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History of Phoenicia. George Rawlinson
Читать онлайн.Название History of Phoenicia
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isbn 4057664640888
Автор произведения George Rawlinson
Жанр Документальная литература
Издательство Bookwire
The mountain ranges, which belong in some measure to the geography of Phoenicia, are four in number—Carmel, Casius, Bargylus, and Lebanon. Carmel is a long hog-backed ridge, running in almost a straight line from north-west to south-east, from the promontory which forms the western protection of the bay of Acre to El-Ledjun, on the southern verge of the great plain of Esdraelon, a distance of about twenty-two miles. It is a limestone formation, and rises up abruptly from the side of the bay of Acre, with flanks so steep and rugged that the traveller must dismount in order to ascend them,123 but slopes more gently towards the south, where it is comparatively easy of access. The greatest elevation which it attains is about Lat. 32º 4´, where it reaches the height of rather more than 1,200 feet; from this it falls gradually as it nears the shore, until at the convent, with which the western extremity is crowned, the height above the sea is no more than 582 feet. In ancient times the whole mountain was thickly wooded,124 but at present, though it contains “rocky dells” where there are “thick jungles of copse,"125 and is covered in places with olive groves and thickets of dwarf oak, yet its appearance is rather that of a park than of a forest, long stretches of grass alternating with patches of woodland and “shrubberies, thicker than any in Central Palestine,” while the larger trees grow in clumps or singly, and there is nowhere, as in Lebanon, any dense growth, or even any considerable grove, of forest trees. But the beauty of the tract is conspicuous; and if Carmel means, as some interpret, a “garden” rather than a “forest,” it may be held to well justify its appellation. “The whole mountain-side,” says one traveller,126 “was dressed with blossoms and flowering shrubs and fragrant herbs.” “There is not a flower,” says another,127 “that I have seen in Galilee, or on the plains along the coast, that I do not find on Carmel, still the fragrant, lovely mountain that he was of old.”
The geological structure of Carmel is, in the main, what is called “the Jura formation,” or “the upper oolite”—a soft white limestone, with nodules and veins of flint. At the western extremity, where it overhangs the Mediterranean, are found chalk, and tertiary breccia formed of fragments of chalk and flint. On the north-east of the mountain, beyond the Nahr-el-Mukattah, plutonic rocks appear, breaking through the deposit strata, and forming the beginning of the basalt formation which runs through the plain of Esdraelon to Tabor and the Sea of Galilee.128 Like most limestone formations, Carmel abounds in caves, which are said to be more than 2,000 in number,129 and are often of great length and extremely tortuous.
Carmel, the great southern headland of Phoenicia, is balanced in a certain sense by the extreme northern headland of Casius. Mount 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