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Purfleet Chalk Pits SSSI
 
Purfleet Chalk Pits SSSI, Essex, is important for its sequence of Quaternary, or Ice Age, deposits which overlie the chalk bedrock. The Quaternary sands and gravels, which were laid down in an early course of the River Thames, are associated with both fossil remains and archaeological evidence in the form of worked materials. The Quaternary history of the River Thames is complex, but, on the basis of the fossil assemblage and the position of the deposits within the Thames terrace system, Purfleet has been correlated to Oxygen Isotope Stage 9 (around 300,000 yrs BP).
 
Purfleet Chalk Pits SSSI comprises a number of old quarries which are either disused or currently subject to redevelopment proposals. Development could potentially have had an adverse impact on certain areas of the site, particularly where sand and gravel deposits have been removed or obscured. However the opportunities for improved site management afforded by development of the area have allowed both an improvement in site condition and access. In addition geological and archaeological research of newly exposed sequences through the terrace deposits has improved our knowledge of the geological interest and its contribution to our understanding of the evolution of the River Thames.
 
Purfleet Chalk Pits SSSI, Essex - Photo : Chris Gleed-Owen, Natural England Raising land levels in the quarry will facilitate access to the brown Quaternary deposits at the top of the face, overlying the white Cretaceous chalk, which is not designated as part of the special interest of this site.  
Photo : Chris Gleed-Owen, Natural England
 
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