The Land of Midian, vol 2 | Page 7

twenty thousand souls. But that extent by no means represents the whole; our next march will prolong it along the valley for a total of at least four miles. The material is various--boulders of granite and syenite; squares of trap and porphyry; the red sandstones of the Hismá; the basalts of the Harrah; and the rock found in situ, a brown and crumbling grit, modern, and still in process of agglutination. The heaps and piles which denote buildings are divided by mounds and tumuli of loose friable soil, white with salt,--miniatures of Babylon, Nineveh, and Troy. On either flanks of the river-holm the periodical torrents have done their worst, cutting up the once regular bank into a succession of clay buttresses. On the right side we find a large fort, half sliced away, but still showing the concrete flooring of a tower. About the centre of the length are the remnants of a round Burj; blocks of buildings, all levelled to the foundations, lie to the north-west, and on the west appear signs of a square. Perhaps the most interesting discovery is that of catacombs, proving a civilization analogous to Magháir Shu'ayb, but ruder, because more distant from the centre. The "caves" are hollowed in a long reef of loose breccia, which, fronting eastward, forms the right bank of the smaller branch. They are now almost obliterated by being turned into sheep-folds; the roofs have fallen in, and only one preserves the traces of two loculi.
The arrangements touching fuel and water in this great metal-working establishment are on a large scale. The biggest of the Afrán ("furnaces") lies to the north-west, near the right bank of the valley: all are of the ordinary type, originally some five or six feet high, to judge from the bases. They are built of fire-brick, and of the Hismá stone, which faces itself into a natural latex. We dug deep into several of them; but so careful had been the workmen, or perhaps those who afterwards ransacked these places, that not the smallest tear of metal remained: we found only ashes, pottery, and scoriae, as usual black and green, the latter worked sub-aerially; many of them had projections like stalactite. Round the furnaces are strewed carbonate of lime, stained black with iron, like that of Sharmá; and a quantity of the chlorite-enamelled serpentine still used in the Brazil as a flux.
Quartz was absent, and we were at a loss to divine what stone had been worked. At last we observed near the catacombs sundry heaps of pinkish earth, evidently washed out; and our researches in the South Country afterwards suggested that this may have been the remains of the micaceous schist, whose containing quartz was so extensively worked at Umm el-Haráb. Moreover, a short study of Shaghab threw more light on the matter.
Water also had been stored up with prodigious labour. We could easily trace the lines of half a dozen aqueducts, mostly channelled with rough cement, overlying a fine concrete; some of them had grooved stones to divert the stream by means of lashers. The Fiskíyyah or "tanks," as carefully built, were of all sizes; and the wells, which appeared to be mediaeval, were lined with stones cut in segments of circles: we shall see the same curve in Sultán Selim's work near Zibá. The greatest feat is an aqueduct which, sanded over in the upper part, subtends the left side of the valley. It is carefully but rudely built, and where it crosses a gully, the "horizontal arch" is formed of projecting stone tiers, without a sign of key. This magnum opus must date from the days when the southern part of the Wady was nearly what it is now.
About a mile and a quarter below our camp, the Wady, which broadens to a mile, shows on the left bank a wall measuring a thousand metres long, apparently ending in a tank of 110 feet each way. Around it are ruined parallelograms of every size, which in ancient times may have been workshops connected with the buildings in the island higher up. The torrents have now washed away the continuation, if ever there was any; and, though the lower remnants are comparatively safe upon their high ledge, the holm is evidently fated to disappear.
I did not learn till too late that a single day's march southwards from the Wady Shuwák, along the old main line of traffic, leads to the Wady Nejd, upon whose upper course is the plain of Badá; and which, after assuming four different names, falls, as will be seen, into the sea about thirty-five miles north of El-Wijh.
We left Shuwák considerably posed, puzzled, and perplexed by what it had shown us. A little pottery had been picked up, but our diggings had not produced a coin or even