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- W623403748 abstract "On june 15th, 1995, an earthquake of magnitude Ms 6,1R occured offshore of the Aigion town in the Western Gulf of Corinth. An offshore survey using a 3.5 kHz subbotom profiling system, which carried out fifteen days after the main shock has shown that the earthquake caused a small-size subaerial to submarine landslide in the Eliki fan delta deposits. Further examination of the landslide, using a side scan sonar system and R.O.V for the visual inspection of the seafloor to map the complex seafloor morphology in and adjacent to the landslide, has shown that the Eliki submarine landslide is a complex low-angle translatory slide less than 5 m deep and that the sliding took place over a single basal glide plane dipping at about 1o. The instability mechanism that triggered the landslide is liquefaction of a subsurface horizon at a depth of 5 m as suggested by the presence of sand and water injection features (sand boils) in the beach near the slide site and the conical depressions observed on the seafloor. Gas expulsions from the liquefied horizon perhaps enhanced the failure as suggested by the presence of gas charged sediments under the sliding plane and the rising of bubbles in the water column as observed by the fishermen." @default.
- W623403748 created "2016-06-24" @default.
- W623403748 creator A5083793739 @default.
- W623403748 date "2008-03-13" @default.
- W623403748 modified "2023-09-23" @default.
- W623403748 title "Μελέτη της παράκτιας κατολίσθησης των Νικολέϊκων που προκλήθηκε από το σεισμό του Αιγίου 6,1 R (1995)" @default.
- W623403748 hasPublicationYear "2008" @default.
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