Geology of Kent into northern France. The fold arises from the continuing Alpine orogeny and results in the general northward dip of the rock strata in most of Kent. There are extensive spreads of coastal and estuarine alluvium on the Thames Estuary coast, in the low ground surrounding the Isle of Thanet and across Romney Marsh. Alluvium also floors the valleys of the River Medway and Stour. 'Clay-with-flints' is a commonly occurring deposit across the North Downs which is a product of periglacial conditions during the last ice age. Loessic deposists, of aeolian origin i.e. windblown, are common in east Kent, especially on
Languages of the United Kingdom included here. UK speakers, in the 2011 census, 59,824,194 (over the age of three) 98%. English is a West Germanic language brought around the fifth century CE to the east coast of what is now England by Germanic-speaking immigrants from around present-day northern Germany, who came to be known as the Anglo-Saxons. The fusion of these settlers' dialects became what is now termed Old English: the word "English" is derived from the name of the Angles. English soon displaced the previously predominant British Celtic and British Latin throughout most of England. It spread into what was to become south-east Scotland