Holtug Chalk Quarry

Until 1972, limestone and chalk were quarried at Holtug Chalk Quarry, which is now a very special natural area, a Natura 2000 site, and an EU-protected area. You’ll experience wild nature as you walk from the top down into the quarry.

A very special place

The chalk quarry is home to many endangered and protected animal and plant species. Please therefore take particular care when visiting the site – stick to the paths and do not pick the plants. With a bit of luck, you may spot the great crested newt and the plant known as the broomrape, which are on the so-called Red List – a list of plant species at risk of extinction in Denmark unless we provide them with special protection. The broomrape is unique because its leaves do not contain chlorophyll, and so the plant cannot use sunlight for photosynthesis. Instead, it parasitises the roots of plants such as the thistle-like greater knapweed, and has earned its name because it literally starves its host plant.

In the soft, white chalk of the quarry, you may be lucky enough to find fossils of sea urchins, squid and sharks. If you’re going fossil hunting, bear in mind the three simple rules mentioned further down the page.

A Natura 2000 site that you should take particular care to protect

Chalk was quarried at Holtug for over 100 years, but the quarry has remained largely untouched since 1972. Today, you can take a walk down through the quarry and out to the water – the paths can be slippery, so we recommend you wear suitable footwear.

There are fossils dating back millions of years at Stevns Klint – in fact, the cliff itself consists of fossils: skeletons and tiny shell fragments from algae and bryozoans that died and ended up at the bottom of the Chalk Sea.

  • Fossils

    Fossils are the remains of animals and plants. Some of them become petrified, but not all, and certainly not at Stevns Klint, where they are often made of chalk or limestone. A petrified remains is therefore a fossil, whilst a fossil does not necessarily have to be a petrified remains.

    Some truly unique fossils have been found at Stevns Klint. Several of them have been designated as ‘Danekræ’. The typical fossils found here include barnacles, various sea urchins and corals – but you can also find shark teeth, as well as teeth or parts of a mosasaur.

  • The layers in the cliff

    The lower part of Stevns Klint consists of chalk from the end of the Cretaceous period.

    Above the chalk lies a thin layer of Fiskeler, which marks the K/T boundary – that is, the transition between the Cretaceous and Tertiary periods. This layer contains evidence of the mass extinction that took place 66 million years ago.

    The upper part of the cliff consists of hard limestone, in many places containing curved flint bands.

  • Three simple rules

    Stevns Klint is a truly unique place on Earth. That is why collecting fossils is only possible if we all work together to look after this World Heritage Site. Here are three simple rules to follow when collecting fossils at Stevns Klint:

    • Never chip away at the cliff face; only collect from fallen boulders. The same applies in the quarries, where you must not chip away at the ground either.
    • Do not dig in Fiskeleret – nothing may be collected there either. At Højerup, you must not use any tools, but may only collect what you find lying loose on the beach.
    • If you find fallen blocks or lumps of chalk and limestone, you are welcome to take them home and examine them.

     

Practical information

  • Find your way

    There are very limited parking facilities at Holtug Chalk Quarry, so we recommend parking at Mandehoved and walking to Holtug Chalk Quarry along the Trampestien path.

  • Parking

    There are very limited parking facilities at Holtug Chalk Quarry, so we recommend parking at Mandehoved and walking to Holtug Chalk Quarry along the Trampestien path.

  • Accommodation

    You can go camping and stay overnight in shelters at Mandehoved and in hotels in Rødvig.

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