Joshua rose up early in the morning; and they removed from Shittim, and came to the Jordan, he and all the children of Israel; and they lodged there before they passed over.
The Jordan, then, by far the most important river of Palestine, is formed, near its northern frontiers, by several streams which descend from the mountains of Lebanon, and after flowing nearly due south, for a direct distance of about 175 miles, discharges its waters into the north side of the Dead Sea. In the upper part of its course, before it reaches the late of Tiberius, more familiarly known by its usual scriptural name of the Sea of Galilee, it has much of the character of an impetuous torrent, and is hemmed closely in on both sides by loftly mountains, but on issuing from the south side of the lake, it begins to flow in a valley, the most remarkable circumstance connected with which, is its great depth beneath the level of the ocean. Even the Sea of Galilee is 84 feet, and the Dead Sea, where the Jordan falls into it is 1337 feet beneath this level. The intervening space between the two seas, forms what is properly called the valley of the Jordan, and consists of a plain, about six miles across in its northern, but much wider in its southern half, where it spreads out, on its east or left bank, into the plains of Moab, and on its west or right bank, into the plains of Jericho. This valley, throughout its whole length, is terminated on either side by a mountain chain, which in many parts rises so rapidly as soon to attain a height exceeding 2500. Within the valley thus terminated, a minor valley is enclosed. It is about three quarters of a mile in breadth, and consists, for the most part, of a low flat, bounded by sandy slopes, and covered by trees or brushwood. Nearly in the center of this flat the river, almost concealed beneath its overhanging banks, pursues its course, with few large windings, but with such a multiplicity of minute tortuosities, that though the direct distance is not more than sixty-five, the indirect distance or total length of the stream is estimated at not less than two hundred miles. The river, in its ordinary state, within its banks, has a width of from twenty to thirty yards, and a depth, varying from nine to fifteen feet. The banks are there from twelve to fourteen feet high, and immediately beyond them, the flat bears evident marks of being frequently inundated. These inundation’s take place in spring, and are caused by the melted snow brought down, partly by the three principal tributaries of the Jordan, the Jarmuch, or Shurat-el-Mandour, the Jabbok, or Zerka, and the Arnon, or Wady Modjet, which all join it from the east, but chiefly by the main stream, which is then copiously supplied from the snowy heights of Lebanon. This rising of the waters, of course, begins as soon as the thawing influence of the returning heat begins to be felt, but does not attain its maximum till the impression has been fully made, or, in the first weeks of April. Such was the state of the stream as the Israelites now safely assumed to have been from seven to Twelve miles north of the Dead Sea, and not far from the Bethabarah, where our Savior, after condescending to receive baptism at the hands of his forerunner, went up from the banks, while the heavens opened, and the Spirit of God descended like a dove, and lighted upon him. — Ed. 