Holland-on-Sea Cliff terraces can be attributed to the Anglian glaciation, they provide a fixed point for correlation other Anglian sequences in southern Britain and on the Continent. The site is a short stretch of the slope between the Esplanade and the Promenade, opposite Haven Avenue. No geology is visible. Holland-on-Sea Cliff Holland-on-Sea Cliff is a 0.1 hectare geological Site of Special Scientific Interest in Holland-on-Sea, north-west of Clacton-on-Sea in Essex. It is a Geological Conservation Review site. This site is of great importance in understanding the evolution of the London Basin, and it is the type site for two different gravels. The
Clacton-on-Sea Originally built as a landing point for goods and passengers, as Clacton was becoming an increasingly popular destination for day trippers, in 1893 the pier was lengthened to , and entertainment facilities added. Bought by Ernest Kingsman in 1922, it remained in the ownership of the Kingsman family until 1971. In March 2009 the pier was purchased by the Clacton Pier Company, who installed a helter-skelter as a new focal point. A 48 turbine wind farm has been constructed about off the Clacton coast. Clacton has an oceanic climate (Köppen "Cfb") with fairly low precipitation. This makes for pleasantly warm