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Formed of the union of small 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., , the West Country, the Midlands—and retain strong ties to those regions even if they live elsewhere.
The and acid heath, and from clay to sand—each type of soil bearing its own class of vegetation.As in other temperate maritime zones, the averages are moderate, ranging in the Thames river valley from about 35 °F (2 °C) in January to 72 °F (22 °C) in July; but the extremes in England range from below 0 °F (−18 °C) to above 90 °F (32 °C).The Roman historian recorded that the climate was “objectionable, with frequent rains and mists, but no extreme cold.” Yet snow covers the higher elevations of England about 50 days per year. Despite the political, economic, and cultural legacy that has secured the perpetuation of its name, England no longer officially exists as a governmental or political unit—unlike Scotland, Wales, and 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.In the early 19th century, England became the epicentre of a worldwide , 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.Slate covers most of the northern portion of the mountains, and thick beds of lava are found in the southern part.
Other sedimentary layers have yielded chains of hills ranging from 965 feet (294 metres) in the North 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).
Leached brown soils predominate in much of southern England. Fine-grained deposits of alluvium occur in the floodplains, and fine marine silt occurs around the Wash estuary.
Weather in England is as variable as the topography.
Not for nothing has the bumbershoot been the stereotypical walking stick of the English gentleman.
England shares with the rest of Britain a diminished spectrum of vegetation and living creatures, partly because the island was separated from the mainland of Europe soon after much of it had been swept bare by the last glacial period and partly because the land has been so industriously worked by humans.
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.