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

  • Toe of a Slope

    “Toe” of a Slope Definition The “toe” of a slope is essentially the bottom, or baseline section, of the soil mass comprising the slope. It is also defined as the outermost margin of displaced material during a landslide. The toe of a slope is farthest away from the head scarp.

  • Design Methane Pressure (Soil Formation Pressure)

    Design Methane Pressure (Soil Formation Pressure) Design Methane Pressure or Soil Formation Pressure: As per the Los Angeles Department of Building and Safety (LADBS) Methane Code, Ordinance Number 175790, Design Methane Pressure means the highest observed measurement of soil formation pressure during the methane testing process. In fact, a Design Methane Pressure measurement that is…

  • 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…

  • Focus (Hypocenter)

    Focus (Hypocenter) Focus (Hypocenter): In the seismology branch of geology, a focus, or hypocenter, refers to the specific place where an earthquake rupture originates. The focus, or hypocenter, underlies the epicenter when an earthquake occurs at a dip-slip fault, strike-slip fault, oblique-slip fault, or listric fault. In the event of an earthquake, geologists, and seismologists…

  • Dry Strength

    Dry Strength “Dry Strength” is a value that represents the strength of a soil sample, when dry, as determined by the crushing test. There is a common geotechnical engineering laboratory procedure for determining the cohesiveness or plasticity of a sample with organic or inorganic clays and silts.  

  • Seismology

    Seismology Seismology: (seis·mol·o·gy) a branch of geology and geophysics that relates to earthquakes, including but not limited to their causes, effects, hazards, and mitigation techniques.  Seismologists at the United States Geological Survey (USGS) use cutting-edge technology to measure seismic wave properties and geological hazards that trigger them or are triggered by them. In turn, seismology…