BABYLON (Illustrated). George Rawlinson

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СКАЧАТЬ of Antilibanus, in the tract between that range and the great Syrian desert, was another very important district—the district which the Jews called “Aram-Dammesek,” and which now forms the chief part of the Pashalik of Damascus. From the eastern flanks of the Antilibanus two great and numerous smaller streams flow down into the Damascene plain, and, carrying with them that strange fertilizing power which water always has in hot climates, convert the arid sterility of the desert into a garden of the most wonderful beauty. The Barada and Awaaj, bursting by narrow gorges from the mountain chain, scatter themselves in numerous channels over the great flat, intermingling their waters, and spreading them out so widely that for a circle of thirty miles the deep verdure of Oriental vegetation replaces the red hue of the Hauran. Walnuts, planes, poplars, cypresses, apricots, orange-trees, citrons, pomegranates, olives, wave above; corn and grass of the most luxuriant growth, below. In the midst of this great mass of foliage the city of Damascus “strikes out the white arms of its streets hither and thither” among the trees, now hid among them, now overtopping them with its domes and minarets, the most beautiful of all those beautiful towns which delight the eye of the artist in the East. In the south-west towers the snow-clad peak of Hermon, visible from every part of the Damascene plain. West, north-west, and north, stretches the long Antilibanus range, bare, gray, and flat-topped, except where about midway in its course, the rounded summit of Jebel Tiniyen breaks the uniformity of the line. Outside the circle of deep verdure, known to the Orientals as El Merj (“the Meadow”), is a setting or framework of partially cultivable land, dotted with clumps of trees and groves, which extend for many miles over the plain. To the Damascus country must also be reckoned those many charming valleys of Hermon and Antilibanus which open out into it, sending their waters to increase its beauty and luxuriance, the most remarkable of which are the long ravine of the Barada, and the romantic Wady Halbon, whose vines produced the famous beverage which Damascus anciently supplied at once to the Tyrian merchant-princes and to the voluptuous Persian kings.

      Below the Coelo-Syrian valley, towards the south, came Palestine, the Land of Lands to the Christian, the country which even the philosopher must acknowledge to have had a greater influence on the world’s history than any other tract which can be brought under a single ethnic designation. Palestine—etymologically the country of the Philistines—was somewhat unfortunately named. Philistine influence may possibly have extended at a very remote period over the whole of it; but in historical times that warlike people did but possess a corner of the tract, less than one tenth of the whole—the low coast region from Jamnia to Gaza. Palestine contained, besides this, the regions of Galilee, Samaria, and Judaea, to the west of the Jordan, and those of Ituraea, Trachonitis, Bashan, and Gilead, east of that river. It was a tract 140 miles long, by from 70 to 100 broad, containing probably about 11,000 square miles. It was thus about equal in size to Belgium, while it was less than Holland or Hanover, and not much larger than the principality of Wales, with which it has been compared by a recent writer.

      The great natural division of the country is the Jordan valley. This remarkable depression, commencing on the west flank of Hermon, runs with a course which is almost due south from lat. 33° 25’ to lat. 31° 47’, where it is merged in the Dead Sea, which may be viewed, however, as a continuation of the valley, prolonging it to lat. 31° 8’. This valley is quite unlike any other in the whole world. It is a volcanic rent in the earth’s surface, a broad chasm which has gaped and never closed up. Naturally, it should terminate at Merom, where the level of the Mediterranean is nearly reached. By some wonderful convulsion, or at any rate by some unusual freak of Nature, there is a channel opened out from Merom, which rapidly sinks below the sea level, and allows the stream to flow hastily, down and still down, from Merom to Gennesareth, and from Gennesareth to the Dead Sea, where the depression reaches its lowest point, and the land, rising into a ridge, separates the Jordan valley from the upper end of the Gulf of Akabah. The Jordan valley divides Palestine, strongly and sharply, into two regions. Its depth, its inaccessibility (for it can only be entered from the highlands on either side down a few steep watercourses), and the difficulty of passing across it (for the Jordan has but few fords), give it a separating power almost equal to that of an arm of the sea. In length above a hundred miles, in width varying from one mile to ten, and averaging some five miles, or perhaps six, it must have been valuable as a territory, possessing, as it does, a rich soil, abundant water, and in its lower portion a tropical climate.

      On either side of the deep Jordan cleft lies a highland of moderate elevation, on the right that of Galilee, Samaria, and Judsea, on the left that of Ituraea, Bashan, and Gilead. The right or western highland consists of a mass of undulating hills, with rounded tops, composed of coarse gray stone, covered, or scarcely covered, with a scanty soil, but capable of cultivation in corn, olives, and figs. This region is most productive towards the north, barer and more arid as we proceed southwards towards the desert. The lowest portion, Judaea, is unpicturesque, ill-watered, and almost treeless; the central, Samaria, has numerous springs, some rich plains, many wooded heights, and in places quite a sylvan appearance; the highest, Galilee, is a land of water-brooks, abounding in timber, fertile and beautiful. The average height of the whole district is from 1500 to 1800 feet above the Mediterranean. Main elevations within it vary from 2500 to 4000 feet. The axis of the range is towards the East, nearer, that is, to the Jordan valley than to the sea. It is a peculiarity of the highland that there is one important break in it. As the Lowland mountains of Scotland are wholly separated from the mountains of the Highlands by the low tract which stretches across from the Frith of Forth to the Frith of Clyde, or as the ranges of St. Gall and Appenzell are divided off from the rest of the Swiss mountains by the flat which extends from the Rhine at Eagatz to the same river at Waldshut, so the western highland of Palestine is broken in twain by the famous “plain of Esdraelon,” which runs from the Bay of Acre to the Jordan valley at Beth-Shean or Scythopolis.

      East of the Jordan no such depression occurs, the highland there being continuous. It differs from the western highland chiefly in this—that its surface, instead of being broken up into a confused mass of rounded hills, is a table-land, consisting of a long succession of slightly undulating plains. Except in Trachonitis and southern Ituraea, where the basaltic rock everywhere crops out, the soil is rich and productive, the country in places wooded with fine trees, and the herbage luxuriant. On the west the mountains rise almost precipitously from the Jordan valley, above which they tower to the height of 3000 or 4000 feet. The outline is singularly uniform; and the effect is that of a huge wall guarding Palestine on this side from the wild tribes of the desert. Eastward the tableland slopes gradually, and melts into the sands of Arabia. Here water and wood are scarce; but the soil is still good, and bears the most abundant crops.

      Finally, Palestine contains the tract from which it derives its name, the low country of the Philistines, which the Jews called the Shephelah, together with a continuation of this tract northwards to the roots of Carmol, the district known to the Jews as “Sharon,” or “the smooth place.” From Carmol to the Wady Sheriah, where the Philistine country ended, is a distance of about one hundred miles, which gives the length of the region in question. Its breadth between the shore and the highland varies from about twenty-five miles, in the south, between Gaza and the hills of Dan, to three miles, or less, in the north, between Dor and the border of Manasseh. Its area is probably from 1400 to 1500 square miles, This low strip is along its whole course divided into two parallel belts or bands-the first a flat sandy tract along the shore, the Ramleh of the modern Arabs; the second, more undulating, a region of broad rolling plains rich in corn, and anciently clothed in part with thick woods, watered by reedy streams, which flow down from the great highland. A valuable tract is this entire plain, but greatly exposed to ravage. Even the sandy belt will grow fruit-trees; and the towns which stand on it, as Gaza, Jaffa, and Ashdod, are surrounded with huge groves of olives, sycamores, and palms, or buried in orchards and gardens, bright with pomegranates and orange-trees. The more inland region is of marvellous fertility. Its soil is a rich loam, containing scarcely a pebble, which yields year after year prodigious crops of grain—chiefly wheat—without manure or irrigation, or other cultivation than a light ploughing. Philistia was the granary of Syria, and was important doubly, first, as yielding inexhaustible supplies to its conqueror, and secondly as affording the readiest passage to the great armies which contended in these regions for the mastery of the Eastern World.

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