[Sidenote: ASCENT TOWARDS PASS. _May, 1848._]

In the lower part of the ascent, the rock was clay-slate; but near my camp it was succeeded by the same gneiss, with large crystals of felspar, which I had found (in boulders) around Dadu. In general appearance, this gneiss was very similar to that observed on the mountains north of Nasmon, on the Chenab; and as these two places have nearly the same relative position as the usual line of strike in the north-western Himalaya, it is very probable that the rock is the same in both.

Western Himalaya and Tibet — Part 204

On the morning of the 1st of June, I continued to follow the course of the stream, ascending now very gently. The valley was open, and the road lay over undulating grassy ground, the forest having receded to some distance on both sides. Round my camp I had noticed very little in the vegetation different from what was common one or two thousand feet lower; but almost immediately after starting, I found myself among numerous bushes of _Rhododendron campanulatum_ in full flower, and many other alpine plants appeared very shortly afterwards: of these, perhaps the most lovely was the elegant _Primula rosea_, which was extremely plentiful in hollow marshy spots from which snow had recently melted.

Western Himalaya and Tibet — Part 204

[Sidenote: PASS SOUTH OF BADARWAR _June, 1848._]

Western Himalaya and Tibet — Part 204

The ascent continued exceedingly gentle till close to the end, when, turning suddenly to the left into a pine-clad ravine, a few steps brought me to the crest of the ridge over which my road ran,--a lateral spur from the great snowy mass, which (as is often the case) was a good deal lower where it branched off than at a greater distance from the main range. After gaining the crest of the ridge, I followed it for a few hundred yards previous to commencing the descent. I had unfortunately somewhat rashly concluded, the day before, that the ascent during the day would be very trifling, and therefore did not carry with me the means of ascertaining the elevation of the pass; I believe, however, that it a little exceeded 11,000 feet. It was still in the forest zone. The trees were mostly the alpine oak, with a few scattered individuals of _Pinus excelsa_. At a short distance, on the more shady slope, and still higher than the pass, _Picea_ was plentiful. The highest level of trees only rose a few hundred feet above me, and the lofty snowy peak which lay to the southward, attaining a height of probably little under 14,000 feet, was quite bare.