History of Phoenicia. George Rawlinson
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and rather bare plain, well watered, and with soft turf in many parts, which gently slopes to the foot of the main ascent, a wall of rock generally half covered with snow, up which winds the rough track whereby travellers reach the summit. Rills of water are not wanting; flowers bloom to the very edge of the snow, and the walnut-tree flourishes in sheltered places to within two or three thousand feet of the summit; but the general character of the tract is bare and bleak; the villages are few; and the terraced cultivation, which adds so much to the beauty of the western side, is wanting. In the southern half of the range the descent is abrupt from the crest of the mountain into the Buka’a, or valley of the Litany, and the aspect of the mountain-side is one of “unrelieved bareness."141
There is, however, one beauty at one point on this side of the Lebanon range which is absent from the more favoured western region. On the ascent from Baalbek to the Cedars the traveller comes upon Lake Lemone, a beautiful mountain tarn, without any apparent exit, the only sheet of water in the Lebanon. Lake Lemone is of a long oval shape, about two miles from one end to the other, and is fed by a stream entering at either extremity, that from the north, which comes down from the village of Ainât, being the more important. As the water which comes into the lake cannot be discharged by evaporation, we must suppose some underground outlet,142 by which it is conveyed, through the limestone, into the Litany.
The eastern side of Lebanon drains entirely into this river, which is the only stream whereto it gives birth. The Litany is the principal of all the Phoenician rivers, for the Orontes must be counted not to Phoenicia but to Syria. It rises from a small pool or lake near Tel Hushben,143 about six miles to the south-west of the Baalbek ruins. Springing from this source, which belongs to Antilibanus rather than to Lebanon, the Litany shortly receives a large accession to its waters from the opposite side of the valley, and thus augmented flows along the lower Buka’a in a direction which is generally a little west of south, receiving on either side a number of streams and rills from both mountains, and giving out in its turn numerous canals for irrigation. As the river 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 of a most extraordinary character. Nothing in the conformation of the strata, or in the lie of ground, indicates the coming marvel144—the roots of Lebanon and Hermon appear to intermix—and the further progress of the river seems to be barred by a rocky ridge stretching across the valley from east to west, when lo! suddenly, the ridge is cut, as if by a knife, and a deep and narrow chasm opens in it, down which the stream plunges in a cleft 200 feet deep, and so narrow that in one place it is actually bridged over by masses of rock which have fallen from the cliffs above.145 In the gully below fig-trees and planes, besides many shrubs, find a footing, and the moist walls of rock on either side are hung with ferns of various kinds, among which is conspicuous the delicate and graceful maidenhair. Further down the chasm deepens, first to 1,000 and then to 1,500 feet, “the torrent roars in the gorge, milk-white and swollen often with the melting snow, overhung with semi-tropical oleanders, fig-trees, and oriental planes, while the upper cliffs are clad with northern vegetation, two zones of climate thus being visible at once."146 Where the gorge is the deepest, opposite the Castle of Belfort (the modern Kulat-esh-Shukif), the river suddenly makes a turn at right angles, altering its course from nearly due south to nearly due west, and cuts through the remaining roots of Lebanon, still at the bottom of a tremendous fissure, and still raging and chafing for a distance of fifteen miles, until at length it debouches on the coast plain, and meanders slowly through meadows to the sea,147 which it enters about five miles to the north of Tyre. The course of the Litany may be roughly estimated at from seventy to seventy-five miles.
The other streams to which Lebanon gives birth flow either from its northern or its western flank. From the northern flank flows one stream only, the Nahr-el-Kebir or Eleutherus. The course of this stream is short, not much exceeding thirty miles. It rises from several sources at the edge of the Coelesyrian valley, and, receiving affluents from either side, flows westward between Bargylus and Lebanon to the Mediterranean, which it enters between Orthosia (Artousi) and Marathus (Amrith) with a stream, the volume of which is even in the summer-time considerable. In the rainy season it constitutes an important impediment to intercourse, since it frequently sweeps away any bridge which may be thrown across it, and is itself unfordable. Caravans sometimes remain encamped upon its banks for weeks, waiting until the swell has subsided and crossing is no longer dangerous.148
From the western flank of Lebanon flow above a hundred streams of various dimensions, whereof the most important are the Nahr-el-Berid or river of Orthosia, the Kadisha or river of Tripolis, the Ibrahim or Adonis, the Nahr-el-Kelb or Lycus, the Damour or Tamyras, the Auly (Aouleh) or Bostrenus, and the Zaherany, of which the ancient name is unknown to us. The Nahr-el-Berid drains the north-western angle of the mountain chain, and is formed of two main branches, one coming down from the higher portion of the range, about Lat. 34º 20´, and flowing to the north-west, while the other descends from a region of much less elevation, about Lat. 34º 30´, and runs a little south of west to the point of junction. The united stream then forces its way down a gorge in a north-west direction, and enters the sea at Artousi, probably the ancient Orthosia.149 The length of the river from its remotest fountain to its mouth is about twenty miles.
The Kadisha or “Holy River” has its source in the deep basin already described, round which rise in a semicircle the loftiest peaks of the range, and on the edge of which stand “the Cedars.” Fed by the perpetual snows, it shortly becomes a considerable stream, and flows nearly due west down a beautiful valley, where the terraced slopes are covered with vineyards and mulberry groves, and every little dell, every nook and corner among the jagged rocks, every ledge and cranny on precipice-side, which the foot of man can reach, or on which a basket of earth can be deposited, is occupied with patch of corn or fruit-tree.150 Lower down near Canobin the valley contracts into a sublime chasm, its rocky walls rising perpendicularly a thousand feet on either side, and in places not leaving room for even a footpath beside the stream that flows along the bottom.151 The water of the Kadisha is “pure, fresh, cool, and limpid,"152 and makes a paradise along its entire course. Below Canobin the stream sweeps round in a semicircle towards the north, and still running in a picturesque glen, draws near to Tripolis, where it bends towards the north-west, and enters the sea after passing through the town. Its course, including main windings, measures about twenty-five miles.
The Ibrahim, or Adonis, has its source near Afka (Apheca) in Lat. 34º 4´ nearly. It bursts from a cave at the foot of a tremendous cliff, and its foaming waters rush down into a wild chasm.153 Its flow is at first towards the north-west, but after receiving a small tributary from the north-east, it shapes its course nearly westward, and pursues this direction, with only slight bends to the north and south, for the distance of about fifteen miles to the sea. After heavy rain in Lebanon, its waters, which are generally clear and limpid, become tinged with the earth which the swollen torrent detaches from the mountain-side,154 and Adonis thus “runs purple to the sea”—not however once a year only, but many times. It enters the Mediterranean about four miles south of Byblus (Jebeil) and six north of Djouni.
The Lycus or Nahr-el-Kelb (“Dog River”) flows from the northern and western flanks of Jebel Sunnin. It is formed by the confluence of three main streams. One of these rises near Afka, and runs to the south of west, past the castle and temples of Fakra, to its junction with the second stream, which is formed of several rivulets flowing from the northern flank of Sunnin. Near Bufkeiya the river constituted by the union of these two branches is joined by a third stream flowing from the western flank of Sunnin with a westerly course, and from this point the Lycus pursues its way in the same general direction down a magnificent gorge to the Mediterranean. Both banks are lofty, but especially that to the south, where one of Lebanon’s great roots strikes out far, and dips, a rocky precipice, into the bosom of the deep.155 Low in the depths of the gorge the mad torrent dashes over its rocky bed in sheets of foam, its banks fringed with oleander, which it bathes with its spray. Above rise jagged precipices of white limestone, crowned far overhead by many a convent and village.156 The course of the Nahr-el-Kelbis about equal to that of the Adonis.
The Damour or Tamyras drains the western flank of Lebanon to the south of Jebel Sunnin (about Lat. 33º 45´), the districts known as Menassif and Jourd Arkoub, about Barouk and Deir-el-Kamar. It collects the waters from an area of about 110 square miles,