Cliff collapse at Stevns Klint, south-east Denmark

Stevns Klint, a UNESCO World Heritage Site and renowned geological formation, experiences frequent cliff collapses due to the contrast between soft Cretaceous chalk and harder Tertiary bryozoan limestone. This study highlights how the erosion-resistant bryozoan limestone forms overhanging projections, leading to recurrent collapses, while the underlying chalk is eroded by storm waves and debris shedding. The research provides insights into the dynamic processes shaping this iconic coastal cliff, offering a deeper understanding of its geological evolution.

Schack Pedersen, S. A., & Damholt, T. (2012). Cliff collapse at Stevns Klint, south-east Denmark. Geological Survey of Denmark and Greenland Bulletin, 26, 33–36. https://doi.org/10.34194/geusb.v26.4745