History of Phoenicia. George Rawlinson

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СКАЧАТЬ Casius is, strictly speaking, the termination of a spur from Bargylus; but it has so marked and peculiar a character that it seems entitled to separate description. Rising up abruptly from the Mediterranean to the height of 5,318 feet, it dominates the entire region in its vicinity, and from the sea forms a landmark that is extraordinarily conspicuous. Forests of fine trees clothe its flanks, but the lofty summit towers high above them, a bare mass of rock, known at the present day as Jebel-el-Akra, or “the Bald Mountain.” It is formed mainly of the same cretaceous limestone as the other mountains of these parts, and like them has a rounded summit; but rocks of igneous origin enter into its geological structure; and in its vegetation it more resembles the mountain ranges of Taurus and Amanus than those of southern Syria and Palestine. On its north-eastern prolongation, which is washed by the Orontes, lay the enchanting pleasure-ground of Daphné, bubbling with fountains, and bright with flowering shrubs, where from a remote antiquity the Syrians held frequent festival to their favourite deity—the “Dea Syra”—the great nature goddess.

      The elevated tract known to the ancients as Bargylus, and to modern geographers as the Ansayrieh or Nasariyeh mountain-region, runs at right angles to the spur terminating in the Mount Casius, and extends from the Orontes near Antioch to the valley of the Eleutherus. This is a distance of not less than a hundred miles. The range forms the western boundary of the lower Coelesyrian valley, which abuts upon it towards the east, while westward it looks down upon the region, partly hill, partly lowland, which may be regarded as constituting “Northern Phoenicia.” The axis of the range is almost due north and south, but with a slight deflection towards the south-east. Bargylus is not a chain comparable to Lebanon, but still it is a romantic and picturesque region. The lower spurs towards the west are clothed with olive grounds and vineyards, or covered with myrtles and rhododendrons; between them are broad open valleys, productive of tobacco and corn. Higher up “the scenery becomes wild and bold; hill rises to mountain; soft springing green corn gives place to sterner crag, smooth plain to precipitous heights;"130 and if in the more elevated region the majesty of the cedar is wanting, yet forests of fir and pine abound, and creep up the mountain-side, in places almost to the summit, while here and there bare masses of rock protrude themselves, and crag and cliff rise into the clouds that hang about the highest summits. Water abounds throughout the region, which is the parent of numerous streams, as the northern Nahr-el-Kebir, which flows into the sea by Latakia, the Nahr-el-Melk, the Nahr Amrith, the Nahr Kublé, the Nahr-el-Abrath, and many others. From the conformation of the land they have of necessity short courses; but each and all of them spread along their banks a rich verdure and an uncommon fertility.

      But the great range of Phoenicia, its glory and its boast is Lebanon. Lebanon, the “White Mountain"131—“the Mont Blanc of Palestine"132—now known as “the Old White-headed Man” (Jebel-esh-Sheikh), or “the Mountain of Ice” (Jebel-el-Tilj), was to Phoenicia at once its protection, the source of its greatness, and its crowning beauty. Extended in a continuous line for a distance of above a hundred miles, with an average elevation of from 6,000 to 8,000 feet, and steepest on its eastern side, it formed a wall against which the waves of eastern invasion naturally broke—a bulwark which seemed to say to them, “Thus far shall ye go, and no further.” The flood of conquest swept along its eastern flank, down the broad vale of the Buka’a, and then over the hills of Galilee; but its frowning precipices and its lofty crest deterred or baffled the invader, and the smiling region between its summit and the Mediterranean was, in the early times at any rate, but rarely traversed by a hostile army. This western region it was which held those inexhaustible stores of forest trees that supplied Phoenicia with her war ships and her immense commercial navy; here were the most productive valleys, the vineyards, and the olive grounds, and here too were the streams and rills, the dashing cascades, the lovely dells, and the deep gorges which gave her the palm over all the surrounding countries for variety of picturesque scenery.

      The geology of the Lebanon is exceedingly complicated. “While the bulk of the mountain, and all the higher ranges, are without exception limestone of the early cretaceous period, the valleys and gorges are filled with formations of every possible variety, sedimentary, metamorphic, and igneous. Down many of them run long streams of trap or basalt; occasionally there are dykes of porphyry and greenstone, and then patches of sandstone, before the limestone and flint recur."133 Some slopes are composed entirely of soft sandstone; many patches are of a hard metallic-sounding trap or porphyry; but the predominant formation is a greasy or powdery limestone, bare often, but sometimes clothed with a soft herbage, or with a thick tangle of shrubs, or with lofty forest trees. The ridge of the mountain is everywhere naked limestone rock, except in the comparatively few places which attain the highest elevation, where it is coated or streaked with snow. Two summits are especially remarkable, that of Jebel Sunnin towards the south, which is a conspicuous object from Beyrout,134 and is estimated to exceed the height of 9,000 feet,135 and that of Jebel Mukhmel towards the north, which has been carefully measured and found to fall a very little short of 10,200 feet.136 The latter, which forms a sort of amphitheatre, circles round and impends over a deep hollow or basin, opening out towards the west, in which rise the chief sources that go to form the romantic stream of the Kadisha. The sides of the basin are bare and rocky, fringed here and there with the rough knolls which mark the deposits of ancient glaciers, the “moraines” of the Lebanon. In this basin stand “the Cedars.” It is not indeed true, as was for a long time supposed, that the cedar grove of Jebel Mukhmel is the sole remnant of that primeval cedar-forest which was anciently the glory of the mountain. Cedars exist on Lebanon in six other places at least, if not in more. Near Tannurin, on one of the feeders of the Duweir, a wild gorge is clothed from top to bottom with a forest of trees, untouched by the axe, the haunt of the panther and the bear, which on examination have been found to be all cedars, some of a large size, from fifteen to eighteen feet in girth. They grow in clusters, or scattered singly, in every variety of situation, some clinging to the steep slopes, or gnarled and twisted on the bare hilltops, others sheltered in the recesses of the dell. There are also cedar-groves at B’sherrah; at El Hadith; near Dûma, five hours south-west of El Hadith; in one of the glens north of Deir-el-Kamar, at Etnub, and probably in other places.137 But still “the Cedars” of Jebel Mukhmel are entitled to pre-eminence over all the rest, both as out-numbering any other cluster, and still more as exceeding all the rest in size and apparent antiquity. Some of the patriarchs are of enormous girth; even the younger ones have a circumference of eighteen feet; and the height is such that the birds which dwell among the upper branches are beyond the range of an ordinary fowling-piece.

      But it is through the contrasts which it presents that Lebanon has its extraordinary power of attracting and delighting the traveller. Below the upper line of bare and worn rock, streaked in places with snow, and seamed with torrent courses, a region is entered upon where the freshest and softest mountain herbage, the greenest foliage, and the most brilliant flowers alternate with deep dells, tremendous gorges, rocky ravines, and precipices a thousand feet high. Scarcely has the voyager descended from the upper region of naked and rounded rock, when he comes upon “a tremendous chasm—the bare amphitheatre of the upper basin contracts into a valley of about 2,000 feet deep, rent at its bottom into a cleft a thousand feet deeper still, down which dashes a river, buried between these stupendous walls of rock. All above the chasm is terraced as far as the eye can reach with indefatigable industry. Tiny streamlets bound and leap from terrace to terrace, fertilising them as they rush to join the torrent in the abyss. Some of the waterfalls are of great height and of considerable volume. From one spot may be counted no less than seven of these cascades, now dashing in white spray over a cliff, now lost under the shade of trees, soon to reappear over the next shelving rock."138 Or, to quote from another writer,139—“The descent from the summit is gradual, but is everywhere broken by precipices and towering rocks, which time and the elements have chiselled into strange fantastic shapes. Ravines of singular wildness and grandeur furrow the whole mountain-side, looking in many places like huge rents. Here and there, too, bold promontories shoot out, and dip perpendicularly into the bosom of the Mediterranean. The ragged limestone banks are scantily clothed with the evergreen oak, and the sandstone with pines; while every available spot is carefully cultivated. The cultivation is wonderful, and shows what all Syria might be of under a good government. Miniature fields of grain are often seen where one would suppose that the eagles alone, which hover round СКАЧАТЬ