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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.
Cotswolds, and the moors and chalk downs of southern England serve as watersheds for most of England’s rivers.
It was influenced not by a political but by an industrial revolution.
It is true that theorists such as Adam Smith, Thomas Paine, and Thomas Robert Malthus proposed state organization of…
It is rare for institutions to operate for England alone.
Notable exceptions are the Church of England (Wales, Scotland, and Ireland, including Northern Ireland, have separate branches of the Anglican Communion) and sports associations for cricket, rugby, and football (soccer).
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.
Formed of the union of small Celtic and Anglo-Saxon kingdoms during the early medieval period, England has long comprised several distinct regions, each different in dialect, economy, religion, and disposition; indeed, even today many English people identify themselves by the regions or shires from which they come—e.g., Yorkshire, the West Country, the Midlands—and retain strong ties to those regions even if they live elsewhere.
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.In many ways England has seemingly been absorbed within the larger mass of Great Britain since the Act of Union of 1707.Laced by great rivers and small streams, England is a fertile land, and the generosity of its soil has supported a thriving agricultural economy for millennia.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).