tectonic hazards mark scheme answers

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Last updated 8:31 PM on 4/26/26
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26 Terms

1
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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)

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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

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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

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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

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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

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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

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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

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convection currents

  • heat rising and falling inside the mantle creates convection currents generated by radioactive decay in the core

  • these currents move the plates

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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)

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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

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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)

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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

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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

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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

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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

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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

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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

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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

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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

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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

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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

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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

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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

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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

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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.

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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