either with sh, the old relative pronoun of the Phoenician, or with the Assyrian sha; on the latter supposition one must suppose, as Sayce does, that the compiler of the Egyptian lists had before him sources of information in the cuneiform character.  Birkana appears to be the modern Brukin, and Dutina is certainly Dothain, now Tell-Dothan.

Beyond Ono reddish-coloured sandy clay took the place of the dark and compact loam:  oaks began to appear, sparsely at first, but afterwards forming vast forests, which the peasants of our own days have thinned and reduced to a considerable extent.  The stunted trunks of these trees are knotted and twisted, and the tallest of them do not exceed some thirty feet in height, while many of them may be regarded as nothing more imposing than large bushes.* Muddy rivers, infested with crocodiles, flowed slowly through the shady woods, spreading out their waters here and there in pestilential swamps.  On reaching the seaboard, their exit was impeded by the sands which they brought down with them, and the banks which were thus formed caused the waters to accumulate in lagoons extending behind the dunes.  For miles the road led through thickets, interrupted here and there by marshy places and clumps of thorny shrubs.  Bands of Shausu were accustomed to make this route dangerous, and even the bravest heroes shrank from venturing alone along this route.  Towards Aluna the way began to ascend Mount Carmel by a narrow and giddy track cut in the rocky side of the precipice.**

     * The forest was well known to the geographers of the Graeco-
     Roman period, and was still in existence at the time of the
     Crusades.

** This defile is described at length in the Anastasi Papyrus, No. 1, and the terms used by the writer are in themselves sufficient evidence of the terror with which the place inspired the Egyptians.  The annals of Thutmosis III. are equally explicit as to the difficulties which an army had to encounter here.  I have placed this defile near the point which is now called Umm-el-Fahm, and this site seems to me to agree better with the account of the expedition of Thutmosis III. than that of Arraneh proposed by Conder.

Beyond the Mount, it led by a rapid descent into a plain covered with corn and verdure, and extending in a width of some thirty miles, by a series of undulations, to the foot of Tabor, where it came to an end.  Two side ranges running almost parallel—­little Hermon and Glilboa—­disposed in a line from east to west, and united by an almost imperceptibly rising ground, serve rather to connect the plain of Megiddo with the valley of the Jordan than to separate them.  A single river, the Kishon, cuts the route diagonally—­or, to speak more correctly, a single river-bed, which is almost waterless for nine months of the year, and becomes swollen only during the winter rains with the numerous torrents bursting from the hillsides.  As the flood approaches the sea it becomes of more manageable proportions, and finally distributes its waters among the desolate lagoons formed behind the sand-banks of the open and wind-swept bay, towered over by the sacred summit of Carmel.*