MEDIA (Illustrated). George Rawlinson

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СКАЧАТЬ same longitude. Towards the south there was no marked line or natural boundary; and it is difficult to say with any exactness how much of the great plateau belonged to Media and how much to Persia. Having regard, however, to the situation of Hamadan, which, as the capital, should have been tolerably central, and to the general account which historians and geographers give of the size of Media, we may place the southern limit with much probability about the line of the thirty-second parallel, which is nearly the present boundary between Irak and Fars.

      The shape of Media has been called a square; but it is rather a long parallelogram, whose two principal sides face respectively the north-east and the south-west, while the ends or shorter sides front to the south-east and to the northwest. Its length in its greater direction is about 600 miles, and its width about 250 miles. It must thus contain nearly 150,000 square miles, an area considerably larger than that of Assyria and Chaldaea put together, and quite sufficient to constitute a state of the first class, even according to the ideas of modern Europe. It is nearly one-fifth more than the area of the British Islands, and half as much again as that of Prussia, or of peninsular Italy. It equals three fourths of France, or three fifths of Germany. It has, moreover, the great advantage of compactness, forming a single solid mass, with no straggling or outlying portions; and it is strongly defended on almost every side by natural barriers offering great difficulties to an invader.

      In comparison with the countries which formed the seats of the two monarchies already described, the general character of the Median territory is undoubtedly one of sterility. The high table-land is everywhere intersected by rocky ranges, spurs from Zagros, which have a general direction from west to east, and separate the country into a number of parallel broad valleys, or long plains, opening out into the desert. The appearance of these ranges is almost everywhere bare, arid, and forbidding. Above, they present to the eye huge masses of gray rock piled one upon another; below, a slope of detritus, destitute of trees or shrubs, and only occasionally nourishing a dry and scanty herbage. The appearance of the plains is little superior; they are flat and without undulations, composed in general of gravel or hard clay, and rarely enlivened by any show of water; except for two months in the spring, they exhibit to the eye a uniform brown expanse, almost treeless, which impresses the traveller with a feeling of sadness and weariness. Even in Azerbijan, which is one of the least arid portions of the territory, vast tracks consist of open undulating downs, desolate and sterile, bearing only a coarse withered grass and a few stunted bushes.

      Still there are considerable exceptions to this general aspect of desolation. In the worst parts of the region there is a time after the spring rains when nature puts on a holiday dress, and the country becomes gay and cheerful. The slopes at the base of the rocky ranges are tinged with an emerald green: a richer vegetation springs up over the plains, which are covered with a fine herbage or with a variety of crops; the fruit trees which surround the villages burst out into the most luxuriant blossom; the roses come into bloom, and their perfume everywhere fills the air. For the two months of April and May the whole face of the country is changed, and a lovely verdure replaces the ordinary dull sterility.

      In a certain number of more favored spots beauty and fertility are found during nearly the whole of the year. All round the shores of Lake Urumiyeh, more especially in the rich plain of Miyandab at its southern extremity, along the valleys of the Aras, the Kizil-uzen, and the Jaghetu, in the great valley of Linjan, fertilized by irrigation from the Zenderud, in the Zagros valleys, and in various other places, there is an excellent soil which produces abundantly with very slight cultivation.

      The general sterility of Media arises from the scantiness of the water supply. It has but few rivers, and the streams that it possesses run for the most part in deep and narrow valleys sunk below the general level of the country, so that they cannot be applied at all widely to purposes of irrigation. Moreover, some of them are, unfortunately, impregnated with salt to such an extent that they are altogether useless for this purpose; and indeed, instead of fertilizing, spread around them desolation and barrenness. The only Median streams which are of sufficient importance to require description are the Aras, the Kizil-Uzen, the Jaghetu, the Aji-Su and the Zenderud, or river of Isfahan.

      The Aras is only very partially a Median stream. It rises from several sources in the mountain tract between Kars and Erzeroum, and runs with a generally eastern direction through Armenia to the longitude of Mount Ararat, where it crosses the fortieth parallel and begins to trend southward, flowing along the eastern side of Ararat in a south-easterly direction, nearly to the Julfa ferry on the high road from Erivan to Tabriz. From this point it runs only a little south of east to long. 46° 30’ E. from Greenwich, when it makes almost a right angle and runs directly north-east to its junction with the Kur at Djavat. Soon after this it curves to the south, and enters the Caspian by several mouths in lat. 39° 10’ nearly. The Aras is a considerable stream almost from its source. At Hassan-Kaleh, less than twenty miles from Erzeroum, where the river is forded in several branches, the water reaches to the saddle-girths. At Keupri-Kieui, not much lower, the stream is crossed by a bridge of seven arches. At the Julfa ferry it is fifty yards wide, and runs with a strong current. At Megree, thirty miles further down, its width is eighty yards. In spring and early summer the stream receives enormous accessions from the spring rains and the melting of the snows, which produce floods that often cause great damage to the lands and villages along the valley. Hence the difficulty of maintaining bridges over the Aras, which was noted as early as the time of Augustus, and is attested by the ruins of many such structures remaining along its course. Still, there are at the present day at least three bridges over the stream—one, which has been already mentioned, at Keupri-Kieui, another a little above Nakshivan, and the third at Khudoperinski, a little below Megree. The length of the Aras, including only main windings, is 500 miles.

      The Kizil-Uzen, or (as it is called in the lower part of its course) the Sefid-Rud, is a stream of less size than the Aras, but more important to Media, within which lies almost the whole of its basin. It drains a tract of 180 miles long by 150 broad before bursting through the Elburz mountain chain, and descending upon the low country which skirts the Caspian. Rising in Persian Kurdistan almost from the foot of Zagros, it runs in a meandering course with a general direction of north-east through that province into the district of Khamseh, where it suddenly sweeps round and flows in a bold curve at the foot of lofty and precipitous rocks, first northwest and then north, nearly to Miana, when it doubles back upon itself, and turning the flank of the Zenjan range runs with a course nearly south-east to Menjil, after which it resumes its original direction of north-east, and, rushing down the pass of Budbar, crosses Ghilan to the Caspian. Though its source is in direct distance no more than 320 miles from its mouth, its entire length, owing to its numerous curves and meanders, is estimated at 490 miles. It is a considerable stream, forded with difficulty, even in the dry season, as high up as Karagul, and crossed by a bridge of three wide arches before its junction with the Garongu river near Miana. In spring and early summer it is an impetuous torrent, and can only be forded within a short distance of its source.

      The Jaghetu and the Aji-Su are the two chief rivers of the Urumiyeh basin. The Jaghetu rises from the foot of the Zagros chain, at a very little distance from the source of the Kizil-Uzen. It collects the streams from the range of hills which divides the Kizil-Uzen basin from that of Lake Urumiyeh, and flows in a tolerably straight course first north and then north-west to the south-eastern shore of the lake. Side by side with it for some distance flows the smaller stream of the Tatau, formed by torrents from Zagros; and between them, towards their mouths, is the rich plain of Miyandab, easily irrigated from the two streams, the level of whose beds is above that of the plain, and abundantly productive even under the present system of cultivation. The Aji-Su reaches the lake from the north-east. It rises from Mount Sevilan, within sixty miles of the Caspian, and flows with a course which is at first nearly due south, then north-west, and finally south-west, past the city of Tabriz, to the eastern shore of the lake, which it enters in lat. 37° 50’. The waters of the Aji-Su are, unfortunately, salt, and it is therefore valueless for purposes of irrigation.

      The Zenderud or river of Isfahan rises from the eastern flank of the Kuh-i-Zerd (Yellow Mountain), a portion of the Bakhti-yari chain, and, receiving a number of tributaries from СКАЧАТЬ