Investigation of landslide triggers on Mount Oku, Cameroon, using Newmark displacement and cluster analysis

• Published in: Geoenvironmental disasters 2024-12, Vol.11 (1), p.32-21, Article 32
• Main Authors: Djukem, D. L. W., Braun, A., Fan, X., Wouatong, A. S. L., Fernandez-Steeger, T. M., Havenith, H. B.
• Format: Article
• Language: English
• Subjects: Cameroon volcanic line; Cluster analysis; Depth; Earth and Environmental Science; Earth Sciences; Earth sciences & physical geography; Earthquake; Earthquakes; Environment; Environmental Science (miscellaneous); Environmental Science and Engineering; Factor of safety; Geoecology/Natural Processes; Geography; Geography, Planning and Development; Geological hazards; Geotechnical Engineering and Engineering Geology; Groundwater; Hazard assessment; Hazard identification; Landslides; Landslides & mudslides; Management, Monitoring, Policy and Law; Mount Oku; Natural Hazards; Newmark displacement; Physical, chemical, mathematical & earth Sciences; Physique, chimie, mathématiques & sciences de la terre; Precipitation; Rainfall; Ridges; Rivers; Safety factors; Safety, Risk, Reliability and Quality; Sciences de la terre & géographie physique; Seismic activity; Soil geomechanical properties
• ISSN: 2197-8670; 2197-8670
• DOI: 10.1186/s40677-024-00297-2

Background The landslide inventory of the western flank of Mount Oku, Cameroon, includes spreads or complex landslides, indicating sudden soil weakening, possibly due to seismic activity or heavy rainfall causing groundwater rise. These landslides were likely triggered between 2009 and 2018 based on the dates of the aerial imagery. Identifying triggers for past landslides remains a major unresolved issue in landslide science. However, understanding these triggers is crucial for accurately assessing future landslide hazards. Methodology In this paper, we investigate the possibility of earthquakes to precondition landslide development or reactivation during climatic events. By assuming a magnitude 5.2 earthquake, an epicenter of 10 km from this area, and different wetness conditions, the factor of safety (FS) and Newmark displacement (ND) models were calculated for shallow and deep-seated landslides with sliding depths of 3 and 7.5 m. Afterward, the relationship between FS, assumed ND, and observed landslides was analyzed in a cluster analysis, to derive patterns of climatically and seismically triggered landslides. Results The comparison of FS maps and FS values of the observed landslides revealed that especially for landslides at 7.5 m depth, most sites that are stable during dry conditions become instable under saturated conditions, indicating a climatic trigger. At 3 m depth, however, some landslide sites that are still marginally stable under saturated conditions, display relatively high ND values for the investigated hypothetical earthquake, indicating a possible seismic influence. In the cluster analysis, we clustered the observed landslides according to their distances to rivers and topographic ridges and obtained three clusters. Landslides from cluster 3 with 31% of the landslides display medium to high ND for the assumed earthquake, and were found near ridges and farther away from rivers, suggesting seismic triggering. Cluster 2, with 12% of landslides closer to rivers, suggested climatic origins. Thus, while climate is a critical landslide contributing factor, seismic events may also contribute, either by predisposing to landslides or by reactivating them alongside climatic factors. These results enable the establishment of more precise and effective landslide mitigating measures considering mostly rainfall but also earthquakes as possible triggers.