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,
East Coast of the United States 1677) and Florida (part of New Spain until 1821, though held by the British for 20 years after the French and Indian War). The Middle Colonies (New Jersey, Pennsylvania, New York, and Delaware) had been owned by the Dutch as New Netherland, until they were captured by the English in the mid-to-late 17th century. There are three basic climate regions on the East Coast according to the Köppen climate classification from north to south based on the monthly mean temperature of the coldest month (January): The region from northern Maine south to northern Rhode Island and Connecticut has a continental