History of Phoenicia. George Rawlinson

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СКАЧАТЬ 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 them, could have planted the seed. Fig-trees cling to the naked rock; vines are trained along narrow ledges; long ranges of mulberries on terraces like steps of stairs cover the more gentle declivities; and dense groves of olives fill up the bottoms of the glens. Hundreds of villages are seen, here built amid labyrinths of rock, there clinging like swallows’ nests to the sides of cliffs, while convents, no less numerous, are perched on the top of every peak. When viewed from the sea on a morning in early spring, Lebanon presents a picture which once seen is never forgotten; but deeper still is the impression left on the mind, when one looks down over its terraced slopes clothed in their gorgeous foliage, and through the vistas of its magnificent glens, on the broad and bright Mediterranean.”

      The eastern flank of the mountain falls very far short of the western both in area and in beauty. It is a comparatively narrow region, and presents none of the striking features of gorge, ravine, deep dell, and dashing stream which diversify the side that looks westward. The steep slopes are generally bare, the lower portion only being scantily clothed with deciduous oak, for the most part stunted, and with low scrub of juniper and barberry.140 Towards the north there is an outer barrier, parallel with the main chain, on which follows a tolerably flat 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, СКАЧАТЬ