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Layers of lime have been formed by billions of microscopic lime-rich shells from organisms called coccoliths. Coccoliths lived in the ocean millions of years ago and when they died the fell to the ocean floor where they decomposed and left nothing but their outer shell. Layer upon layer of these organisms compiled to form great deposits of lime.

Later sea floor deposits and the mighty movements of the ice age glaciers has compressed the lime layers and pushed it to the surface in dense belts.

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Dankalk K/S
Aggersundvej 50,
9670 Løgstør DK

(+45) 33 68 74 00
dankalk@dankalk.dk

Åbningstider:
Alle hverdage: 07.15–15.15
Lørdag og Søndag: Lukket

Products agriculture
Feed components
Industry – betocarb and lime filler
Flue gas cleaning with hydrated lime

(+45) 33 68 74 00 Aggersundvej 50, 9670 Løgstør DK dankalk@dankalk.dk

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