Natural Hazards - Theory Flashcards
Characteristics of Oceanic Crust (Name all 4)
200m years old, very dense, can sink, renewable and can be destroyed
Continental Crust (Name all 4)
<1500m years old (older), less dense, can’t sink, can’t be renewed or destroyed
Hazards caused by constructive plate boundaries?
Gentle volcanic and seismic activity, SHIELD VOLCANOES, MID-ATLANTIC RIDGE
Hazards caused by destructive SUBDUCTION plate margins:
Volcanic activity, earthquakes, COMPOSITE volcanoes PHILIPPINE PLATE
Hazards caused by destructive COLLISION plate margins:
Earthquake activity, fold mountains HIMALAYAS (EURASIAN)
Hazards found at conservative plate margins:
Earthquake activity - SAN ANDREAS FAULT
Primary effects of a tectonic hazard:
Immediate loss of life, damage to services, damage to buildings, transport damaged
Secondary effects of a tectonic hazard:
Tsunami, shortages of vital supplies, emotional grief, spread of disease from damaged water, economic issues
Immediate responses from tectonic hazards:
Evacuation from areas affected, international aid sent
Long term responses to tectonic hazards:
Rebuilding infrastructure and settlements, redeveloping areas
Mitigation methods?
Monitoring, prediction, protection, planning
How monitoring works for hazards -
Volcanoes - changes in ground shapes by laser beams, satellites detect changes in heat
Earthquakes - change in water pressure, difficult to prove
How prediction works for hazards -
Volcanoes - none
Earthquakes - Historical predictions used to identify locations at risk
How protection works for hazards -
Volcanoes - lava flow diversions, earth embankments
Earthquakes - buildings constructed to resist shaking, earthquake drills
How planning works for hazards -
Volcanoes - predicting areas likely to be affected, restricting land uses and making evac plans
Earthquakes - predicting risk areas, formulating evac plans
What causes the movement of tectonic plates?
Convection currents in the mantle
How do convection currents work?
As thermal energy rises from the core, this reaches the mantle and upon impact with it moves outwards, causing the mantle to move, dragging oceanic + continental crust with it