Why this matters
Stanbury Point is a headland composed primarily of Cretaceous Chalk, formed from the accumulation of marine microfossils over 66 to 145 million years ago. It is notable as a prominent coastal feature near Chichester, marking the western extent of the South Downs' chalk formation along the English Channel.
What is recorded here
Stanbury Point is shown as a headland on the public map of Chichester. The saved point is the map point or the centre of its mapped shape.
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