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Earth and geophysical science

Geoscience studies the composition, structure and dynamics of the solid Earth, including earthquakes, volcanoes, landslides and subsurface resources. It informs where and how often geological hazards occur and how they cascade into infrastructure and supply disruption. Climate and Hazards stewards this page for the Nexus Consortium.

01In brief

The short answer.

Geoscience studies the composition, structure and dynamics of the solid Earth, including earthquakes, volcanoes, landslides and subsurface resources. Geoscience sets ground-shaking and ground-failure inputs for building codes, siting and catastrophe models. In the Nexus Consortium, Climate and Hazards stewards its canonical page, and 4 other platforms apply it, including Disaster Resilience and Recovery as well as Cities and Built Environment.

02Geography

Disaster exposure and reach in Chile.

Where response must travel furthest from a large city, with the roads, airports and ports that carry relief, shown for Chile as an example geography for this subject.

Where response must travel furthest from a large city, with the roads, airports and ports that carry relief.Indicator derived from Natural Earth at map scale; a screening view, not an assessment.
GCRI · institution · fieldDESIGN FIGURE
03The method

What earth and geophysical science covers.

  1. 01

    Core methods

    seismic hazard analysis; geological mapping; geodetic deformation analysis; volcanic monitoring; slope stability analysis; subsurface imaging.

  2. 02

    Data and instruments

    seismometer networks; satellite radar interferometry; global navigation satellite system stations; boreholes and core samples; geological survey maps.

  3. 03

    Validation

    Hazard models are tested against historical and paleoseismic catalogues and observed ground motions. Deformation estimates are cross-checked between independent geodetic techniques.

  4. 04

    Limits

    Catalogues are short relative to recurrence intervals of large events. Fault interactions and triggering are difficult to predict deterministically.

  5. 05

    Use in risk decisions

    Geoscience sets ground-shaking and ground-failure inputs for building codes, siting and catastrophe models. It identifies where single geological events can disrupt multiple networks at once.

04Reference practice

Seismic and volcanic hazard practice is shared openly.

ReferenceWhat it sets
Global Earthquake Model (OpenQuake)Open probabilistic seismic hazard and risk modelling
USGS Earthquake Hazards ProgramGlobal earthquake catalogues and ShakeMaps
Smithsonian Global Volcanism ProgramVolcano and eruption records
UNDRR-ISC Hazard Information ProfilesStandard definitions of geological hazards
05In systemic risk work

One rupture, many networks.

Geological events are spatially concentrated and sudden, so they test many networks at the same moment: roads, pipelines, power, telecoms and ports in one region. In systemic analysis the value of geoscience is the shared event set: a single catalogue of plausible ruptures applied to every network, rather than each sector using its own hazard map with different assumptions.

  • Apply one stochastic event set across sectors so correlated damage appears.
  • Include secondary hazards: landslides, liquefaction, tsunami and fire following.
  • State catalogue completeness; large events have recurrence intervals longer than the instrumental record.
  • See Disaster Resilience and Recovery for recovery applications.
07Stewardship

Who maintains this page.

Climate and Hazards stewards earth and geophysical science: it keeps this description current and reviews how the method is applied across the platforms.

08Key terms

Terms used on this page.

Each term as this page uses it. Where a standard-setting body defines the term, the wording follows that body.

TermDefinition
Ground motion modelAn equation estimating shaking at a site from magnitude, distance and site conditions.
Logic treeA structure for weighting alternative models to represent uncertainty in hazard.
InSARInterferometric synthetic aperture radar, which measures ground movement by comparing radar images taken at different times.
Slip rateThe average rate at which the two sides of a fault move past each other over geological time.
09Sources

Where this page's references lead.

The bodies and documents this page is read against. Status and editions change; each link goes to the issuing body.

11Questions

Questions and answers.

Why does one institution host every method page?
GCRI hosts the STEM Commons so that each method has one canonical description. Platforms link to it rather than repeat it, which keeps definitions consistent.
How do I suggest a correction to a method page?
Write to integrity@therisk.global with the passage and the reason.
The Global Centre for Risk and Innovation

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The current service level is R0: information and enquiries. An enquiry receives a reference and names the next step; applications, payments, compute allocations and registrations open only when their team, terms and review capacity exist.

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