description Stevns Klint Overview
Stevns Klint is a fossil-rich chalk coastal cliff in southeastern Denmark and a UNESCO World Heritage site. The approximately 15-kilometer cliff exposes a clear geological record of the Cretaceous-Paleogene boundary, including material associated with the Chicxulub impact and the mass extinction at the end of the Cretaceous period. Its rocks and fossils are studied for evidence of extinction, environmental change, and biological recovery, making the site relevant to geology and paleontology.
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Where is Stevns Klint?
Stevns Klint is a fossil-rich chalk cliff on the southeastern coast of Denmark. The cliff stretches for approximately 15 kilometers and is recognized as a UNESCO World Heritage site.
Why is Stevns Klint important to geology?
It exposes a clear record of the Cretaceous-Paleogene boundary. The rock sequence includes material associated with the Chicxulub impact that occurred around the time the non-avian dinosaurs disappeared.
What is Stevns Klint made of?
The coastal cliff is made primarily of chalk with fossil-rich layers. Its exposed strata allow visitors and researchers to examine the boundary between the Cretaceous and Paleogene periods.
What can visitors see at Stevns Klint?
Visitors can see long chalk cliffs and exposed fossil-bearing geological layers along the Danish coast. The site is especially notable for the visible Cretaceous-Paleogene boundary and its UNESCO status.
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