Abstract

A quick clay slide in Gjerdrum, Norway, occurred at 4 a.m. on 30th December 2020, killing 10 people and destroying houses, roads, and other infrastructures. Approximately, 1.35 million cubic meters of clay were released, a large volume liquefied, and debris was transported almost 2 km that the slide was initialized in downstream. An investigation following the slide determined that the slide was initialized in a 30 m high slope after 2-to-2.5 m vertical erosion in a small creek running along the toe of the slope. After the initiation, the slide developed retrogressively in the order of 500 m backward and sideways over a period of about 2 min. A conventional geotechnical slope stability analysis explains the initial slide. However, more advanced numerical tools are needed to simulate the retrogressive mechanism and the debris flow. The aim of the paper is to demonstrate a 3D material point method model to capture some of the mechanisms involved from initiation until the debris comes to rest and how this method can be used to reproduce and study the processes involved in large deformation landslides. © 2024 The Author(s).