Leicester in the Leicester area around AD 47, during their conquest of southern Britain. The Corieltauvian settlement lay near a bridge on the Fosse Way, a Roman road between the legionary camps at Isca (Exeter) and Lindum (Lincoln). It remains unclear whether the Romans fortified and garrisoned the location, but it slowly developed from around the year 50 onwards as the tribal capital of the Corieltauvians under the name Ratae Corieltauvorum. In the 2nd century, it received a forum and bathhouse. In 2013, the discovery of a Roman cemetery found just outside the old city walls and dating back to 300
Southern England Chalk Formation Southern England Chalk Formation The Chalk Formation of Southern England is a system of chalk downland in the south of England. The formation is perhaps best known for Salisbury Plain, the location of Stonehenge, the Isle of Wight, and the twin ridgeways of the North Downs and South Downs. The North Downs are confined chiefly to the counties of Kent and Surrey, and the South to Sussex. Each forms a well-defined long range springing from the chalk area of Dorset and Hampshire, to which, though broken up into a great number of short ranges and groups of hills, the general