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,
Site of the Claudian invasion of Britain in Kent. Dio describes how the troops saw a shooting star whilst at sea and were cheered by this omen. He adds that it travelled from east to west and that this was the direction the Romans were sailing in. However, a voyage from Boulogne to Kent sails from south to north. Taking Boulogne as the point of departure, historians such as John Morris and J. G. F. Hind have used Dio's account to suggest a landing point much further west along the south coast of Britain, around the Solent or Southampton Water. This is supported by Dio's stated reason