To save content items to your account,
please confirm that you agree to abide by our usage policies.
If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account.
Find out more about saving content to .
To save content items to your Kindle, first ensure no-reply@cambridge.org
is added to your Approved Personal Document E-mail List under your Personal Document Settings
on the Manage Your Content and Devices page of your Amazon account. Then enter the ‘name’ part
of your Kindle email address below.
Find out more about saving to your Kindle.
Note you can select to save to either the @free.kindle.com or @kindle.com variations.
‘@free.kindle.com’ emails are free but can only be saved to your device when it is connected to wi-fi.
‘@kindle.com’ emails can be delivered even when you are not connected to wi-fi, but note that service fees apply.
In Germany towards the end of 1929 employment melted away so rapidly that the prosperous period seemed to have been a mere illusion. In Austria the prosperity had been less convincing in any case, and soon the streets of Vienna seemed crowded with beggars. The Socialist Chancellor of Germany, Hermann Müller, resigned, and Hindenburg called upon the leader of the Centre party, Heinrich Brüning, to succeed him in the spring of 1930. Behind Brüning, and far more than he ever realised, intrigues were concentrating upon plans to make Hindenburg more of a pre-1914 emperor, and to reduce the powers of the Reichstag accordingly: these intrigues emanated from a ‘political general’ called Kurt von Schleicher, a friend of the President's son Oscar. When in July 1930 Brüning failed to get the agreement of the Reichstag to some deflationary measures of his, Hindenburg, encouraged by Schleicher, enforced them by emergency decree. Brüning thought it correct to dissolve the Reichstag, which had been elected in May 1928 in the prosperous period.
Elections were held on 14 September 1930: the results were like a bombshell for Germany and for Europe. The number of Communist deputies increased from 54 to 77 and the National Socialist Party (Nazis) shot up from 12 in the last Reichstag to 107: they were now the largest party after the Social Democrats. These Nazis were the followers of the Austrian agitator, Adolf Hitler, who had ignominiously failed to seize power in Munich in November 1923.
At eleven o'clock on the morning of 11 November 1918 the cease-fire sounded along the western front. It was the end of the first world war, which had killed not less than 10 million persons, had brought down four great empires and had impoverished the continent of Europe. The defeat of Germany, so long invincible to more than half the world, had been registered at dawn that day in the Armistice of Compiègne. Its heavy terms were in the main those proposed by Marshal Foch, the Allied generalissimo, and lay between the views of the British Field-Marshal Haig, who overestimated the German capacity for continued resistance and advocated more lenient conditions, and those of the American General Pershing, who had argued in favour of refusing an armistice and maintaining the Allied advance. This matched the attitude of the former president Theodore Roosevelt and a popular American demand for unconditional surrender. As it was, one month after the armistice, Ebert, head of the first government of the new German republic, greeted returning German formations at the Brandenburger Tor with the words: ‘No foe has overcome you … You have protected the homeland from enemy invasion.’
No less important in the long run than the terms of the armistice were the preconditions governing its signature. When the German government had applied to President Wilson on 4 October 1918 for an armistice it had adroitly proposed that peace negotiations, and not only those for an armistice, should be based upon the ‘fourteen points’ of his address of 8 January 1918, as amplified in his subsequent pronouncements.
A comparison between the countries round the Baltic and those round the Mediterranean in the middle of the sixteenth century sheds light L on conditions in the north at a time when the political situation was vastly different from the present one. Though in varying degrees, the European countries on the Mediterranean all had an ancient cultural heritage, and during the last few centuries they had evolved a new culture—the Renaissance—in conscious relation to classical antiquity. The former political disunity was partly overcome in France, was on the way to being overcome in the Iberian peninsula, but was still acute in Italy. At the eastern end of the Mediterranean, on the other side of an ‘iron curtain’, lay the cultural world of the Orient. For centuries it had given many impulses to southern Europe. Now the links were broken, and most of Europe's trade with the Far East followed new routes.
Similarly, in the middle of the sixteenth century the eastern and western sides of the Baltic belonged to different cultural spheres in religion, education, language and custom; the main line of demarcation was between Russia on the one side, and her neighbours Sweden-Finland and Poland on the other. But the dissimilarities to southern Europe were enormous. The northern countries were economically and culturally primitive compared with those in the south. The refinement of the Renaissance had as yet left only small traces in northern Europe, primarily in art. The Reformation's programme, however, had quickly and effectively reached northern Germany, Poland and Scandinavia, spreading not so much among the masses as in certain social groups—particularly the middle-class townspeople—and within government circles.
The Peace of Cateau-Cambrésis ended a war that had become, if indeed it had not started as, ‘a race between spent horses’. It was a peace of exhaustion and it endured because for many years to come none of the states of western Europe felt strong enough to risk another general conflict. Yet although all were afraid to strike, some were still willing to wound. And the internal instability that afflicted all of them, bred of exhaustion and fevered by a crisis of conscience in religion, gave to any dissatisfied power repeated hopes of undermining the foundations upon which the 1559 settlement rested.
In that settlement the British Isles occupied a crucial position. For the treaties left one of the two outstandingly great powers of western Europe, France, hemmed in and all but encircled by the territories of the other, Spain. The dominions of Philip II of Spain ran almost all around France—from Spain itself through the Balearic islands, Sardinia, and Sicily to Naples, the Tuscan ports, Parma, and Milan, with dependent Corsica, Genoa, and Savoy-Piedmont linking on to Franche-Comté and the Netherlands. If the British Isles or at least England could be added to these, as during Mary Tudor's marriage to Philip II (1554–8), then the ring would be complete and virtually unbreakable. If, on the other hand, the French could control England as well as Scotland, then the sea route through the Channel and the Straits of Dover could be closed to the Spaniards.
According to the census taken in 1956, the total population of Iran was 18,944,821; it has increased since then at the rate of 2.4 to 2.5 per cent a year. The centre of the country is largely empty and life has been driven either towards the exterior or towards the interior of the mountains, to the points where there is an adequate water-supply. There are extraordinary variations in density: in the neighbourhood of Tehran, 44 inhabitants per sq km; on the shores of the Caspian, from 20 to 30. According to the 1956 census, the urban population constitutes 30.1 per cent of the total population, and the rural population (including seminomads) 69.9 per cent. In Iran, the marriage rate is generally higher among women than among men. Consanguinity in marriage is on the decline, as demonstrated in part by the growing number of marriages between Iranians and foreigners.
Iran is unfortunate in having recorded no long-term climatic observations. Hence, a great deal of attention was focused on Iran's agricultural potentialities, the assessment of which required adequate knowledge of climatic conditions. The climate of Iran is influenced by many centres of high pressure as well as a number of low pressure centres. In a country like Iran having extensive flat deserts, highly complex mountain systems, topography is a major modifying factor and surface winds are greatly influenced by local topographical features. The country has five temperature zones, namely, the Caspian zone, Persian Gulf zone, Zagros zone, Alburz zone, and the interior zone. Over Iran, it can be said that precipitation decreases from north to south and from west to east, except where relief of the land upsets the regularity in this arrangement. The mean annual precipitation for the entire country is 400 mm.
Vegetal conditions in Iran were at their optimum during the third and second millennia BC. The regional changes in distribution and character of the country's natural vegetation cover stem from four factors: climatic situation; hytogeographical region; pronounced and varied topography of the plateau; and impact of human activity upon the vegetation. Many modes of interference have given rise to many forms of semi-natural vegetation, which may represent stages either in a process of destruction or of regeneration. All the relevant types of vegetation can be arranged according to their dependence: first, on atmospheric humidity (precipitation) or ground moisture; and second, on temperature as expressed in elevation or exposure. In the western part of the Iranian plateau there is only one area of a truly humid forest. The chapter also presents a discussion of the azonal vegetation types.
This chapter deals with the geology of Iran, the information of which is somewhat uneven. The stratigraphical column in Iran contains samples of all the systems, from Pre-Cambrian to Quaternary; and from the beginning of the Palaeozoic onwards, diagnostic fossils are sometimes abundant. An introduction to the geomorphology of the country can be made by journeying across it from south-west to north-east. Starting then from the Shaṭṭ al-ʿArab near Ābādān and crossing an occasionally flooded alluvial plain for seventy miles, never far from the meanders of the Karun river, one comes to a series of low isolated ridges of brown sandstone, the Ahvāz hills. The Zagros range skirts its south-western side for 800 miles and beyond the Zagros are the plains of Iraq or Mesopotamia, the growing delta of the Euphrates and Tigris, and the Persian Gulf. These elements forming the west of the region have features of structural history in common.
The zoogeography of any region can be viewed from three perspectives, all of which are closely interrelated: descriptive, ecological, and historical. This chapter is based upon a comprehensive study of the systematics of the lizards of Iran. Southwest Asia has two major distributional components in its lizard fauna, one of which is the Iranian Plateau. The chapter first focuses on the distribution of species within the various physiographic regions of Iran including the Central Plateau, Sistan basin, Türkmen steppe, Zagors mountains. So little is known about the Iranian lizards in nature, and information about the physical environment so lacking in detail, that the chapter presents only general remarks can be made relative to the immediate factors determining present distributions. The significance of endemic species (or subspecies) from the standpoint of historical zoogeography is threefold, one of which is a narrowly restricted form may be relictual, occupying the remaining habitable area of a once much broader distribution.
Old mine-workings have long been known in many provinces of Iran. Traces of gold in alluvium or quartz veins have been recorded, and minerals yielding silver, lead, zinc, and copper are widely but sparingly distributed. This chapter presents a description of several minerals and metals along with their mine-locations in Iran such as coal, iron, copper, lead-zinc, chromite, bauxite, molybdenum, arsenic, antimony, fluorspar. Coal is an obvious alternative to charcoal, and for a considerable time coal has been dug in the mountains north of Tehrān. Iron ore deposits have been observed in many parts of the country, most of them between the southern slopes of the Alburz system and the Volcanic belt, especially somewhat north-east of the limits of the Volcanic belt. References to fluorspar are made in the record of some of the lead-zinc workings, such as the one at Mīkhās near Qazvin where quartz, calcite and fluor are vein minerals.
While the westward-flowing streams of the Zagros mountains provide some of the world's most impressive canyon scenery, they also present an extremely perplexing problem of drainage genesis. Seldom are drainage anomalies as pronounced as they are among the great petrified waves of the Zagros. The disharmony between the drainage and the deformational pattern in the Zagros is manifested in the profound gorges, or tangs, which breach range after range in the youngest portion of the mountain system. The vast majority of the drainage anomalies and the most spectacular tangs in the Zagros are found in the zone of powerful but simple folding along the south-western (outer) margin of the highland. The drainage anomaly in the central Zagros may be resolved into two distinct problems: the courses of the trunk streams, and the behaviour of their tributaries, large and small. Each of these appears to be an independent development.
There is no fossil evidence from the Middle East as a whole, let alone Iran, for anything but the most limited traces of very early human occupations. Even this limited evidence is sufficient to prove that Palaeolithic man lived in many parts of Iran, ranging from Lake Rezāʾiyeh (Urumiyeh) in the north-west to Shiraz in the south-west, to the south-eastern littoral of the Caspian and eastward into southern Khurāsān. The cave of Bīsitūn, located some thirty miles east of Kirmānshāh, has provided evidence of one ulna fragment and one human incisor tooth, in association with a highly developed Mousterian industry. The skull discovered in a cave in Teshik Tash distinctly resembles that of a western Neanderthaler, though it is morphologically more modern than those of most, if not all, the western Neanderthalers, particularly because it has a higher cranial vault.
In spite of being the sixth largest petroleum producer in the world Iran still derives between 23 and 30 per cent of her gross national income from agricultural farming. However, the resources used and usable for agriculture are severely limited. The areal extent of land available for agricultural production cannot be increased by any significant amount although the regional balance may well be altered. Indeed the present cultivated area is largely the product of an extensive approach to land use. Rice, grown on some 330,000 hectares, is the only staple food product of which there is an exportable surplus. Added to paucity of land resources and rural poverty there is also ignorance; some 85 per cent of the total population is illiterate. Climatic, ecological and hydrological conditions in the regions of seasonal water surplus impose stringent controls on the use of such water in the deficit zones.