History of Phoenicia. George Rawlinson
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indigenous, but formed a leading and striking characteristic, everywhere along the low sandy shore lifting its tuft of feathery leaves into the bright blue sky, high above the undergrowth of fig, and pomegranate, and alive. Hence they called the tract Phoenicia, or “the Land of Palms;” and the people who inhabited it the Phoenicians, or “the Palm-tree people.”
The term was from the first applied with a good deal of vagueness. It was probably originally given to the region opposite Cyprus, from Gabala in the north—now Jebili—to Antaradus (Tortosa) and Marathus (Amrith) towards the south, where the palm-tree was first seen growing in rich abundance. The palm is the numismatic emblem of Aradus, and though not now very frequent in the region which Strabo calls “the Aradian coast-tract," must anciently have been among its chief ornaments. As the Grecian knowledge of the coast extended southward, and a richer and still richer growth of the palm was continually noticed, almost every town and every village being embosomed in a circle of palm groves, the name extended itself until it reached as far south at any rate as Gaza, or (according to some) as Rhinocolura and the Torrens Ægypti. Northward the name seems never to have passed beyond Cape Posideium (Possidi) at the foot of Mount Casius, the tract between this and the range of Taurus being always known as Syria, never as Phoenecia or Phoenicé.
The entire length of the coast between the limits of Cape Possidi and Rhinocolura is, without reckoning the lesser indentations, about 380 miles, or nearly the same as that of Portugal. The indentations of the coast-line are slight. From Rhinocolura to Mount Carmel, a distance of 150 miles, not a single strong promontory asserts itself, nor is there a single bay of sufficient depth to attract the attention of geographers. Carmel itself is a notable headland, and shelters a bay of some size; but these once passed the old uniformity returns, the line being again almost unbroken for a distance of seventy-five miles, from Haifa to Beyrout (Berytus). North of Beyrout we find a little more variety. The coast projects in a tolerably bold sweep between the thirty-fourth parallel and Tripolis (Tarabulus) and recedes almost correspondingly between Tripolis and Tortosa (Antaradus), so that a deepish bay is formed between Lat. 34º 27´ and Lat. 34º 45´, whence the line again runs northward unindented for fifty miles, to beyond Gabala (Jebili). After this, between Gabala and Cape Posideium there is considerable irregularity, the whole tract being mountainous, and spurs from Bargylus and Casius running down into the sea and forming a succession of headlands, of which Cape Posideium is the most remarkable.
But while the name Phoenicia is applied geographically to this long extent—nearly 400 miles—of coast-line, historically and ethnically it has to be reduced within considerably narrower limits. A race, quite distinct from that of the Phoenicians, was settled from an early date on the southern portion of the west Asian coast, where it verges towards Africa. From Jabneh (Yebna) southwards was Palestine, the country of the Philistines, perhaps even from Joppa (Jaffa), which is made the boundary by Mela. Thus at least eighty miles of coast-line must be deducted from the 380, and the length of Phoenicia along the Mediterranean shore must be regarded as not exceeding three hundred miles.
The width varied from eight or ten miles to thirty. We must regard as the eastern boundary of Phoenicia the high ridge which forms the watershed between the streams that flow eastward toward the Orontes, Litany, and Jordan, and those that flow westward into the Mediterranean. It is difficult to say what was the average width, but perhaps it may be fairly estimated at about fifteen miles. In this case the entire area would have been about 4,500 square miles.
The tract was one of a remarkably diversified character. Lofty mountain, steep wooded hill, chalky slope, rich alluvial plain, and sandy shore succeeded each other, each having its own charm, which was enhanced by contrast. The sand is confined to a comparatively narrow strip along the seashore, and to the sites of ancient harbours now filled up. It is exceedingly fine and of excellent silicious quality, especially in the vicinity of Sidon and at the foot of Mount Carmel. The most remarkable plains are those of Sharon, Acre, Tyre, Sidon, Beyrout, and Marathus. Sharon, so dear to the Hebrew poets, is the maritime tract intervening between the highland of Samaria and the Mediterranean, extending from Joppa to the southern foot of Carmel—a distance of nearly sixty miles—and watered by the Chorseas, the Kaneh, and other rivers. It is a smooth, very slightly undulating tract, about ten miles in width from the sea to the foot of the mountains, which rise up abruptly from it without any intervening region of hills, and seem to bound it as a wall, above which tower the huge rounded masses of Ebal and Gerizim, with the wooded cone, on which stood Samaria, nestling at their feet. The sluggish streams, several of them containing water during the whole of the year, make their way across it between reedy banks, and generally spread out before reaching the shore into wide marshes, which might be easily utilised for purposes of irrigation. The soil is extremely rich, varying from bright red to deep black, and producing enormous crops of weeds or grain, according as it is cultivated or left in a state of nature. Towards the south the view over the region has been thus described: “From Ramleh there is a wide view on every side, presenting a prospect rarely surpassed in richness and beauty. I could liken it to nothing but the great plain of the Rhine by Heidelberg or, better still, to the vast plains of Lombardy, as seen from the cathedral of Milan and elsewhere. In the east the frowning mountains of Judah rose abruptly from the tract at their foot; while on the west, in fine contrast, the glittering waves of the Mediterranean Sea associated our thoughts with Europe. Towards the north and south, as far as the eye could reach, the beautiful plain was spread out like a carpet at our feet, variegated with tracts of brown from which the crops had just been taken, and with fields still rich with the yellow of the ripe corn, or green with the springing millet. Immediately below us the eye rested on the immense olive groves of Ramleh and Lydda, and the picturesque towers and minarets and domes of these large villages. In the plain itself were not many villages, but the tract of hills and the mountain-side beyond, especially in the north-east, were perfectly studded with them, and as now seen in the reflected beams of the setting sun they seemed like white villas and hamlets among the dark hills, presenting an appearance of thriftiness and beauty which certainly would not stand a closer examination." Towards its northern end Sharon is narrowed by the low hills which gather round the western flanks of Carmel, and gradually encroach upon the plain until it terminates against the shoulder of the mountain itself, leaving only a narrow beach at the foot of the promontory by which it is possible to communicate with the next plain towards the north.
Compared with Sharon the plain of Acre is unimportant and of small extent. It reaches about eight miles along the shore, from the foot of Carmel to the headland on which the town of Acre stands, and has a width between the shore and the hills of about six miles. Like Sharon it is noted for its fertility. Watered by the two permanent streams of the Kishon and the Belus, it possesses a rich soil, which is said to be at present “perhaps the best cultivated and producing the most luxuriant crops, both of corn and weeds, of any in Palestine." The Kishon waters it on the south, where it approaches Carmel, and is a broad stream, though easily fordable towards its mouth. The Belus (Namâané) flows through it towards the north, washing Acre itself, and is a stream of even greater volume than the Kishon, though it has but a short course.
The third of the Phoenician plains, as we proceed from south to north, is that of Tyre. This is a long but comparatively narrow strip, reaching from the Ras-el-Abiad towards the south to Sarepta on the north, a distance of about twenty miles, but in no part more than five miles across, and generally less than two miles. It is watered about midway by the copious stream of the Kasimiyeh or Litany, which, rising east of Lebanon in the Buka’a or Coelesyrian valley, forces its way through the mountain chain by a series of tremendous gorges, and debouches upon the Tyrian lowland about three miles to the south-east of the present city, near the modern Khan-el-Kasimiyeh, whence it flows peaceably to the sea with many windings through a broad low tract of meadow-land. Other rills and rivulets descending from the west flank of the great mountain increase the productiveness of the plain, while copious fountains of water gush forth with surprising force in places, more especially at Ras-el-Ain, three miles from Tyre, to the south. The plain is, even at the present day, to a large extent covered with orchards, gardens, and cultivated fields, in which are grown rich crops of tobacco, cotton, and cereals.
The plain of Sidon, which follows that of Tyre, and is sometimes regarded as a part of it, extends from a little north of Sarepta to the Ras-el-Jajunieh, a distance of about ten miles, and resembles that of Tyre in its principal features. It