Chapter 2 the Historical Background
CHAPTER 2 THE HISTORICAL BACKGROUND 1 5 I GEOGRAPHICAL AND CLIMATIC FOUNDATIONS As an area of historical study the Greater milder climate, by comparison both with the Manchester County has the disadvantage of being moors and with other westerly facing parts of without an history of its own. Created by Act Britain. Opening as they do on to what is, of Parliament a little over ten years ago, it climatically speaking, an inland sea, they joins together many areas with distinct avoid much of the torrential downpours brought histories arising from the underlying by Atlantic winds to the South West of England. geographical variations within its boundaries. At the same time the hills give protection from the snow bearing easterlies. The lowland areas The Greater Manchester County is the are fertile, and consist largely of glacial administrative counterpart of 20th century deposits. urban development which has masked the diversity of old pre-industrial southeast In the northwest of the Greater Manchester Lancashire and northeast Cheshire. County the plain rises around Wigan and Standish. For centuries the broad terraced The area has three dominant geographic valley of the Rivers Mersey and Irwell, which characteristics: the moorlands; the plains; and drains the plain, has been an important barrier the rivers, most notably the Mersey/Irwell to travel because of its mosses. Now the system. region's richest farmland, these areas of moss were largely waste until the early 19th century, when they were drained and reclaimed. The central area of Greater Manchester County, which includes the major part of the The barrier of the Mersey meant that for conurbation, is an eastward extension of the centuries northeast Cheshire developed .quite Lancashire Plain, known as the 'Manchester separately from southeast Lancashire, and it Embayment1 because it lies, like a bay, between was not until the twenties and thirties that high land to the north and east.
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