The challenge of natural hazards Flashcards
(63 cards)
Atmospheric (hydro-meteorological) hazards
hazards that are caused by the weather
- droughts
- floods
- tropical storms
- acid rain
Geological (geophysical) hazards
hazards caused by tectonic plates
- tsunami
- earthquakes
- volcano
- landslides
what’s the relation between natural disasters and natural hazards?
natural disasters are events caused by nature that have actually happened whereas natural hazards are events that have/ can occur that can disrupt humans or damage property
Natural disasters
events caused by nature that can cause disruption to human life and destroy property/ possessions
Why may people choose to live somewhere vulnerable to a natural hazard?
- we can’t accurately predict the hazard (its timing, magnitude and location) so its worth the risk to stay as there is a small chance of being effected.
- we can’t move, some people cannot move due to it being more expensive to do so or they aren’t socially able. Language can be difficult when moving to another country and some are not educated enough to be able to move away.
- don’t want to go, perhaps they strongly believe in their defences or they are optimistic that it won’t happen.
- worth the risk perhaps if the jobs there have high salaries or the land has good natural resources.
What factors affect the hazard risk of natural hazards?
- vulnerability: a densely populated area has a greater risk than a sparsely populated area, timing during the day
- capacity to cope: normally HICs cope better due to their advancements in technology that can predict hazards and issue warnings and they have advanced infrastructure made to cope with the conditions
- nature of the natural hazards: some natural hazards are easier to monitor and predict (tropical storms rather than earthquakes), the magnitude of the hazard and how frequent it is.
how vulnerability affects natural hazard risks:
- natural factors (height of land, geology, and location): soft rock in an earthquake poses more risk as it is more unstable, a funnel shaped coastline can increase the likeliness of a storm surge.
- population density and distribution: greater density = greater risk
how capability to cope affects natural hazard risks:
- management to reduce (prediction, planning and protection): we can monitor some hazards better than others and issue out evacuations, we can build houses to suit the conditions, we can prevent as much damage by carrying out rules
- education on what to do in the circumstances
- how much money can be invested into advanced preparation; HICs
how nature affects natural hazard risks:
- time: when asleep or during working hours = more risk
- frequency: more frequent = less hazard as people become more educated and aware, they aren’t taken by surprise
- magnitude
What 2 factors make tectonic plates movie:
- convectional currents
- ridge push and slab pull
convectional currents
radioactive decay in the mantle produces heat which heats up the magma. as the magma gets hotter it becomes less dense and rises to the surface (crust). as it rises it cools and is forced to disperse in different directions beneath the crust, causing the plates to move in the same convectional current. as the magma cools at the surface, it solidifies and becomes denser, sinking back down to the mantle to melt again and repeat.
ridge push and slab pull
through the cracks in the curst, magma (under lots of pressure from the convectional current in the mantle) escapes from the gap, erupting. this magma now at the surface (lava) cools and creates new plate area, causing the plates to be pushed apart.
slab pull is when at the other end of the plate, the denser plate subjects under the lighter one under gravity. it melts into the mantle feeding the convectional currents which pulls the rest of the plate with it.
Describe how the Mercalli scale measures earthquakes:
the Mercalli scale is a scale of 12, 1 being least destructive and 12 being devastating. this is based on the effects of the earthquake (people’s opinions and observation) and doesn’t measure the energy of the earthquake.
Describe how the Moment scale measures earthquakes:
the Moment scale uses a logarithmic scale from 1 to 10 (1 being the weakest). it uses seismographs to measure the seismic waves given off from the focus. it shows both the intensity of the earthquake but also shows how often the intensity occurs in the world.
Describe the composite volcanoes:
Composite volcanoes occur at destructive plate margins where a denser oceanic crust subducts under a lighter continental crust. as the oceanic crust melts into the mantle, it creates gas pockets and lots of pressure which collects in magma chambers near the surface of the crust. as the pressure builds, the magma may be forced out of vents in the crust, causing violent and infrequent eruptions of thicker magma. this magma travels slowly due to its high silica content so travels shorter distances before setting, creating taller and steeper sloped volcanoes. some eruptions may be pyroclastic flows (flows of ash, hot steam and rocks) therefore composite volcanoes are made up of layers of both lava and ash.
Describe shield volcanoes:
Shield volcanoes occur at constructive plate boundaries where the tectonic plates are diverging from another. this causes the magma from the mantle to erupt out from the gap, this magma is more liquid, so it erupts frequently and spreads quickly across the land forming thinner layers. its gas bubbles are able to easily expand so they erupt gently with no explosions. this makes these volcanoes low and gently sloping.
Explain how volcanic eruptions occur at destructive and constructive plate boundaries:
at destructive plate boundaries, the denser heavier oceanic crust subducts beneath the lighter less dense continental crust into the mantle. as the oceanic crust subducts into the mantle it melts into magma, creating pressure as gases and magma build up. this collects into a magma chamber beneath the surface and rises through cracks in the crust called vents. the magma erupts out of the curst as lava forming a volcano.
in constructive margins, magma rises through the gap -as lava- created between the tectonic plates as they move apart from each other, creating a volcano.
Lahars
Lahars are fast moving flows of mud made out of settled ash on a volcano which can be triggered by heavy rainfall events. as the layers of ash receive the rain, they become unstable and can collapse, sending flows down the volcano at high speeds, often picking up debris on the way carrying them for 10’s of miles.
Pyroclastic flows
these are flows of hot steam, ash and rocks that avalanche down a volcano.
volcanoes
openings in the crust allow hot magma, ash and gases to escape from the mantle
earthquakes
short sudden intense shocks periods that are ground shaking.
they are caused by the pressure that builds up between two plate margins that are passing each other (at conservative boundaries). as they pass each other, they overcome friction which builds their pressure. eventually, they will jerk past each other sending shocks and/or seismic waves through the crust from the focus to an epicentre on the crust. these vibrations are an earthquakes.
Where is Haiti?
Haiti is an island country located in Hispaniola, west of the Dominican Republic in the Caribbean. it sits on the conservative fault line between the Caribbean and North American plate resulting in the 2010 earthquake of a 7.0 magnitude.
Why was Haiti more heavily affected by the earthquake than Christchurch’s 2011 earthquake?
though Christchurch’s focus was shallower and its epicentre was nearer to the city, it experienced less severe impacts because in Haiti…
- 86% of the population live in slum conditions, whose housing was improper and underdeveloped to withstand earthquakes, hence many collapsed leaving people homeless and jobless.
- it had a long history of ineffective and unstable governance, therefore the responses after the earthquake weren’t organised enough leading to slow recovery.
- it is the poorest country in the western hemisphere, with 70% living under $2 a day, this means that funding the recovery was difficult as the country couldn’t afford to implement better infrastructure, making it vulnerable to future events.
compare the effects and responses of Haiti and Christchurch
Haiti primary effects - 220,000 died
Christchurch primary effects - 185 died
Haiti secondary effects - 10 months later, they experienced outbreaks of cholera, $8 billion cost
Christchurch secondary effects - school has to close for 2 weeks due to the damages, $28 billion cost
Haiti short term response - 10,000 troops were sent from the USA, however these were sent for defence purposes to tame communities expecting violence, so primary aid wasn’t distributed and unplanned.
Christchurch short term response - government zoned areas to assess the damage and relocated patients from the hospital to surrounding hospitals to allows victims to be cared for immediately.
Haiti long term response - the new development of advanced infrastructure was eventually introduced but was slow, one year after 1million were still homeless.
Christchurch long term response - New Zealand governments supplied temporary housing and 10,000 affordable houses were constructed.