History of Phoenicia

n of the name-S

ength of Phoenici

General character

aron-Plain of Acre

f Berytus-Plain

anges-Carmel-Casiu

Rivers-The Litany-

Adonis-The Lycus

Zaherany-The

inaccessibility

ctive

e, it would seem, in their early voyagings, the Pre-Homeric Greeks first came upon a land where the palm-tree was not only indigenous, but formed a leading and striking characteristic, everywhere along the low sandy shore lifting its tuft of

not now very frequent in the region which Strabo calls "the Aradian coast-tract,"12 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, t

lf 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 (An

he 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

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 w

e wooded cone, on which stood Samaria, nestling at their feet.16 The sluggish streams, several of them containing water during the whole of the year, make their way across it between reedy banks,17 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

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."110 The Kishon wate

, 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 fr

ell-watered and very fertile. The principal streams are the Bostrenus (Nahr-el-Auly) in the north, just inside the promontory of Jajunieh, the Nahr-San?k, south of Sidon, a torrent dry in the summer-time,114 and the Nahr-ez-Zaherany, two and a half miles north of Sarepta, a river of moderate capacity. Fine foun

he skirts of Lebanon, which here approach very near to the sea. The plain begins at Wady Shuweifat on the south, about four miles from the town of Beyrout, and extends northwards to the sea on the western side of the Nahr Beyrout. The northern part of the plain is known

he Nahr Amrith, a strong running brook which empties itself into the sea a few miles south of Tortosa (Antaradus), the Nahr Kublé, which joins the Nahr Amrith near its mouth, and the Eleutherus or Nahr-el-Kabir, which reaches the sea a little north of Arka. Of these the Eleutherus is the most important. "It is a considerable stream even in summer, and in the rainy season it is a barrier to intercourse, caravans sometimes remaining encamped on its banks for sever

escribed; but, not unfrequently, it commences at the water's edge, and fills with its undulations the entire space, leaving not even a strip of lowland. This is especially the case in the central region between Berytus and Arka, opposite the highest portion of the Lebanon; and again in the north between Cape Possidi and Jebili, opposite the more n

y 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,

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 formatio

e 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;

outh, 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 pi

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

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 wi

, 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

wards 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 flourish

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 dow

ore, 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, and a deep and narrow chasm opens in it, down which the stream plunges in a cleft 200 feet deep, and so narrow that in one place it is actually bridged over by masses of rock which have fallen from the cliffs above.145 In the gully below fig-trees and planes, besides many shrubs, find a footing, and the moist walls of rock on either side are hung with ferns of various kinds, among which is conspicuous the delicate and graceful maidenhair. Further down the chasm deepens, first to 1,000

the Coelesyrian valley, and, receiving affluents from either side, flows westward between Bargylus and Lebanon to the Mediterranean, which it enters between Orthosia (Artousi) and Marathus (Amrith) with a stream, the volume of which is even in the summer-time considerable. In the rainy season

of which the ancient name is unknown to us. The Nahr-el-Berid drains the north-western angle of the mountain chain, and is formed of two main branches, one coming down from the higher portion of the range, about Lat. 34o 20′, and flowing to the north-west, while the other descends from a region of much less ele

corner among the jagged rocks, every ledge and cranny on precipice-side, which the foot of man can reach, or on which a basket of earth can be deposited, is occupied with patch of corn or fruit-tree.150 Lower down near Canobin the valley contracts into a sublime chasm, its rocky walls rising perpendicularly a thousand feet on either side, and in places not leaving room for even a footpath beside the stream that flows alo

tary from the north-east, it shapes its course nearly westward, and pursues this direction, with only slight bends to the north and south, for the distance of about fifteen miles to the sea. After heavy rain in Lebanon, its waters, which are generally clear and limpid, b

the river constituted by the union of these two branches is joined by a third stream flowing from the western flank of Sunnin with a westerly course, and from this point the Lycus pursues its way in the same general direction down a magnificent gorge to the Mediterranean. Both banks are lofty, but especially that to the south, where one of Lebanon's great roots strikes out far, and

about Barouk and Deir-el-Kamar. It collects the waters from an area of about 110 square miles, and carries them to the sea in a course which is a little north

by a stream from Jezzin, which flows into it from the south-east. On receiving this stream, the Auly turns almost at a right angle, and flows to the west down the fine alluvial track called Merj

breaks through one of the spurs from Rihan by a magnificent chasm. The gorge is one "than which there are few deeper or more savage in Lebanon. The mountains on each side rise up almost precipitously to the height of two or three thousand feet above the stream, that on the northern bank being considerably the higher. The steep sides of the southern mountain are dotted with shrub, oak, and other dwarf trees."158 The river descends in its chasm still in a south-west direction until, just opposite Arab Salim, it "turns round the precipit

en cut with great labour through the rock, and is said by tradition to have been the work of Alexander the Great. Previously, both here and at the Ras-en-Nakura, the ascent was by steps, and the passes were known as the Climaces Tyriorum, or "Staircases of the Tyrians." Another similar precipice guards the mouth of the Lycus on its south side and has been engineered with considerable skill, first by the Egyptians and then by the Romans.161 North of this, at Djouni, the coast road "traverses another pass, where the m

must have soon turned their thoughts to the possibility of communicating by sea. The various "staircases" were painful and difficult to climb, they gave no passage to animals, and only light forms of merchandise could be conveyed by them. As

ook no note of its marvellous and almost unequalled beauty, must at any rate have seen that here was one of earth's most productive gardens-emphatically a "good land," that might well content whosoever should be so fortunate as to possess it. There is nothing equal to it in Western Asia. The Damascene oasis, the lower valley of the Orontes, the Ghor or Jordan plain, the woods of Bashan, and the downs of Moab are fertile and attractive regions; but they are comparatively narrow tracts and present little variety; each is fitted mainly for one kind of growth, one class of products. Phoenicia, in its long extent fr