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,
Kingdom of Kent to East Anglia and others went back to northern France as the forebears of the Normans who conquered England in 1066. Kingdom of Kent The Kingdom of the Kentish (; ), today referred to as the Kingdom of Kent, was an early medieval kingdom in what is now South East England. It existed from either the fifth or the sixth century CE until it was fully absorbed into the Kingdom of England in the tenth century. Under the preceding Romano-British administration the area of Kent faced repeated attacks from seafaring raiders during the fourth century CE. It is likely that