BABYLON (Illustrated). George Rawlinson

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СКАЧАТЬ number were salt, and of little value, except as furnishing the salt of commerce; but four—the Lake of Antioch, the Bahr-el-Kades, the Lake Merom, and the Sea of Galilee-were fresh-water basins lying upon the courses of streams which ran through them; and these not only diversified the scenery by their clear bright aspect, but were of considerable value to the inhabitants, as furnishing them with many excellent sorts of fish.

      Of the salt lakes the most eastern was the Sabakhah. This is a basin of long and narrow form, lying on and just below the 36th parallel. It is situated on the southern route from Balis to Aleppo, and is nearly equally distant between the two places. Its length is from twelve to thirteen miles; and its width, where it is broadest, is about five miles. It receives from the north the waters of the Nahr-el-Dhahab, or “Golden River” (which has by some been identified with the Daradax of Xenophon), and from the west two or three insignificant streams, which empty themselves into its western extremity. The lake produces a large quantity of salt, especially after wet seasons, which is collected and sold by the inhabitants of the surrounding country.

      The Bahr-el-Molak, the lake which absorbs the Koweik, or river of Aleppo, is less than twenty miles distant from Lake Sabakhah, which it very much resembles in its general character. Its ordinary length is about nine miles, and its width three or four; but in winter it is greatly swollen by the rains, and at that time it spreads out so widely that its circumference sometimes exceeds fifty miles. Much salt is drawn from its bed in the dry season, and a large part of Syria is hence supplied with the commodity. The lake is covered with small islands, and greatly frequented by aquatic birds-geese, ducks, flamingoes, and the like.

      The lakes in the neighborhood of Damascus are three in number, and are all of a very similar type. They are indeterminate in size and shape, changing with the wetness or dryness of the season; and it is possible that sometimes they may be all united in one. The most northern, which is called the Bahret-esh-Shurkiyeh, receives about half the surplus water of the Barada, together with some streamlets from the outlying ranges of Antilibanus towards the north. The central one, called the Bahret-el-Kibliyeh, receives the rest of the Barada water, which enters it by three or four branches on its northern and western sides. The most southern, known as Bahret-Hijaneh, is the receptacle for the stream of the Awaaj, and takes also the water from the northern parts of the Ledjah, or region of Argob. The three lakes are in the same line—a line which runs from N.N.E. to S.S.W. They are, or at least were recently, separated by tracts of dry land from two to four miles broad. Dense thickets of tall reeds surround them, and in summer almost cover their surface. Like the Bahr-el-Melak, they are a home for water-fowl, which flock to them in enormous numbers.

      By far the largest and most important of the salt lakes is the Great Lake of the South—the Bahr Lut (“Sea of Lot”), or Dead Sea. This sheet of water, which has always attracted the special notice and observation of travellers, has of late years been scientifically surveyed by officers of the American navy; and its shape, its size, and even its depth, are thus known with accuracy. The Dead Sea is of an oblong form, and would be of a very regular contour, were it not for a remarkable projection from its eastern shore near its southern extremity. In this place, a long and low peninsula, shaped like a human foot, projects into the lake, filling up two thirds of its width, and thus dividing the expanse of water into two portions, which are connected by a long and somewhat narrow passage. The entire length of the sea, from north to south, is 46 miles: its greatest width, between its eastern and its western shores, is 101 miles. The whole area is estimated at 250 geographical square miles. Of this space 174 square miles belong to the northern portion of the lake (the true “Sea”), 29 to the narrow channel, and 46 to the southern portion, which has been called “the back-water,” or “the lagoon.”

      The most remarkable difference between the two portions of the lake is the contrast they present as to depth. While the depth of the northern portion is from 600 feet, at a short distance from the mouth of the Jordan, to 800, 1000, 1200, and even 1300 feet, further down, the depth of the lagoon is nowhere more than 12 or 13 feet; and in places it is so shallow that it has been found possible, in some seasons, to ford the whole way across from one side to the other. The peculiarities of the Dead Sea, as compared with other lakes, are its depression below the sea-level, its buoyancy, and its extreme saltness. The degree of the depression is not yet certainly known; but there is reason to believe that it is at least as much at 1300 feet, whereas no other lake is known to be depressed more than 570 feet. The buoyancy and the saltness are not so wholly unparalleled. The waters of Lake Urumiyeh are probably as salt and as buoyant; those of Lake Elton in the steppe east of the Wolga, and of certain other Russian lakes, appear to be even salter. But with these few exceptions (if they are exceptions), the Dead Sea water must be pronounced to be the heaviest and saltest water known to us. More than one fourth of its weight is solid matter held in solution. Of this solid matter nearly one third is common salt, which is more than twice as much as is contained in the waters of the ocean.

      Of the fresh-water lakes the largest and most important is the Sea of Tiberias. This sheet of water is of an oval shape, with an axis, like that of the Dead Sea, very nearly due north and south. Its greatest length is about thirteen and its greatest width about six miles. Its extreme depth, so far as has been ascertained, is 27 fathoms, or 165 feet. The Jordan flows into its upper end turbid and muddy, and issues forth at its southern extremity clear and pellucid. It receives also the waters of a considerable number of small streams and springs, some of which are warm and brackish; yet its own water is always sweet, cool, and transparent, and, having everywhere a shelving pebbly beach, has a bright sparkling appearance. The banks are lofty, and in general destitute of verdure. What exactly is the amount of depression below the level of the Mediterranean remains still, to some extent, uncertain; but it is probably not much less than 700 feet. Now, as formerly, the lake produces an abundance of fish, which are pronounced, by those who have partaken of them, to be “delicious.”

      Nine miles above the Sea of Tiberias, on the course of the same stream, is the far smaller basin known now as the Bahr-el Huleh, and anciently (perhaps) as Merom. This is a mountain tarn, varying in size as the season is wet or dry, but never apparently more than about seven miles long, by five or six broad. It is situated at the lower extremity of the plain called Huleh, and is almost entirely surrounded by flat marshy ground, thickly set with reeds and canes, which make the lake itself almost unapproachable. The depth of the Huleh is not known. It is a favorite resort of aquatic birds, and is said to contain an abundant supply of fish.

      The Bahr-el-Kades, or Lake of Hems, lies on the course of the Orontes, about 139 miles N.N.E. of Merom, and nearly the same distance south of the Lake of Antioch. It is a small sheet of water, not more than six or eight miles long, and only two or three wide, running in the same direction with the course of the river, which here turns from north to north-east. According to Abulfeda and some other writers, it is mainly, if not wholly, artificial, owing its origin to a dam or embankment across the stream, which is from four to five hundred yards in length, and about twelve or fourteen feet high. In Abulfeda’s time the construction of the embankment was ascribed to Alexander the Great, and the lake consequently was not regarded as having had any existence in Babylonian times; but traditions of this kind are little to be trusted, and it is quite possible that the work above mentioned, constructed apparently with a view to irrigation, may really belong to a very much earlier age.

      Finally, in Northern Syria, 115 miles north of the Bahr-el-Kades, and about 60 miles N.W.W. of the Bahr-el-Melak, is the Bahr-el-Abyad (White Lake), or Sea of Antioch. This sheet of water is a parallelogram, the angles of which face the cardinal points: in its greater diameter it extends somewhat more than ten miles, while it is about seven miles across. Its depth on the western side, where it approaches the mountains, is six or eight feet; but elsewhere it is generally more shallow, not exceeding three or four feet. It lies in a marshy plain called El-Umk, and is thickly fringed with reeds round the whole of its circumference. From the silence of antiquity, some writers have imagined that it did not exist in ancient times; but the observations of scientific travellers are opposed to this theory. The lake abounds with fish of several kinds, and the fishery attracts and employs a considerable number of the natives who dwell near it.

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