The pit shows a sequence of PleistoceneAnglian and pre-Anglian deposits. It displays an early blocking of the pre-Anglian Thames Valley, at a time when the River Thames followed a more northerly course, resulting in the formation of a lake. This was overrun by a second advance of ice during the Anglian glaciation around 450,000 years ago, which diverted the Thames to its present course and initiated Colne drainage in the area. The site is regarded by Natural England as of fundamental importance as the only one which demonstrates the diversion of the Thames from its pre-Anglian course.[1]
There is no access to the deep quarry, which is partly filled with water, but it can be viewed by crossing the railway line at How Wood station and turning south to follow the east side of the Abbey Line.