Geology and Natural Hazards: Volcanic, Seismic, Slope, Coastal and Fluvial Risks

This domain assesses whether you can separate hazard, vulnerability, exposure and risk, then analyse a specific process and propose mitigation. Balearic examples include seismic shaking and tsunamis, coastal erosion, slope instability and torrential floods.

Core definitions

  • Hazard: probability of a damaging event of a given magnitude in a period and area.
  • Vulnerability: propensity of exposed elements to be damaged.
  • Exposure: people, assets and activities in the hazard zone.
  • Risk is commonly expressed as hazard × vulnerability × exposure (expected loss). Reducing exposure and vulnerability is the practical lever.

Seismic hazard

Distinguish magnitude (energy released, one value per earthquake) from intensity (local effects, EMS-98 scale). Hypocentre versus epicentre. The Balearics have low to moderate seismicity, linked to Africa-Eurasia convergence and to nearby Algerian margin faults; the 2003 Boumerdès earthquake produced a small tsunami reaching Balearic coasts.

Volcanic hazard (general)

Viscosity and gas content control eruptive style: fluid basaltic lava versus explosive rhyolitic eruptions producing pyroclastic flows, ash and lahars. No active volcanism exists in the Balearics, but the concepts are examinable.

Slope, coastal and fluvial hazards

  • Slope: falls, slides and flows, triggered by rainfall, earthquakes and undercutting; the factor of safety decreases with pore pressure.
  • Coastal: storm waves, longshore drift, dune loss, sea-level rise and beach narrowing. Hard defences often shift erosion downdrift.
  • Fluvial: flash floods in rambles and torrents, where a dry channel can carry a debris-laden flow within minutes.

Worked example

On 9 October 2018, more than 200 mm of rain fell in a few hours on the Sant Llorenç area of eastern Mallorca. A small, normally dry torrent drained a steep, partly urbanised catchment. The lag time was very short because of impermeable surfaces and channel encroachment, so the peak arrived with little warning and caused fatalities. The lesson: hazard was extreme rainfall, but risk was amplified by exposure on the floodplain and by a short lag time.

Traps that cost marks

  • Using magnitude and intensity interchangeably.
  • Saying a 100-year return period means the event occurs every 100 years.
  • Confusing hazard with risk; a hazard in an empty area has no risk.
  • Believing hard coastal defences eliminate erosion rather than displace it.