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Erosion by rain, river, and tides and subsidence in parts of eastern England subsequently shaped the hills and the coastline.Plateaus of limestone, gritstone, and carboniferous strata are associated with major coalfields, some existing as outcrops on the surface.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.In the early 19th century, England became the epicentre of a worldwide Industrial Revolution and soon the world’s most industrialized country.Drawing resources from every settled continent, cities such as Manchester, Birmingham, and Liverpool converted raw materials into manufactured goods for a global market, while London, the country’s capital, emerged as one of the world’s preeminent cities and the hub of a political, economic, and cultural network that extended far beyond England’s shores.It is rare for institutions to operate for England alone.

In England the development of a “national” education took a completely different course.

When the last ice sheet melted, the sea level rose, submerging the land bridge that had connected Great Britain with the European mainland.

Deep deposits of sand, gravel, and glacial mud left by the retreating glaciers further altered the 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.

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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.