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why do people live in areas at risk of volcanic eruptions?
geothermal energy can be harnessed by using steam from underground heated by magma - can produce electricity such as in ireland
volcanic areas (hot springs) attract tourists - which creates employment and may have a multiplier effect
mining - magma and lava may contain minerals (gold, silver, diamonds, copper and zinc) - basalt can be used in construction + to build roads
fertile (nutrient rich) soil - produce crops and rich harvests
people believe the chances of volcano erupting are very slim
many people don’t have a choice as they can’t afford to live away from volcanoes as they provide jobs + their friends and families live there
some places are well prepared so people feel safe (confident in the defences)
why do people live in earthquake zones?
plate margins often coincide with favourable areas for settlement - such as coastal areas where there’s ports
offer job opportunities, such as san francisco and la
risk is outweighed by economic or social opportunities
engineering can make people feel safe - earthquake proof buildings (people are confident in the defences)
protection, planning and monitoring may be advances - potential risks are reduced
fault lines associated with earthquakes can allow water supplies to reach the surface
what are general reasons that people live in areas at risk of tectonic hazards?
they’ve always lived there - moving away would mean leaving family and friends
employed in the area - would have to find new jobs
people living in poverty have other priorities - money, food, security, family
people can’t afford to move - housing may be cheaper in some hazardous zones
primary effects of earthquakes
buildings collapse
communication links damaged or destroyed
loss of power / water supply
people may be injured or killed / trapped under rubble
people made homeless - accepted as primary
primary effects of volcanic eruptions
houses submerged under lava flow
properties destroyed by fire
people injured or killed
roads blocked by lava
trees/crops burnt or covered by lava
air pollution
ridge push
magma rises as the plates move apart
the magma cools to form new plate material
as it cools it becomes denser and slides down away from the ridge
this causes other plates to move away from each other
slab pull
the denser plate sinks back into the mantle under the influence of gravity
it pulls the rest of the plate along behind it
convection currents
heat rising and falling inside the mantle creates convection currents generated by radioactive decay in the core
these currents move the plates
processes causing volcanic activity at CONSTRUCTIVE MARGINS
two plates move apart
magma rises through the crust, and some can erupt producing volcanoes (usually gentle sided basic lava cones)
earthquakes at constructive margins as plates move apart
faults are formed at the margin and earthquakes can occur here - they are usually of low magnitude
some may be linked to volcanic activity
most happen at shallow depths below the surface where the plates are moving apart
processes causing volcanic activity at destructive margins
two plates move towards each other
the denser plate sinks below the lighter, less dense plate and melts in the subduction zone
hot magma rises up through the overlying mantle and crust, and some can eventually erupt out at the surface producing volcanoes
(magma becomes increasingly viscous or sticky as it rises to the surface, producing composite volcanoes which are steep sided and have violent eruptions)
earthquakes at destructive margins
as the two plates converge, pressure builds up
the rocks eventually fracture causing an earthquake - most happen at shallow depths below the surface where the plates collide
they also occur at greater depth, in the lower part of the subduction zone
earthquakes at conservative plate margins
plates move past each other (in opposite directions) or side by side moving at different speeds
as the plates move, friction occurs and plates become stuck
pressure builds up
when pressure is released, it sends out huge amounts of energy, causing an earthquake
earthquakes can be very destructive as they occur close to the earth’s surface
there are NO volcanoes at a conservative plate margin
why do earthquakes and volcanic eruptions occur at a DESTRUCTIVE PLATE MARGIN?
destructive plate margins occur when two tectonic plates move towards each other and one is subducted under the other
(or collision boundaries - if two continental plates collide, the pressure and strain may cause an earthquake)
if an oceanic and continental plate collide, the denser oceanic plate is subducted and sinks below the continental plate and into the earth’s mantle
this causes part of the mantle to melt and hot magma may rise up through the overlying mantle and lithosphere
this may eventually erupt out of the earth’s surface causing a volcano
(slab pull and gravitational movement of plates: the denser plate sinks into the mantle under the influence of gravity, which pulls the rest of the plate along behind it)
an earthquake may occur because as the plates converge, pressure builds up, the rock may fracture and the pressure is released as an earthquake
disadvantages of living in areas at risk of volcanic eruptions
volcanic eruptions can kill people and damage property
economic activity can suffer as it is hard for businesses to operate after an eruption
habitats and landscapes are damaged by lava flows
ash disperses in the air, and together with volcanic gases can affect breathing - it may cover the land, including fields, houses, roads, and industrial plants
pyroclastic flows can destroy houses and trees
eruptions may trigger tsunamis, which lead to destructive flooding of the coastline
disadvantages of living in areas at risk of earthquakes?
in seismic areas ground shaking causes bridges and buildings to collapse, windows to shatter, power lines to collapse, water/gas mains and sewers to fracture
immediate deaths and injuries result from crushing, falling glass, fire and transport accidents
people become homeless
slope failures set off avalanches
there may be panic, fear and hunger
longer term disadvantages include diseases spread from polluted water, civil disorder, looting, power cuts, reduced emergency services, unemployment, disability, loss of farmland and food production
how can planning reduce the effects of an earthquake / volcanic eruption?
prepare emergency aid and distribution
practise earthquake/volcano drills
plan evacuation routes
stockpile blankets, clean water and food
educate people so they know what to do if an earthquake or volcano happens
prepare hazard maps to show areas most at risk of damage
how can the risks of a tectonic hazard be reduced?
monitoring – recording physical changes, such as earthquake tremors around a volcano, to help forecast when and where a natural hazard might strike
prediction – attempts to forecast when and where a hazard will strike, this can be done to some extent for volcanic eruptions, but less reliably for earthquakes
planning – actions taken to enable communities to respond to, and recover from, natural disasters, through emergency evacuation plans and warning systems
protection - actions taken before a hazard strikes to reduce its impact, such as educating people or improving building design
how can monitoring and prediction reduce the risks of an earthquake?
using seismometers to monitor earth tremors, but specific times and locations are not possible to predict
how can protection reduce the risks of an earthquake?
constructing buildings so that they are safe to live in and will not collapse
rubber shock absorbers in the foundations to absorb the earth tremors
steel frames that can sway during earth movements
open areas outside of the buildings where people can assemble during an evacuation
how can planning reduce the risks of earthquakes?
hospitals, emergency services and residents may practise for an earthquake
they have drills in all public buildings so that people know what to do in the event of an earthquake - this helps to reduce the impact and increases their chance of survival
planning may also involve emergency evacuation plans
how can monitoring and prediction reduce the risks of volcanic eruptions?
measuring gas concentrations, using tiltmeters to monitor changes in the volcano’s surface
using seismometers to measure small earthquakes and tremors
thermal heat sensors to detect changes in the temperature of the volcano’s surface
how can protection reduce the risks of volcanic eruptions?
protection is difficult but it may be possible to use earth embankments or explosives to divert lava flows away from property
how can planning reduce the risks of volcanic eruptions?
hazard maps have been produced for many of the world’s most dangerous volcanoes, showing the likely areas to be affected
they can be used in planning to restrict certain land uses or to identify which areas need to be evacuated when an eruption is about to happen
immediate responses of a tectonic hazard? (first/emergency actions taken by people after an event)
providing water supplies, medicine, first aid + supplies essential to survival
the need to search for and rescue people, getting them to safety or to hospital
possibly moving inland or to higher ground if a tsunami
a need to try to provide medical help
ensure there is clean water (and food)
a need to bury the dead, often in mass graves to stop the spread of disease
all of this may require international aid with teams of sniffer dogs, heavy equipment, medical staff, provisions of water purifying tablets, blankets, setting up shelters, tents etc.
long-term responses (occur over weeks/months/years)
involve the need to rebuild houses, ideally using different materials and designs, to make them less easy to destroy
rebuild public buildings and infrastructure
may be a requirement to rebuild roads and railways
ensure jobs are being created - such as for local builders, electricians and carpenters
help people to come to terms with a traumatic event and loss of parents and children
to predict and prepare for future events and introduce measures to reduce the effects of future hazards