Stevns Klint

Map

Stevns Klint: A Geological Testimony to the Cretaceous-Paleogene Extinction Event

Stevns Klint, situated on the Danish island of Zealand, offers a unique glimpse into the Earth's history, making it a significant addition to the UNESCO World Heritage List in 2014. Known colloquially as the Cliffs of Stevns, this 17-kilometer-long white chalk cliff stands as a testament to the Cretaceous-Paleogene (K/P) extinction event, which occurred approximately 65 million years ago.

More to come…

UNESCO Description of the World Heritage Site

This geological site comprises a 15 km-long fossil-rich coastal cliff, offering exceptional evidence of the impact of the Chicxulub meteorite that crashed into the planet at the end of the Cretaceous, about 65 million years ago. Researchers think that this caused the most remarkable mass extinction ever, responsible for the disappearance of over 50 per cent of all life on Earth. The site harbours a record of the cloud of ash formed by the impact of the meteorite – the exact site being at the bottom of the ocean off the coast of Mexico’s Yucatán Peninsula. An exceptional fossil record is visible at the site, showing the complete succession of fauna and micro-fauna charting the recovery after the mass extinction.

Encyclopedia Record: Stevns Klint

Stevns Klint, known as the Cliffs of Stevns in English, is a white chalk cliff located some 6 km (3.7 mi) southeast of Store Heddinge on the Danish island of Zealand. Stretching 17 km (11 mi) along the coast, it is of geological importance as one of the best exposed Cretaceous-Tertiary (K/T) boundaries in the world. Subject to frequent erosion, the cliff rises to a height of up to 40 m (130 ft). Because of its exceptional fossil record, Stevns Klint was inscribed on the UNESCO World Heritage List in 2014.

Read more on Wikipedia