The national character area of the Humberhead Levels cover a large expanse of very flat, low-lying land towards the western end of the Humber estuary in northern England. The Levels occupies the area of the former Glacial Lake Humber. The area bounded to the east by the Yorkshire Wolds and the northern Lincolnshire Edge, a limestone escarpment, and to the west by the southern part of the Yorkshire magnesian limestone ridge. In the north the Levels merge with the slightly more undulating Vale of York close to the Escrick glacial moraine, and to the south merge into the Trent Vale. 
Glacial Lake Humber
During the last ice age, a glacier extended across this area almost to where Doncaster now is. The main glacial front was at Escrick where the Escrick moraine marks its furthest extension. This formed the northern limit of an extensive lake which was impounded by the blocking of the Humber gap by another ice front. The lake bottom was gradually filled with clay sediments, which are up to 20 metres thick in some places. These clay sediments are locally overlain by peat deposits forming raised mires. At the base of the peat layers can be found the remains of a buried forest.
The Humberhead levels have been settled for several thousand years. The drier northern area was settled before the Roman era. The lighter soils there were easier to drain with hand tools, and the area was extensively cleared for small-scale pastoral farming. The system of easily navigable rivers was used by invading late fifth- and sixth-century Angles and eighth- and ninth-century Vikings to penetrate deep into the countryside.