Dinosaur footprint found in armourstone at Reculver. Believed that the stone is of French origin as was shipped in to protect towers from costal erosion.
Photographer: Geoff Downer
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Grid Reference: TQ688534
The Wateringbury SSSI contains a tufa deposit important for Quaternary studies. Tufa is a soft calcium carbonate commonly precipitated by springs which have flowed through chalk or limestone. Tufa is geologically important as it often provides a detailed and complete stratigraphy, preserving a rich and diverse fauna commonly in situ and therefore reflecting local and regional environmental changes.
The Wateringbury tufa contains a detailed record of early Flandrian (10,000 to 7,500 years ago) mollusc biostratigraphy (mollusc assemblage zones a to d). It is particularly valuable in demonstrating the order of species recolonisation after the late Devensian cold stage, and for the length and completeness of the record. It is also notable for the small area of deposition which allowed large numbers of terrestrial snails to be incorporated in the tufa. These are of greater value for interpreting regional faunal changes than are autochthonous (in situ) freshwater and swamp species. Related pollen, ostracod and vertebrate records are also available from the site making this a key locality for understanding the changing environments of the early Flandrian across southern England.
For more detailed information on this remarkable SSSI site visit the English Nature website.
(Regionally Important Geological Sites)
RIGS are geological sites that are important for historical, scientific research or educational reasons.
(Sites of Special Scientific Interest)
SSSIs give legal protection to the best sites for wildlife and geology in England.