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Stevns Klint

Stevns Klint is a chalk cliff on eastern Zealand where a thin dark layer records the mass extinction at the end of the Cretaceous. The coast also holds a striking church and Cold War history.

Stevns Klint

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Why go

Few landscapes make deep time as visible as Stevns Klint's pale chalk and dark fish-clay boundary. Højerup Church stands close to the eroding edge, while the former Stevnsfortet fortress brings the story into the twentieth century. These layers make the cliff more than a viewpoint.

What to look for

  • A thin dark fish-clay layer marks the Cretaceous–Paleogene boundary.
  • Højerup Church stands by the eroding cliff edge.
  • Stevnsfortet's tunnels reveal a Cold War use for the chalk.

Useful to know

  • Stay on marked access around the eroding cliff and check conditions before descending toward the shore.
  • Treat the fortress as a separate visit if you want to explore its underground history.

Original World content and translations, shown as supplied. Practical information may need updating.

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