Management Strategies (DP IB Geography)

Revision Note

Pre-event Management Strategies - Volcanoes

  • There are signs warning of an eruption before most volcanic eruptions

  • Pre-event management of volcanoes includes monitoring these signs so that people can be evacuated and warned 

  • Volcanologists (scientists who study volcanoes) monitor changes using GPS, tilt meters, satellites, seismometers and gas detection

  • Signs of an eruption include:

    • Magma rising, which can be detected by heat sensors and satellites

    • Changes in surface level as rising magma causes bulges

    • Increased emissions of sulphur dioxide and other gases

    • Increased seismic activity caused by magma movement detected by seismometers

Methods of monitoring volcanoes

Diagram depicting various volcanic monitoring methods: gas detection, tiltmeters, GPS, cameras, thermal imaging via helicopter, satellite, and earthquake sensors.
Methods of monitoring volcanoes
  • Improved prediction of volcanic eruptions has led to a decrease in death tolls 

Diversion channels

  • Lava flows can be managed by constructing diversion channels 

  • These are used to direct the flow away from economically valuable areas or areas of population

Pre-event Management Strategies - Earthquakes

  • It is not possible to predict earthquakes:

    • An understanding of tectonic activity can help scientists identify areas most at risk

    • Over 90% of earthquakes occur on or near plate boundaries

    • Building design and construction can be used to reduce the impact

Earthquake resistant building design

Diagram of an earthquake-resistant building with weights on the roof, automatic window shutters, sway-supporting steel frames, shock absorbers, and fire-resistant materials.
Earthquake resistant building design
  • Hazard mapping can also be used to predict areas at highest risk

  • Land use zoning can then ensure that valuable buildings are not built in these areas

Tsunami

  • For earthquake-induced tsunamis, scientists are unable to predict the earthquake itself

  • When the earthquake happens, this will be detected by the global network of seismometers, which will locate the epicentre of the earthquake

    • Ocean monitoring technology can then be used to detect a tsunami

    • Warnings can then be issued to coastal areas that may be affected

Tsunami warning system

Diagram showing tsunami warning system: seabed sensors detect pressure changes, data sent to surface buoy, then to satellite, and ground stations alert the public.
Tsunami warning system
  • Sea walls have also been built to reduce the impact of tsunami

    • After the 2011 Tokohu tsunami in Japan, the height of the sea wall was increased to over almost 15 meters in places

Pre-event Management Strategies - Mass Movement

  • The management of mass movement needs to control the factors that affect the risks, including:

    • Slope angle and stability

    • Drainage

    • Human activities

    • Erosion

Terracing or re-grading of slopes

  • Terracing or re-grading reduces the angle of the slope 

Revegetation

  • Stabilises the slope material, increasing the amount of stress that the slope can withstand

  • Reduces slope saturation by take-up of water through the roots and increased interception

  • Decreases erosion, which affects the stability of the slope

Improving drainage

  • Water makes slopes more unstable

  • Improved drainage reduces saturation of the slope 

  • This reduces the weight of the material and therefore the risk of mass movement

Stabilisation structures

  • Use of pinning:

    • Steel rods are drilled into the slope to support the weight of the slope

    • Bolts can also be used to transfer the weight from the surface to the interior of the slope

  • Pinning is often used in combination with netting, which contains any falling material 

  • Shotcrete shoring is when a mixture of cement and aggregate is applied to the slope; this strengthens the slope and reduces erosion

  • Retaining walls and gabions, which hold the slope in place

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