Why this matters
Chilling Cliff is a sea cliff composed primarily of Cretaceous-age Chalk, formed through the accumulation of marine microfossils over 66 to 145 million years ago. It is notable for its exposure of the South Downs geological formation and its susceptibility to erosion by coastal processes.
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Chilling Cliff is shown as a cliff on the public map of Fareham. The saved point is the map point or the centre of its mapped shape.
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