Europe: A History Read Free Page A

school, was not above a touch of Gallic chauvinizing. The geography of France, he stressed, was marked by the keynote of variety. ‘Against the diversities which assail her’, he wrote, ‘France sets her force d’assimilation , her power of assimilation. She transforms everything that she receives.’ On Britain, in contrast, he quotes the doggerel lines about ‘this paltry little isle, I with acres few and weather vile’. One hundred years later one finds Fernand Braudel doing similar things. 2 Variety is indeed a characteristic of France’s superb make-up. But it is not a French monopoly, it is a hallmark of Europe as a whole.
    In fact, the Peninsula of Europe is not really a ‘continent’ at all: it is not a self-contained land mass. At c.10 million km 2 (3.6 million square miles), it is less than one-quarter the size of Asia, one-third of Africa, one-half of each of the Americas. Modern geographers classify it, like India, as a subcontinent of Eurasia: ‘a cape of the old continent, a western appendix of Asia’. Even so, it is impossible to deny that Europe has been endowed with a formidable repertoire of physical features. Europe’s landforms, climate, geology, and fauna have combined to produce a benign environment that is essential to an understanding of its development.

    Map 4. Europe: Physical Regions
    Europe’s landforms do not resemble those of any other continent or subcontinent. The depressions to north and south have been flooded by the ocean to form two parallel sea-chains which penetrate deep into the interior. In the north, the North Sea-Baltic sea lane stretches 1,500 miles (2,500 km) from the Atlantic to Russia. In the south, the Mediterranean-Black Sea system stretches over 2,400 miles (4,000 km) from Gibraltar to the Caucasus. Within these protected seas liea vast complex of lesser gulfs and a huge spangle of islands. As a result, the ratio of shoreline to landmass is exceptionally high: at c .37,000 km, or more than 23,000 miles, the European shoreline is almost exactly the length of the Equator. For early Man, this was perhaps the most important measure of accessibility.
    What is more, since the shores of the Peninsula lie in the temperate latitudes of Eurasia’s western extremity, they are served by a user-friendly climate. Prevailing ocean winds blow westerly; and it is the western coasts of the great continents that stand to benefit most from the moderating influx of sea air. Yet few other west-facing continental coasts can actually enjoy the advantage. Elsewhere, if the western shore is not blocked by towering peaks or icy currents, it is lined by deserts such as the Sahara, the Kalahari, or the Atacama.
    The climate of Europe, therefore, is unusually temperate for its latitude. Generally speaking, under the influence of the Gulf Stream, northern Europe is mild and moist; southern Europe is relatively warm, dry, and sunny. Central and eastern Europe enjoy elements of a true continental climate, with clear, cold winters and baking hot summers. But everywhere the weather is changeable. Extremes are usually avoided. Even in European Russia, where the difference between the mean temperatures of January and July can approach 45 °C, the range is only half what it is in Siberia. The wettest district in Europe is in western Norway, with an average annual precipitation of 3,500 mm (138 inches). The dryest district surrounds the Caspian Sea, with less than 250 mm (9 inches) per annum. The coldest spot is Vorkuta, with a mean January chill of −20°C; the hottest is disputed between Seville and Astrakhan, both with mean July roasts of +29°C. These extremes do not compare with their counterparts in Asia, Africa, or the Americas.
    Europe’s temperate climate favoured the requirements of primitive agriculture. Most of the Peninsula lies within the natural zone of cultivable grasses. There were abundant woodlands to provide fuel and shelter. Upland pasture often occurs in close proximity to