Bottom sediments (formation), regionally
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The data set shows bottom sediments in the top 1-2 m of the seabed, classified by soil type. Soil as a property describes the method of formation of the loose mass. The data covers parts of the Norwegian continental shelf in the Barents Sea, the Norwegian Sea, the North Sea and Skagerrak, and has been digitised with a scale of 1:100 000-1 250,000 (regional mapping).



