Seismic Risk Definition

Seismic Risk Definition

Seismic risk is the probability that a subject site will be adversely affected by any seismic hazard, such as an earthquake. Seismic risk tends to increase in areas that are more earthquake-prone and vulnerable to damage. And vulnerability refers to the potential impact on people, as well as properties. For instance, places that are densely populated, and have numerous buildings that are not structurally sound to withstand an intense seismic event.

While the descriptions of seismic risk hazards are relatively straightforward, a seismic risk assessment is a professional service that provides a detailed investigation and report of the matter. Seismic risk assessments are an important part of the real estate due diligence process. For these reasons, licensed professional geologists are often employed to conduct a seismic risk assessment that will meet the specific needs of the property owner or developer.

Seismic Hazard

Seismic hazard refers to the natural phenomenon of earthquakes, or earthquake-induced tsunamis, landslides, avalanches, sinkholes, and more. Thus, seismic risk is determined by the likelihood that an earthquake could negatively impact the people and property where such a hazard occurs. For example, consider two areas that are equally prone to earthquakes. And one location lies in an undeveloped area, while the other is within a densely populated and developed city. While the seismic hazard occurrence may be equal at both sites, the seismic risk is greater in the second scenario, because more people and property are vulnerable to damage.

Even more specifically, professionals can assess two different cities with equal seismic hazards and equal populations.  To illustrate, if one city comprises structures that are more structurally sound, then that city would have lower seismic risk because its buildings are less vulnerable to damage during a catastrophic event.

 

Similar Posts

  • |

    Geologic Time Scale

    Geologic Time Scale The Geologic Time Scale is an international system used by geologists to classify and identify major geologic events and formations. The geologic timescale essentially categories the earth’s entire geologic (and biologic) history, within a series of defined eons, eras, periods, epochs, and ages. Updates & Maintenance The geologic time scale is continuously…

  • Normal Fault Definition

    Normal Fault Normal Fault: In the field of geology, a normal fault is a type of dip-slip fault where the hanging wall moves downwards from the footwall. The average dipping angle of a normal fault ranges from 45 to 90 degrees. Normal faults are the opposite of reverse faults. Detachment Fault Detachment Fault: A detachment…

  • Asthenosphere

    Asthenosphere Asthenosphere: The asthenosphere underlies the lithosphere. The Asthenosphere comprises the upper mantle, where isostatic adjustments are made, and where magma is generated. It is also in this part of the earth, where seismic waves strongly attenuate.

  • Translational Slide Definition

    Translational Slide Landslide Translational Slide: In the seismology branch of geology, a translational slide is a type of landslide movement that occurs predominantly along a planar surface. Alternatively, this movement can occur along gently undulating surfaces. For instance, the Palona Schist metamorphic bedrock on the eastern embankment of the former St. Francis Dam comprises an…

  • Juvenile Water

    Juvenile Water Juvenile Water: In geology, juvenile water is water derived directly from magma, introduced into the Earth’s surface through geological processes such as magmatic and volcanic activity. Since juvenile water is derived from Earth’s center, its characteristics, are associated with higher temperatures and pressures.

  • Aphanitic

    Aphanitic Definition Aphanitic: In geology, the term aphanitic describes the texture of plutonic or volcanic igneous rocks, with grains that are not visible to the naked eye. In fact, an aphanitic texture is usually the result of faster cooling and solidification of liquid magma.