Geological hazard
A geologic hazard or geohazard is an adverse geologic condition capable of causing widespread damage or loss of property and life. These hazards are geological and environmental conditions and involve long-term or short-term geological processes. Geohazards can be relatively small features, but they can also attain huge dimensions and affect local and regional socio-economics to a large extent.
Sometimes the hazard is instigated by the careless location of developments or construction in which the conditions were not taken into account. Human activities, such as drilling through overpressured zones, could result in significant risk, and as such mitigation and prevention are paramount, through improved understanding of geohazards, their preconditions, causes and implications. In other cases, particularly in montane regions, natural processes can cause catalytic events of a complex nature, such as an avalanche hitting a lake and causing a debris flow, with consequences potentially hundreds of miles away, or creating a lahar by volcanism.
Marine geohazards in particular constitute a fast-growing sector of research as they involve seismic, tectonic, volcanic processes now occurring at higher frequency, and often resulting in coastal sub-marine avalanches or devastating tsunamis in some of the most densely populated areas of the world
Such impacts on vulnerable coastal populations, coastal infrastructures, offshore exploration platforms, obviously call for a higher level of preparedness and mitigation.
Speed of development
Sudden phenomena
Sudden phenomena include:- avalanches and its runout
- earthquakes and earthquake-triggered phenomena such as tsunamis
- forest fires leading to deforestation
- geomagnetic storms
- gulls associated with cambering of valley sides
- ice jams on rivers or glacial lake outburst floods below a glacier
- landslide
- mudflows
- pyroclastic flows
- rockfalls, rock slides, and debris flows
- torrents
- liquefaction
- volcanic eruptions, lahars and ash falls.
Slow phenomena
- alluvial fans
- caldera development
- geyser deposits
- ground settlement due to consolidation of compressible soils or due to collapseable soils
- ground subsidence, sags and sinkholes
- sand dune migration
- shoreline and stream erosion
- thermal springs
Evaluation and mitigation
- Geologic hazards may be avoided by relocation. Publicly available databases, via searchable platforms, can help people evaluate hazards in locations of interest.
- Mapping geohazards using conventional or remote sensing techniques can also help identify suitable areas for urban development.
- The stability of sloping earth can be improved by the construction of retaining walls, which may use techniques such as slurry walls, shear pins, tiebacks, soil nails or soil anchors. Larger projects may use gabions and other forms of earth buttress.
- Shorelines and streams are protected against scour and erosion using revetments and riprap.
- The soil or rock itself may be improved by means such as dynamic compaction, injection of grout or concrete, and mechanically stabilized earth.
- Additional mitigation methods include deep foundations, tunnels, surface and subdrain systems, and other measures.
- Planning measures include regulations prohibiting development near hazard-prone areas and adoption of building codes.
Earth observation of geohazards