Hunstanton, on the North Norfolk Coast is noted for the Cretaceous
chalk cliffs.  A brittle white chalk at the top overlies a narrow bed of red
chalk below which is an iron sandstone called the Carrstone.  The white
and red chalks are fossiliferous, containing shell fragments, burrow trace
fossils, and bivalves.

The cliffs at Hunstanton should not be hammered directly since
this is unneccessary and extremely dangerous.  There will be plenty
of fossil-bearing loose fallen blocks on the beach.  Do not work at
the base of the cliffs or below overhangs.

Weathering patterns in the Carrstone.

The different layers show up well in this photograph.

The cliffs are unstable.  Frequent falls occur, particularly during
winter storms.  The green above the cliffs has become noticably
narrower in the last 15 years.

Above 3 photographs: remains of a wave cut platform.

Sunset over the Wash

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