Note 11 — Chapter XII · ASCENT OF ARARAT

Disappointed perhaps, but relieved of the gradient, and elated with the success of our climb, we run in the teeth of the wind across the platform, our feet scarcely sinking in the storm-swept crust of the surface, the gently undulating roof of the dome.... Along the edge of a spacious snow-field which dips towards the centre, and is longest from north-west to south-east, on the vaulted rim of the saucer which the surface resembles, four separate elevations may conveniently be distinguished as the highest points in the irregular oval figure which the whole platform appears to present. The highest among these rounded elevations bears north-west from the spot where we first touch the summit or emerge upon the roof. That spot itself marks another of these inequalities; the remaining two are situated respectively in this manner—the one about midway between the two already mentioned, but nearer to the first and on the north side; the other about south of the north-western elevation, and this seems the lowest of all. The difference in height between the north-western elevation and that upon the south-east is about 200 feet; and the length of the figure between these points—we paced only a certain portion of the distance—is about 500 yards. The width of the platform, so far as we could gauge it, may be some 300 yards. A single object testifies to the efforts of our fore-runners and to the insatiable enterprise of man—a stout stake embedded upon the north-western elevation in a little pyramid of stones. It is here that we take our observations, and make our longest halt.11 Before us lies a valley or deep depression, and on the further side rises the north-western summit, a symmetrical cone of snow. This summit connects with the bold snow buttresses beyond it, terraced upon the north-western slope. The distance down and up from where we stand to that summit may be about 400 yards; but neither the Swiss nor ourselves consider it higher, and we are prevented from still further exploring the summit region by the increasing violence of the gale and by the gathering gloom of cloud. The sides and floor of the saddle between the two summits are completely covered with snow, and we see no trace of the lateral fissure which Abich, no doubt under different circumstances, was able to observe.