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Other sedimentary layers have yielded chains of hills ranging from 965 feet (294 metres) in the North Downs to 1,083 feet (330 metres) in the Cotswolds.
The hills known as the Chilterns, the North York Moors, and the Yorkshire and Lincolnshire Wolds were rounded into characteristic plateaus with west-facing escarpments during three successive glacial periods of the Pleistocene Epoch (about 2,600,000 to 11,700 years ago).
England’s topography is low in elevation but, except in the east, rarely flat.
The country’s island location has been of critical importance to the development of the English character, which fosters the seemingly contradictory qualities of candour and reserve along with conformity and eccentricity and which values social harmony and, as is true of many island countries, the good manners that ensure orderly relations in a densely populated landscape.
Between these regions lie bands of sandstones and limestones of different geologic periods, many of them relicts of primeval times when large parts of central and southern England were submerged below warm seas.
Geologic forces lifted and folded some of these rocks to form the spine of northern England—the Pennines, which rise to 2,930 feet (893 metres) at Cross Fell.
The geologic complexity of England is strikingly illustrated in the cliff structure of its shoreline.
Along the southern coast from the ancient granite cliffs of Land’s End in the extreme southwest is a succession of sandstones of different colours and limestones of different ages, culminating in the white chalk from the Isle of Wight to Dover.
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No place in England is more than 75 miles (120 km) from the sea, and even the farthest points in the country are no more than a day’s journey by road or rail from London.