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In the early 19th century, England became the epicentre of a worldwide Industrial Revolution and soon the world’s most industrialized country.

While English culture draws on the cultures of the world, it is quite unlike any other, if difficult to identify and define.The oldest sedimentary rocks and some igneous rocks (in isolated hills of granite) are in Cornwall and Devon on the southwestern peninsula, ancient volcanic rocks underlie parts of the Cumbrian Mountains, and the most recent alluvial soils cover the Fens of Cambridgeshire, Lincolnshire, and Norfolk.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.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.A varied panorama of cliffs, bays, and river estuaries distinguishes the English coastline, which, with its many indentations, is some 2,000 miles (3,200 km) long.

The Welland river valley forms part of the rich agricultural land of Lincolnshire.

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