Two or three hours brought us to the foot of Jebal Sun-neen, and up near the foot of the snows. Here we selected a good spot, and again pitched our tents; intending to employ the next day in our ascent to the top and return to the same place. We found it much colder than it was in the lower parts of the mountain. We really needed fire; but it was with difficulty that wood enough could be procured to make our tea, much more to make a fire to warm half-a-dozen people in the open air. We had, however, expected this, and brought clothing accordingly, so that we did not suffer much. In the morning, we began the ascent; we rode nearly an hour, and took a donkey still farther for the benefit of the ladies; but then left all our animals, and betook ourselves in good earnest to the matter of ascending the Mount. On the side which we ascended, between where we encamped and the top, are two or three offsets, then the mountain falls off and leaves a kind of level. These general levels have small ridges and round hills on them, and many deep valleys and sink-holes, or holes of that peculiar kind which abound in districts where a horizontal limestone stratum lies on the surface. In these deep sink-hole places, and in the valleys, and on the sides of the ridges, the snow was accumulated in great quantities, but it did not cover the whole surface of the mountain, as I had supposed it might. But a small part of the mountain had snow on it. It lay in patches, and possibly not over one-twentieth part was covered with it. I saw no ice--all was snow. From the action of the sun and wind, it was just hard enough to walk on with safety. The foot would sink in it one, two, or three inches--seldom more. I walked on it in my shoes without inconvenience. We were three hours in reaching the top--we proceeded slowly, and stopped frequently to allow the ladies rest. We found the summit much like the offset, which I have just described. There was what may be called a general level, of a mile or two across, with many rises in it, and full of deep holes of various shapes, some nearly round, others long and narrow. These were full of snow. It was usually much melted at one side, and the largest masses were, as a general thing, found lying on the west or south-west side of the hollow. What appeared most singular, was the fact, that for the most part, the outsides of this great cone appeared the highest--around it were the highest knolls, while the inner parts were lower, and its holes and sinks more deep. The rain and snow water does not seem to flow over and down the outside of the cone, but sinks in it, and finds its way out as it can.