Geology of Kent the northern slopes of the Downs where they are known as brickearths. Landslips are known along the north coast of the Isle of Sheppey, the coast near Reculver and either side of Folkestone and indeed the former coastline west of Folkestone overlooking Romney Marsh. Geology of Kent The geology of Kent in southeast England largely consists of a succession of northward dipping late Mesozoic and Cenozoic sedimentary rocks overlain by a suite of unconsolidated deposits of more recent origin. Kent is the south-easternmost county in England. It is bounded on the north by the River Thames and the North Sea,
Town of South Coast the entire Southport Division became the Shire of Southport on 31 March 1903. On 12 April 1918, the Shire of Southport became the Town of Southport. On 9 December 1948, as part of a major reorganisation of local government in South East Queensland, an Order in Council replacing ten former local government areas between the City of Brisbane and the New South Wales border with only four. The former ten were: The four resulting local government areas were: The Order came into effect on 10 June 1949, when the first elections were held. The proposed name "South Coast" was not