HAZARDS Flashcards
3 types of geological hazards
Geophysical- land
Atmospheric- wind
Hydrological- water
Perception
How people have different viewpoints of how dangerous hazards are and the risk they pose.
Dependant on lifestyle factors.
E.g a wealthy person worries less as they have to money to solve the damage
Fatalism
The viewpoint that hazards are uncontrollable natural events
Losses should be accepted as there is nothing we can do about it.
Prediction
Using scientific research and paste events, to know when a hazard might take place.
So that warnings can be delivered and the impacts can be reduced.
Adaptation
Attempting to live with the hazard
Adjusting lifestyle choices
So that vulnerability of the hazard is reduced
Mitigation
Strategies that help to reduce the severity of the hazard
Management
Strategies to reduce the hazards effects
Risk sharing
Community preparedness: share risks and invest collectively.
Park model
Graphical representation of steps carried out in HAZARD RECOVERY
Rough time frame
Good for comparing hazards
Stages of the park model 1,2,3
1- relief. (Hours and days). Immediate local response: medical age, search and rescue
2- rehabilitation. services begin to be restored. Food and water. Temporary shelters.
3- reconstruction. Restoring the area
Hazard management cycle
Outlines the stages of responding to events, showing the same stages take place after every hazard
4 stages of the hazard management cycle
Preparedness.
Response
Recovery
Mitigation
Inner core
Solid ball of iron or nickel
Very hot due to pressure and radioactive decay
Responsible for earths internal energy
Outer core
Semi- molten
Iron/ nickel
Mantle
Main,y solid
Rocks high in silicone
Top of many,e is the asthenosphere
Asthenosphere
Semi molten
Moves due to convection currents
Lithosphere above
Lithosphere
Broken up into plates
Top is the crust
Crust
Thin top of the lithosphere
Oceanic crust is dense and is destroyed by plate movement
Continental crust is less dense and is NOT destroyed
Destructive plate boundaries direction
Towards
Conservative movement
Along side
Constructive movement
Away from eachother
Landforms made by destructive plate margin
Volacnoes
Fold mountains
Earthquakes
Island arcs
Ocean trenches
Landforms made by conservative
Eq
Landforms made by constructive
Volcanoes
Eq
Ocean ridges
Rift valley
Destructive (continental and oceanic)
Denser oceanic plate subducts below continental
Leave a deep ocean trench
Destructive (oceanic and oceanic)
Heavier plate subducts leaving an ocean trench
Built up pressure causes and underwater volacnoes
Lava cools and causes island arcs
Destructive (continental and continental)
Both plates not as dense
Oceanic is subducted slightly
Fold mountains form
Ridge push
Gravity pushes plates further away
Widens gap
Known as gravitational sliding