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Summary
DescriptionLayers of glacial sediments resting on chalk base - geograph.org.uk - 613947.jpg
English: Layers of glacial sediments resting on chalk base. The pebble beach at Weybourne marks the start of the cliff section of the Norfolk coast that extends in easterly direction. This change in the character of the coastline is due to the properties of the chalk, which is harder to the east. The cliffs resting on this chalk base are composed of layers of glacial sediments of flints and fossils. For a more distant view of these cliffs see > 613925
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== {{int:filedesc}} == {{Information |description={{en|1=Layers of glacial sediments resting on chalk base The pebble beach at Weybourne marks the start of the cliff section of the Norfolk coast that extends in easterly direction. This change in the char