Geology of Kent into northern France. The fold arises from the continuing Alpine orogeny and results in the general northward dip of the rock strata in most of Kent. There are extensive spreads of coastal and estuarine alluvium on the Thames Estuary coast, in the low ground surrounding the Isle of Thanet and across Romney Marsh. Alluvium also floors the valleys of the River Medway and Stour. 'Clay-with-flints' is a commonly occurring deposit across the North Downs which is a product of periglacial conditions during the last ice age. Loessic deposists, of aeolian origin i.e. windblown, are common in east Kent, especially on
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