A view of the spectacular cliffs in Hunstanton, North Norfolk. This area is on the east coast but gets great sunsets as it faces back west. The cliffs are a popular geological feature with white chalk from the Upper Cretaceous
era, a layer of limestone known as red chalk from the lower cretaceous period formed over a period of 15 million years and finally beneath that is grey/green carstone.
era, a layer of limestone known as red chalk from the lower cretaceous period formed over a period of 15 million years and finally beneath that is grey/green carstone.
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A view of the spectacular cliffs in Hunstanton, North Norfolk. This area is on the east coast but gets great sunsets as it faces back west. The cliffs are a popular geological feature with white chalk from the Upper Cretaceous
era, a layer of limestone known as red chalk from the lower cretaceous period formed over a period of 15 million years and finally beneath that is grey/green carstone.
era, a layer of limestone known as red chalk from the lower cretaceous period formed over a period of 15 million years and finally beneath that is grey/green carstone.
Ref:
Date:
Location:
Photographer:
British landscapes
A view of the spectacular cliffs in Hunstanton, North Norfolk. This area is on the east coast but gets great sunsets as it faces back west. The cliffs are a popular geological feature with white chalk from the Upper Cretaceous
era, a layer of limestone known as red chalk from the lower cretaceous period formed over a period of 15 million years and finally beneath that is grey/green carstone.
era, a layer of limestone known as red chalk from the lower cretaceous period formed over a period of 15 million years and finally beneath that is grey/green carstone.
Ref:
Date:
Location:
Photographer: