A Brief History of Britain 1851-2010 - download pdf or read online

By Jeremy Black

ISBN-10: 1849018197

ISBN-13: 9781849018197

From the good Exhibition to the credits Crunch - the transformation of england from the world's maximum country to the current day

In 1851 Queen Victoria opened the nice Exhibition in Hyde Park, it used to be the excessive water mark of English success - the state on the vanguard of the economic Revolution, on the center of a burgeoning Empire, with a queen who could reign for one more 50 years. within the following a hundred and fifty years, the destiny of the kingdom has confronted turmoil and transformation. however it is simply too easy to speak of decline? Has nice Britain sacrificed its identification as a way to remain a part of the current global order.

Leading historian, Jeremy Black, completes the landmark 4 quantity short historical past of england sequence with a super, insightful exam of ways ultra-modern Britain used to be formed.

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Present high mountain ranges could therefore have formed at low elevations, even below sea level, and later have been bodily upheaved thousands of feet by the heating of mountain roots and down-slipped crustal blocks, the latter being an interesting forerunner of the idea of plate subduction. The work of Holmes and of Vening Meinesz will be discussed later in this chapter with respect to continental drift. Holmes (1928–9) employed a complex model of thermally produced convection currents in the substratum below the simatic layer which included convergence under continental margins; compression; the formation of geosynclines, borderlands and foredeeps; mountain building; and the formation of new minor substratum currents due to the development of the thickened mountain root leading to the thinning and destruction of the borderlands.

Du Toit reconstructed Gondwanaland in much greater and accurate detail than hitherto and altogether made a truly important contribution to the hypothesis of continental drift. We must be content with one non-controversial quote: An outstanding consequence of the Hypothesis is the orderly and interrelated nature of all associated phenomena…the critic may, and with justification, ask why the Hypothesis has apparently found so few whole-hearted supporters. The answer is, first, that it cuts at the basis of customary geological interpretations and is hence not particularly welcome, and, second, that no forces have so far been, nor according to its opponents can be, invoked competent to move the continents about as supposed.

11 (reprinted in (1925) Journal of the Washington Academy of Science vol. 15). Fisher, O. (1881) Physics of the Earth’s Crust, London: Macmillan. de (1892) ‘Quaternary changes of level in Scandinavia’, Bulletin of the Geological Society of America 3:65–8. K. (1890) ‘Lake Bonneville’, US Geological Survey Monograph 1. ——(1895) ‘A new light on isostasy’, Journal of Geology 3:331–4. Gilluly, J. (1949) ‘Distribution of mountain building in geologic time’, Bulletin of the Geological Society of America 60:561–90.

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A Brief History of Britain 1851-2010 by Jeremy Black


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