Stevns Klint, located on the Danish island of Zealand, is renowned for its striking white chalk cliffs and rich geological history marking the Cretaceous-Paleogene boundary.
Stevns Klint is an impressive and scientifically significant coastal cliff in Denmark, stretching approximately 15 kilometers along the eastern coast of Zealand. The site showcases 65 million years of Earth's history, with visible layers of chalk from the Cretaceous period and a thin layer of fish clay marking the boundary of the mass extinction event that wiped out the dinosaurs. This geological feature has become a crucial site for studying the causes and effects of the event. Visitors to Stevns Klint can explore the area's scenic beauty through well-marked paths, enjoy stunning views of the Baltic Sea, and visit the Stevns Museum, which offers insights into its geological and historical significance. Several old churches and quaint villages nearby offer a glimpse into the local culture and history, providing a well-rounded experience for history and geology enthusiasts alike.
Højerup Old Church perched on the cliff edge
The visible Cretaceous-Paleogene boundary
Spectacular views over the Baltic Sea
Cold War-era Stevnsfortet Cold War Museum
A historic church with part of its former nave actually fallen into the sea due to erosion.
A distinct geological layer that marks a major extinction event.
A Cold War-era fortress offering underground and above-ground tours.