IB Geography • Section 2

Geophysical Hazard Risks

SYLLABUS LINK

How geophysical systems generate hazard risks for different places

Restored from the original AdornGeo Weebly page • syllabus order preserved

01

Distribution of Geophysical Hazards

IB SYLLABUS BULLET

The distribution of geophysical hazards (earthquakes, volcanoes, mass movements).

Start with pattern before explanation. Earthquakes and volcanoes concentrate around active plate margins, while hot spots create important volcanic exceptions. Mass movements have a wider distribution because relief, geology, water, seismic shaking and human modification all influence slope stability.

Key teaching ideas
  • Earthquakes occur at all plate-margin types, with a major concentration around the Pacific Ring of Fire and the Alpine–Himalayan belt.
  • Most volcanoes occur at constructive and destructive margins; hot spots explain intraplate chains such as Hawaii.
  • Mass movements cluster in steep highland, tectonically active and coastal environments, but rainfall and human disturbance can create risk far from plate margins.
  • A hazard map shows where events may occur; it does not by itself show exposure, vulnerability or disaster risk.
Key vocabulary
spatial distributionhazardexposureplate marginRing of Firehot spotmass movementrisk map
STUDENT TASK

Enquiry 1 — From pattern to process

  1. Read the new Distribution of Geophysical Hazards briefing, then highlight one claim about earthquakes, volcanoes and landslides that the live maps can test.
  2. Open the original A3 map and use the live earthquake, volcano and landslide sources to add three different symbols or layers.
  3. Annotate the Pacific Ring of Fire, the Mid-Atlantic Ridge, the Alpine–Himalayan belt and two intraplate hot spots.
  4. Write one PEEL paragraph for each hazard explaining its main distribution, physical cause and at least one exception.
  5. Add a final warning explaining why event distribution cannot be treated as a complete map of risk.
Global volcano distribution and tectonic plates
Recovered AdornGeo map: compare the global pattern of volcanoes with plate margins and identify the hot-spot exceptions.
Plate-tectonic cross-section
Use the recovered cross-section to connect surface hazard patterns to the processes beneath them.

Watch: Types and distribution of geophysical hazards

Watch: Plate tectonics and the global hazard pattern

MAPPING ACTIVITYA3 blank world-map outline

LIVE EARTHQUAKE MAPUSGS real-time earthquake distribution

LIVE VOLCANO MAPGlobal volcano types and locations

02

Hazard Magnitude, Frequency & Recurrence

IB SYLLABUS BULLET

The relevance of hazard magnitude and frequency/recurrence for risk management.

Risk managers need more than a record of the largest event. Magnitude describes event size, frequency describes how often events occur, and recurrence or return interval estimates the long-term likelihood of a similar event. These measures are uncertain and must be read together.

Key teaching ideas
  • Earthquake magnitude is commonly reported using the Moment Magnitude Scale; each whole-number rise represents ten times greater recorded amplitude and roughly 32 times more energy release.
  • The Modified Mercalli scale describes observed intensity and therefore varies from place to place during the same earthquake.
  • Volcanic explosivity can be compared using the VEI, while mass movements need a profile that includes volume, speed, duration and spatial extent.
  • Frequent low-magnitude events may support awareness and building standards; rare high-magnitude events are harder to remember, finance and plan for.
  • A recurrence interval is a probability based on an incomplete record, not a prediction that an event will happen on schedule.
Key vocabulary
magnitudeintensityMoment Magnitude ScaleModified MercalliVEIfrequencyrecurrence intervalreturn periodhazard profile
STUDENT TASK

Enquiry 2 — Has the world become safer?

  1. Study the century of disaster deaths. Describe the overall change in annual mortality, then identify two major exceptions to the trend.
  2. Compare earthquake and volcanic deaths. Suggest why earthquake bubbles remain more prominent even though both hazards are concentrated near plate margins.
  3. Challenge the graphic: explain why deaths alone cannot show the full severity of a disaster or prove that hazard frequency has fallen.
  4. Create a hazard-profile radar diagram using magnitude, frequency, speed of onset, duration, areal extent and predictability.
  5. Compare a high-frequency, lower-magnitude event with a rare, high-magnitude event and identify the different planning needs.
  6. Answer the IB-style prompt: Explain how frequency of past events and magnitude of past events can each help a community manage risk.
Global deaths from disasters over more than a century
Read bubble size as estimated annual deaths. Use the earthquake and volcanic rows to distinguish changing disaster mortality from changes in the physical occurrence of hazards.

Watch: Moment magnitude explained

Watch: Richter scale and modern earthquake measurement

Watch: Comparing earthquake energy release

DATA EXPLORERNatural disaster events by type

EARTHQUAKE CATALOGUEUSGS magnitude, depth and recurrence explorer

03

Human Risk Factors

IB SYLLABUS BULLET

Geophysical hazard risk as a product of economic factors (levels of development and technology), social factors (education, gender), demographic factors (population density and structure) and political factors (governance).

A physical event becomes a disaster through exposure and vulnerability. Use the risk relationship as an organising device rather than a fixed calculation: risk rises when hazard and exposure are high, and falls when vulnerability is reduced and coping capacity grows.

Key teaching ideas
  • Economic development can reduce mortality through safer buildings, monitoring, insurance and emergency capacity, while also increasing the value of exposed assets.
  • Education, risk perception, language, gender roles and access to warnings influence who receives information and who can act on it.
  • Dense populations and dependent age structures can increase exposure and complicate evacuation, although density can also improve access to services.
  • Governance shapes building-code enforcement, land-use planning, public trust, corruption, emergency coordination and the fair distribution of aid.
  • Vulnerability varies within every country and city; national income alone never explains the complete pattern.
Key vocabulary
riskvulnerabilityexposurecapacity to copegovernancepreparednessrisk perceptionintersectionality
STUDENT TASK

Enquiry 3 — Vulnerability ranking challenge

  1. Working in pairs, cut up or digitally inspect the 12 vulnerability factors. Sort them into economic, social, demographic, political and environmental groups; allow justified overlaps.
  2. Rank the factors for an earthquake-prone megacity, then repeat for an isolated volcanic community. Record which rankings change and why.
  3. Add one missing factor and challenge one card whose wording is too simple. For example, density can increase exposure but may also improve access to services.
  4. Choose one earthquake-prone city and identify its hazard, exposed people and assets, vulnerabilities and capacities.
  5. Sort your evidence into economic, social, demographic and political factors; show interactions with arrows.
  6. Redesign one factor as a practical risk-reduction intervention, naming the stakeholder with the power to act.
Twelve factors that may affect vulnerability
Sort, rank and critique the cards. The aim is not one correct order, but a defensible place-specific explanation of how factors interact.

Watch: UNDRR: the three components of disaster risk

Watch: UNDRR: mapping vulnerability to disasters

Watch: Vulnerability, disasters and older people

RISK PROFILERThinkHazard — compare hazard levels by place

GLOBAL RISK INDEXINFORM risk, vulnerability and coping-capacity explorer

Quizlet: IB Geography Option D — Geophysical Hazards

04

Geographic Factors Affecting Event Impacts

IB SYLLABUS BULLET

Geographic factors affecting geophysical hazard event impacts, including rural/urban location, time of day and degree of isolation.

The same magnitude does not produce the same impact everywhere. Settlement form, daily rhythms and connectivity change exposure, rescue access and the speed at which secondary impacts spread through infrastructure and supply networks.

Key teaching ideas
  • Urban events may expose dense populations, high-rise buildings and interdependent infrastructure; rural events may affect fewer people but leave dispersed communities harder to reach.
  • Time of day changes occupancy: homes, schools, workplaces, roads and public transport contain different populations at different times.
  • Isolation can delay warning, search and rescue, medical care, relief and reconstruction; damaged bridges, ports and communications can create new isolation after an event.
  • Physical geography interacts with these factors: steep relief, unstable sediment, coastlines and weather conditions may intensify secondary hazards and constrain access.
  • Impacts should be assessed through human well-being as well as deaths and financial loss, including health, shelter, education, livelihoods, security and social connection.
Key vocabulary
ruralurbantime of dayisolationaccessibilityinfrastructure cascadesecondary hazardhuman well-being
STUDENT TASK

Enquiry 4 — Same hazard, different place

  1. Read Geographic Factors Affecting the Impacts of Geophysical Events and build a cause–effect table for Christchurch, Nepal, Mexico City, Tōhoku, Pinatubo and Volcán de Fuego.
  2. Apply the same earthquake scenario to a dense city centre, a peri-urban settlement and an isolated mountain community.
  3. Repeat the scenario for daytime and night-time, identifying who is exposed and which services are operating.
  4. Draw an impact cascade from ground shaking to transport, power, water, communications, health care and livelihoods.
  5. Write a reasoned judgement: Which geographic factor matters most? Use two contrasting named places and explain when your judgement would change.
Earthquake process and exposed places
Return to the recovered process diagram, then add the human geography that turns ground shaking into contrasting impacts.
Liquefaction and local ground conditions
Local sediment and water conditions show why impacts can vary sharply within one urban area.

Watch: Earthquakes and social factors — IB Geography

Watch: UNDRR: four pillars of an early-warning system

POPULATION MAPWorldPop — compare settlement density and isolation

DISASTER MAPPINGHumanitarian OpenStreetMap live project map