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,
Geography of Scotland in the Middle Ages been in the regions of the western mainland of Scotland between Cowal and Ardnamurchan, and the adjacent islands, later extending up the West coast in the eighth century. There is place name and archaeological evidence of Anglian settlement in south-east Scotland reaching into West Lothian, and to a lesser extent into south-western Scotland. Later Norse settlement was probably most extensive in Orkney and Shetland, with lighter settlement in the Western Islands, particularly the Hebrides and on the mainland in Caithness, stretching along fertile river valleys through Sutherland and into Ross. There was also extensive settlement in Bernicia stretching into the