Liquefaction and the 1992 Roermond earthquake, the Netherlands
Abstract
The scanty information available on liquefaction phenomena during the Roermond earthquake does not allow firm conclusions on the technical significance of these phenomena. However, speculations based on applied mechanics principles justify a few conclusions on what happened and what did not happen. First, the presence of fracture vents and sand boils agrees well with the estimated earthquake magnitude ML = 5.8-5.9; second, the rare occurrence of sand boils and the absence of visible settlements indicate that liquefaction was not an important phenomenon during the earthquake; third, damage of farms due to liquefaction seems absent. This observation is in agreement with the theoretical analysis of responses of the farm foundations to liquefaction. If the area affected by liquefaction had exceeded some 1% of the total area, significant damage would have been detectable. The low ground water tables during the time of the earthquake have most probably prevented extensive damage.
Authors contributing to Netherlands Journal of Geosciences retain copyright of their work, with first publication rights granted to the Netherlands
Journal of Geosciences Foundation. Read the journal's full Copyright- and Licensing Policy.