BABYLON (Illustrated). George Rawlinson

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СКАЧАТЬ the Kara Su, or “Black River,” which reaches it from the Aga Denghis, or Bahr-el-Abiyad, about five miles below Jisr Hadid and four or five above Antioch. This stream brings into the Orontes the greater part of the water that is drained from the southern side of Amanus. It is formed by a union of two rivers, the upper Kara Su and the Afrin, which flow into the Aga Denghis (White Sea), or Lake of Antioch, from the north-west, the one entering it at its northern, the other at its eastern extremity. Both are considerable streams; and the Kara Su on issuing from the lake carries a greater body of water than the Orontes itself, and thus adds largely to the volume of that stream in its lower course from the point of junction to the Mediterranean.

      The Litany, or river of Tyre, rises from a source at no great distance from the head springs of the Orontes. The almost imperceptible watershed of the Buka’a runs between Yunin and Baalbek, a few miles north of the latter; and when it is once passed, the drainage of the water is southwards. The highest permanent fountain of the southern stream seems to be a small lake near Tel Hushben, which lies about six miles to the south-west of the Baalbek ruins. Springing from this source the Litany flows along the lower Buka’a in a direction which is generally a little west of south, receiving on either side a number of streamlets and rills from Libanus and Anti-libanus, and giving out in its turn numerous canals for irrigation, which fertilize the thirsty soil. As the stream descends with numerous windings, but still with the same general course, the valley of the Buka’a contracts more and more, till finally it terminates in a gorge, down which thunders the Litany—a gorge a thousand feet or more in depth, and so narrow that in one place it is actually bridged over by masses of rock which have fallen from the jagged sides. Narrower and deeper grows the gorge, and the river chafes and foams through it, gradually working itself round to the west, and so clearing a way through the very roots of Lebanon to the low coast tract, across which it meanders slowly, as if wearied with its long struggle, before finally emptying itself into the sea. The course of the Litany may be roughly estimated at from 70 to 75 miles.

      The Barada, or river of Damascus, rises in the plain of Zebdany—the very centre of the Antilibanus. It has its real permanent source in a small nameless lake in the lower part of the plain, about lat. 33° 41’; but in winter it is fed by streams flowing from the valley above, especially by one which rises in lat. 33° 46’, near the small hamlet of Ain Hawar. The course of the Barada from the small lake is at first towards the east; but it soon sweeps round and flows-southward for about four miles to the lower end of the plain, after which it again turns to the east and enters a romantic glen, running between high cliffs, and cutting through the main ridge of the Antilibanus between the Zebdany plain and Suk, the Abila of the ancients. From Suk the river flows through a narrow but lovely valley, in a course which has a general direction of south-east, past Ain Fijoh (where its waters are greatly increased), through a series of gorges and glens, to the point where the roots of the Antilibanus sink down upon the plain, when it bursts forth from the mountains and scatters. Channels are drawn from it on either side, and its waters are spread far and wide over the Merj, which it covers with fine trees and splendid herbage.

      One branch passes right through the city, cutting it in half. Others irrigate the gardens and orchards both to the north and to the south. Beyond the town the tendency to division still continues. The river, weakened greatly through the irrigation, separates into three main channels, which flow with divergent courses towards the east, and terminate in two large swamps or lakes, the Bahret-esh-Shurkiyeh and the Bahret-el-Kibli-yeh, at a distance of sixteen or seventeen miles from the city. The Barada is a short stream, its entire course from the plain of Zebdany not much exceeding forty miles.

      The Jordan is commonly regarded as flowing from two sources in the Huleh or plain immediately above Lake Merom, one at Banias (the ancient Paneas), the other at Tel-el-Kady, which marks the site of Laish or Dan. But the true highest present source of the river is the spring near Hasbeiya, called Nebaes-Hasbany, or Eas-en-Neba. This spring rises in the torrent-course known as the Wady-el-Teim, which descends from the north-western flank of Hermon, and runs nearly parallel with the great gorge of the Litany, having a direction from north-east to south-west. The water wells forth in abundance from the foot of a volcanic bluff, called Eas-el-Anjah, lying directly north of Hasbeiya, and is immediately used to turn a mill. The course of the streamlet is very slightly west of south down the Wady to the Huleh plain, where it is joined, and multiplied sevenfold, by the streams from Banais and Tel-el-Kady, becoming at once worthy of the name of river. Hence it runs almost due south to the Merom lake, which it enters in lat. 33° 7’, through a reedy and marshy tract which it is difficult to penetrate. Issuing from Merom in lat. 33° 3’, the Jordan flows at first sluggishly southward to “Jacob’s Bridge,” passing which, it proceeds in the same direction, with a much swifter current down the depressed and narrow cleft between Merom and Tiberias, descending at the rate of fifty feet in a mile, and becoming (as has been said) a sort of “continuous waterfall.” Before reaching Tiberias its course bends slightly to the west of south for about two miles, and it pours itself into that “sea” in about lat. 32° 53’. Quitting the sea in lat. 32° 42’, it finally enters the track called the Ghor, the still lower chasm or cleft which intervenes between Tiberias and the upper end of the Dead Sea. Here the descent of the stream becomes comparatively gentle, not much exceeding three feet per mile; for though the direct distance between the two lakes is less than seventy miles, and the entire fall above 600 feet, which would seem to give a descent of nine or ten feet a mile, yet, as the course of the river throughout this part of its career is tortuous in the extreme, the fall is really not greater than above indicated. Still it is sufficient to produce as many as twenty-seven rapids, or at the rate of one to every seven miles. In this part of its course the Jordan receives two important tributaries, each of which seems to deserve a few words.

      The Jarmuk, or Sheriat-el-Mandhur, anciently the Hiero-max, drains the water, not only from Gaulonitis or Jaulan, the country immediately east and south-east of the sea of Tiberias, but also from almost the whole of the Hauran. At its mouth it is 130 feet wide, and in the winter it brings down a great body of water into the Jordan. In summer, however, it shrinks up into an inconsiderable brook, having no more remote sources than the perennial springs at Mazarib, Dilly, and one or two other places on the plateau of Jaulan. It runs through a fertile country, and has generally a deep course far below the surface of the plain; ere falling into the Jordan it makes its way through a wild ravine, between rugged cliffs of basalt, which are in places upwards of a hundred feet in height.

      The Zurka, or Jabbok, is a stream of the same character with the Hieromax, but of inferior dimensions and importance. It drains a considerable portion of the land of Gilead, but has no very remote sources, and in summer only carries water through a few miles of its lower course. In winter, on the contrary, it is a roaring stream with a strong current, and sometimes cannot be forded. The ravine through which it flows is narrow, deep, and in some places wild. Throughout nearly its whole course it is fringed by thickets of cane and oleander, while above, its banks are clothed with forests of oak.

      The Jordan receives the Hieromax about four or five miles below the point where it issues from the Sea of Tiberias, and the Jabbok about half-way between that lake and the Dead Sea. Augmented by these streams, and others of less importance from the mountains on either side, it becomes a river of considerable size, being opposite Beth-shan (Beisan) 140 feet wide, and three feet deep, and averaging, in its lower course, a width of ninety with a depth of eight or nine feet. Its entire course, from the fountain near Hasbeiya to the Dead Sea, including the passage of the two lakes through which it flows, is, if we exclude meanders, about 130, if we include them, 360 miles. It is calculated to pour into the Dead Sea 6,090,000 tons of water daily.

      Besides these rivers the Babylonian territory comprised a number of important lakes. Of these some of the more eastern have been described in a former volume: as the Bahr-i-Nedjif in Lower Chaldsea, and the Lake of Khatouniyeh in the tract between the Sinjar and the Khabour. It was chiefly, however, towards the west that sheets of water abounded: the principal of these were the Sabakhah, the Bahr-el-Melak, and the Lake of Antioch in Upper Syria; the Bahr-el-Kades, or Lake of Hems, in the central region; and the Damascus lakes, the Lake of Merom, the Sea of Galilee or Tiberias, and the Dead Sea, in the regions lying furthest to СКАЧАТЬ