Chapter 6: Natural Hazards Flashcards
Structure of earth
Crust - oceanic and continental tectonic plates
Mantle - convection currents move plates
Core - highest pressure to move iron in convection current for magnetic field
Distribution of earthquakes and volcanoes
convention currents in mantle cause tectonic plates to move and collide with each other’s plate boundaries
Types of plate boundaries
constructive (divergent) - plates move apart to form new crust as magma rises (rift valleys)
destructive (convergent) - oceanic and continental come together, oceanic pushed down as more dense into subduction zone, melts so magma rises (volcanoes, ocean trenches)
collision- two continental collide and pushed upwards since same density (fold mountains)
conservative - plates run alongside causing friction (earthquakes)
Formation of earthquakes
tectonic plates locked together due to friction
pressure builds up
strain released
shock waves of energy travel outward from focus underground towards epicentre surface
Factors of amount of damage of earthquakes
depth of focus
geology of area (sedimentary rocks vibrate)
magnitude
vulnerability of population
Impact of earthquake
loss of life
destroyed infrastructure
water bourne diseases (cholera)
landslides
tsunamis
financial losses
Types of volcanoes
Fissure - lava erupts from long thin vent
Shield - runny lava, wider
Dome - thicker, steep convex slope
Strato - viscous lava + ash
Structure of volcano
magma chamber
lava flows (surface of volcano)
volcanic bombs
crater
layers of lava and ash (inside)
ash and gas
side vent (from magma flowing upwards)
Impact of volcanoes
lava flows
gas clouds (co2 and n2o)
volcanic bombs (giant rocks)
pyroclastic flows (fast clouds of ash and gas)
lahars (violent mudflows of ice or snow melt)
loss of life
ash fall
destroyed habitats
Managing impacts before an earthquake
before -
monitor fault lines
satellite technology
earthquake proof designed buildings
retrofit old buildings
education
earthquake drills
Managing impacts during an earthquake
seismometers send signals to rescue stations
emergency supply kits
technology for fast warnings
Managing impacts after an earthquake
search rescue (sniffer dogs/ lifting equipment)
emergency hospitals
emergency aid/ foreign aid
repair and clear up
reconstruct and rebuild
Managing impacts before an volcanic eruption
evacuation plans based on historic ash records
monitored from space or tiltmeters
seismometers detect movement in magma
volcano shelters
education
evacuation
Managing impacts after an volcanic eruption
search and rescue
rebuild buildings
ash fall cleared
settlements abandoned
Distribution of tropical cyclones
between 5 and 20 degrees north and south of the equator
warm tropical water 27 degrees celsius
ocean depth of 60m