Cotswold Line the station is Bledington. The Oxfordshire Way which has been close to the railway since Akeman Street now turns west to Bourton-on-the-Water but it is replaced by another long distance footpath, the Diamond Way. At Moreton-in-Marsh the line crosses the course of another major Roman road, the Fosse Way which linked "Isca Dumnoniorum" (Exeter) and "Lindum Colonia" (Lincoln). Moreton-in-Marsh was the headquarters of the railway spot-hire company Cotswold Rail until the company moved to Gloucester. About after Oxford is Moreton-in-Marsh. This was once the southern end of the Stratford and Moreton Tramway. The line then passes the corner of the
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