MECHANISM OF SEISMOGENIC LIQUEFACTION LANDSLIDES

Authors

  • I.A. Torgoev Institute of Geomechanics and Subsoil Development of the National Academy of Sciences of the Kyrgyz Republic Author

Keywords:

seismogenic landslide, landslide-flow, soil liquefaction, loess-like loam, Hindu Kush earthquakes, pore pressure, stability coefficient

Abstract

This article examines the genesis and development dynamics of large-scale seismogenic liquefaction landslides using the catastrophic Sary-Bulak landslide near the town of Kok-Jangak as an example. The author analyzes in detail the triggering effects of long-duration low-frequency vibrations from deep-focus Hindu Kush earthquakes on metastable loess-like loams under conditions of high groundwater pressure. Based on geotechnical testing and computational modeling using the SLIDE 4.0 software, the physical and mechanical mechanism behind the sharp increase in pore pressure and the drop in effective stresses, which led to the transition of the soil mass to a fluid state and its extremely long-distance movement, is revealed.

References

1. Ниязов Р.А. Оползни Узбекистана (тенденции развития на рубеже ХХI века). – Ташкент: ГИДРОИНГЕО, 2009. – 208 с.

2. Torgoev I.,NijazovR.,Havenith H.-B. Tien-Shan landslides triggered by earthquakes in Pamir-Hindukush zone // Proceedings of the second world landslide forum. Roma, 2011 (in Press).

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Published

2026-08-26