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,
Vale of Kent landscape of "Low Weald", of which the Vale of Kent is a part. The Weald-Artois Anticline continues some further south-eastwards under the Straits of Dover, and includes the Boulonnais of France. Vale of Kent The Vale of Kent, located in Kent, England, is the name given to the broad clay vale between the Greensand Ridge and the High Weald. The area is drained by a number of rivers, including the Beult, Eden Medway, Stour and River Teise. Principal settlements in the Vale include Ashford and Tonbridge. The Weald is the eroded remains of a geological structure, an anticline, a dome