Hazards Flashcards
(47 cards)
definition
Hazard
Potential threat to human life and property caused by an event
Three major types of geographical hazards?
geophysical, atmospheric, hydrological
Geophysical hazard
Hazards caused by land processes mainly tectonic plates e.g. volcanoes
Atmospheric hazards
Hazards caused by atmospheric processes and conditions created because of these such as weather systems e.g. wildfires
Hydrological hazards
Hazards caused by water bodies and movements
e.g. floods
Hazard Perception
One’s viewpoint of how dangerous a hazard is and what risk they pose.
Varies depending on lifestyle factors
e.g. economic and cultural factors
Prediction
Using scientific research and past events in order to know when a hazard will take place so that warning may be delivered and impacts of the hazard reduced or even prevented.
Adaptation
Attempting to live with hazards by adjusting lifestyle choices so that vulnerability to hazards is lessened.
Mitigation
Strategies carried out to lessen the severity of a hazard.
Management
Coordinated strategies to reduce a hazard’s effect, this includes prediction, adaptation, mitigation.
Risk Sharing
A form of community preparedness, whereby the community shares the risk posed and invest collectively to mitigate the impacts of future hazards.
The Park Model
Graphical representation of human responses to hazards. It shows the steps carried out in recovery after a hazard giving a rough indication of time frame.
Stages of the Park Model
Stage 1 (hours/days): Relief - Immediate local response, medical aid, search/rescue.
Stage 2 (days/weeks): Rehabilitation - Services begin to be restored, temporary shelters/hospitals, foreign aid.
Stage 3 (weeks/years): Reconstruction - Restoring the area to the same or better. Infrastructure rebuilt. Mitigation strategies.
Stages of the Hazard Management Cycle
Preparedness, Response, Recovery, Mitigation
Evaluate the Models
(Park Model and Hazard Mangement Cycle)
Both models do not take into account the socio-economic development of the region.
Vague in time frame
Plate tectonic theory
The lithosphere is broken into large slabs of rock called tectonic plates. The plates move due to convection currents in the atmosphere which push and pull the plates in different directions.
Convection currents occur when less dense magma rises, cools then sinks. the edges are plate margins.
Constructive plate boundaries
Plates pull apart
Oceanic: New land forms (sea floor spreading)
Continental: Rift valley (Graben)
Destructive plate boundary
Plates move toward eachother
Continental/Oceanic: ocean trench, fold mountains, composite volcanoes.
Oceanic: ocean trench, fold mountains, volcanoes, island arcs
Continental: fold mountains
Ridge Push
The slope created when plates move apart has gravity acting upon it as it is at a higher elevation. Gravity pushes the plates further away, widening the gap (gravitational sliding).
Slab pull
When the plate subducts, the plate sinking into the mantle also pulls the rest of the plate with it causing further subduction.
Conservative plate boundary
The parallel move in different directions or at different speeds no landforms are created but fault lines can occur
Hotspots
Areas of volcanic activity that are not related to plate boundaries. Hot magma plumes burn and rise through the weaker parts of the crust which can create volcanoes and islands.
The plume stay in one place but the plates continue to move which can create a chain of islands like Hawaii
Volcanic hazards
Lava flows, Lahar, Tephra, Toxic gases, Acid rain, Nuees Ardentes/ Pyroclastic flows.