Hazards Flashcards
Hazard
An extreme event that threatens people, their property and settlements
When does a hazard become a disaster?
When it causes widespread destruction to property and lives
Risk
The probability of an event happening and the scale of its possible damage
Adjustment or mitigation
The ability of a population to take preventative or precautionary measures
Predictability
How easy hazards are to predict
A factor affecting risk
Frequency and severity of events
Hazard categories
Geological, Climatic, Biological, Technical
Outer core (Thickness, state, temperature)
2200km, liquid, 3000
Mantle (Thickness, state, temperature)
2900km, Solid buts flows (theological consistency), 375
Inner core (Thickness, state, temperature)
1270km, Solid (iron and nickel), 3000
Crust (Thickness, state, temperature)
0-70km, Solid (Granite and Basalt), 10
Oceanic crust (age, density, thickness, can/can’t subduct)
Newer (<200 million years old), Denser, 5km, can subduct
Continental crust (age, density, thickness, can/can’t subduct)
Older (1500 million years old), Less dense, 30km, can’t subduct
Lithosphere
Top 100km of the Earth (curst and mantle) that makes up the tectonic plates
Asthenosphere
The rest of the upper part of the mantle that acts as a lubricant for the tectonic plates to move on
How do tectonic plates move?
Slab pull, ridge push and convection currents
Worldwide distribution of earthquakes and volcanoes
- Uneven
- Mostly correlated with plate boundaries
- Some earthquakes can be away from boundaries due to human activity
- 75% of volcanoes in the pacific ring of fire
- Hotspot volcanoes formed away from boundaries where isolated plumes of magma rise up through the crust e.g. Hawaii
Divergent aka Constructive
2 oceanic plates moving apart creating effusive volcanoes and small earthquakes
Convergent aka Destructive
Oceanic plate subducts under continental plate creating powerful earthquakes and explosive volcanoes
Collision
2 continental plates collide creating powerful earthquakes and fold mountains
Transformative aka Conservative
2 continental plates slide past each other creating powerful earthquakes
Shield volcanoes
Short, gently sloping volcanoes composed of basaltic lava due to its low viscosity has effusive eruptions
Stratovolcanoes
Tall, steep sided volcanoes composed of alternating layers of lava and pyroclastic flow deposits due to stick, highly viscous, rhyolitic lava, have explosive eruptions
The scale by which we measure volcanic eruptions
Volcanic Explosivity Index
Primary hazards
Immediate effects resulting from the event
Secondary hazards
Things that happen as a result of primary hazards
Date of Fuego eruption
3rd June 2018
Height of Mt. Fuego
3763m
Plate boundary of Fuego
Cocos and Caribbean destructive
Distance from Guatemala City
48km
Speed of Fuego’s pyroclastic flow
> 100kmph
Physical effects of Fuego
Airport closed, 8500Ha of crop damaged and traffic chaos
Human effects of Fuego
110 killed, 200 missing, 1200 evacuated, 3000 in temporary housing, 1.7 million effected
Fuego aftermath
CONRED (National disaster management agency) accused of mismanaging disaster warnings
Fuego prologue
Scientists warned of eruption 8 hours before but it took 3 hours for evacuation orders to be issued
Kilauea eruption date
4th May 2018
Kilauea eruption ash cloud height
9km
Kilauea location
Hawaiian hotspot