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|description={{en|1=High Rocks, Tunbridge Wells. These joints or vertical fissures were originally caused by the sandstone shrinking on drying, and afterwards made larger by the effects of the weather. Excursion to Tunbridge Wells, May 13th 1916. From: T W Reader geological photographs 1914, 1916. Geologists' Association Carreck Archive. BGS image P804790.}}<br />
|date=2020-10-13<br />
|source=British Geological Survey<br />
|author=British Geological Survey<br />
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