They come and go in all directions, even after starting, not always preserving the original direction. They are less common on days in which winds prevail from any given direction, and vary much in intensity from a mere breeze, lightly laden with dust and with no tortuosity, to a violent cone of wind, capable of throwing down a soldari.
Northerly winds are prevalent here from 1 or 2 P.M. until 8 or 9 P.M., occasionally they only commence in the evening, when they are obviously due to the rarefaction of the air of the valleys by the great heat of the sun, amounting now to 100° at 3 P.M., and the vacuum being supplied by gusts from the high mountains to the north and north-east.
CHAPTER XVIII.
From Peshawur to Pushut.
January 8th.—At Ichardeh. Between Busoollah and Lalpoor are three curious low ridges, none above sixty feet high, and all of small extent; they are covered with fractured masses of rock of the same size as those strewn so liberally about the shingly slopes; but they are much cleaner or fresher looking, and appear to me less worn. Whence do they derive their singular situation? They occur in such numbers, that one would at first think they originated from a mass of ruins, but the ridges present scarcely any surface for buildings to stand upon, certainly not to such extent as would account for the abundance of these fragments.
About Huzarnow and on both sides, low ridges of sand occur. In this sand graves are usually dug, and in some places to an extent indicating dreadful devastations from disease, each grave is headed by a stone, and about every ramification of the irregular size of the burial ground, there is a building of the usual mud structure, designed for a mosque, but not domed as is customary in Mussulman cemeteries, but ornamented with flagstaffs bearing white bits of cloth. These low sand ridges are often very much undulated; they consist of a very fine powder, and at Huzarnow are evidently of the same nature as the cultivated soil: they are neither in attachment as it were to the neighbouring hills, nor distinct from them, but always have some communication with the shingly slopes, to which they are evidently inferior.
So that the base of Khorassan may be taken to be the tillable portions, over which occur, to a vast extent, the shingly very barren slopes, which every section shows to be nothing but a mass of debris, resting on the mountain rocks.
9th.—Ali-Baghan. To this the road is good, along the right bank of the river, wherever it does not wind along over the spurs forming a considerable part of the march. To the first point where this occurs, it extends over the same sort of plain as that about Ichardeh; keeping rather close to the bank of the river, it is good, also through the valley of Gundikuss, and from near the Choky, to Ali-Baghan.
The first rocky ridge is about three-quarters of a mile in length, and is not very difficult; at the end near Gundikuss, is a curious ruin built into the stream, where the latter runs with violence on the rocky bank: it consists of a broadish pathway, with a wall on the river side, breast high; the masonry is good and solid, of the usual Bactrian materials, but well cemented; it has mostly been ruined by the river, only one end being perfect. Although the materials are Bactrian, the contour is Mussulman, and I was told by some people that it was a Mussulman erection: originally it perhaps extended all along this part, as slight traces here and there are discernible; for what use the original structure was intended I know not, as there are no remains visible of a fort.
The inlet of Gundikuss is well cultivated, the village itself a large straggling one, built close under a ridge.