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  2. Soil liquefaction - Wikipedia

    en.wikipedia.org/wiki/Soil_liquefaction

    Although the effects of soil liquefaction have been long understood, engineers took more notice after the 1964 Alaska earthquake and 1964 Niigata earthquake. It was a major cause of the destruction produced in San Francisco's Marina District during the 1989 Loma Prieta earthquake, and in the Port of Kobe during the 1995 Great Hanshin earthquake.

  3. Liquefaction - Wikipedia

    en.wikipedia.org/wiki/Liquefaction

    The effects of soil liquefaction, seen after 2011 Canterbury earthquake. In geology, soil liquefaction refers to the process by which water-saturated, unconsolidated sediments are transformed into a substance that acts like a liquid, often in an earthquake. [6] Soil liquefaction was blamed for building collapses in the city of Palu, Indonesia ...

  4. Ground failure - Wikipedia

    en.wikipedia.org/wiki/Ground_failure

    The term ground failure is a general reference to landslides, liquefaction, lateral spreads, and any other consequence of shaking that affects the stability of the ground. This usually takes place as an after-effect of an earthquake, and is one of the major causes of destruction after an earthquake. Ground failures tend to happen almost every ...

  5. Sand boil - Wikipedia

    en.wikipedia.org/wiki/Sand_boil

    An example of this is during the 1989 earthquake in San Francisco when sand boils brought up debris from the 1906 earthquake. This process is a result of liquefaction. By mapping the location of sand boils that erupted in the Marina District during the 1989 Loma Prieta earthquake, scientists discovered the site of a lagoon that existed in 1906.

  6. Earthquake environmental effects - Wikipedia

    en.wikipedia.org/wiki/Earthquake_environmental...

    Coseismic liquefaction induced by one of the 2012 Emilia, Northern Italy, earthquakes. Secondary effects: mostly this is the intensity of the ground shaking (e.g., landslides, liquefaction, etc.). The importance of a tool to measure earthquake Intensity was already outlined early in the 1990s. [2]

  7. Soil-structure interaction - Wikipedia

    en.wikipedia.org/wiki/Soil-structure_interaction

    When a structure is subjected to an earthquake excitation, it interacts with the foundation and the soil, and thus changes the motion of the ground. Soil-structure interaction broadly can be divided into two phenomena: a) kinematic interaction and b) inertial interaction. Earthquake ground motion causes soil displacement known as free-field ...

  8. Feeling dizzy and nauseated after an earthquake? Here's why.

    www.aol.com/lifestyle/people-reporting-vertigo...

    More than 42% of the 3,656 people that Japanese researchers surveyed in the 12 weeks following massive earthquakes in Kumamoto in 2016 said they felt an “illusion sway” after the quakes.

  9. Seismic retrofit - Wikipedia

    en.wikipedia.org/wiki/Seismic_retrofit

    Seismic retrofitting is the modification of existing structures to make them more resistant to seismic activity, ground motion, or soil failure due to earthquakes.With better understanding of seismic demand on structures and with recent experiences with large earthquakes near urban centers, the need of seismic retrofitting is well acknowledged.