Western Himalaya and Tibet Part 27

[Sidenote: SUMMIT OF Pa.s.s.

_August, 1848._]

From this halting-place the remainder of the ascent was less abrupt, though still steep and extremely stony. There was, however, a little more vegetation than on the lower part, where the barren rocks, except at the very base, produced scarcely anything but _Ephedra_, a dwarf species of _Rhamnus_, and tufts of the hardy _Statice_. Higher up, several species of _Astragalus_ and _Artemisia_ were plentiful, with _Lithospermum euchromon_, _Dracocephalum heterophyllum_, and several _Chenopodiaceae_ and gra.s.ses. The top of the ridge had an elevation of 15,300 feet, but from its extreme aridity and rockiness, and its consequent elevated temperature, no alpine plants occurred. On reaching the top I was able to see something of the road before me, regarding which I had previously had little information, except in accounts of its extreme difficulty. These I had been inclined to consider exaggerated, but the prospect before me was undoubtedly far from tempting. Immediately below lay a narrow stony valley, to which, from the spot on which I stood, the descent was almost perpendicular.

Opposite to me there was a range of mountains higher than that on which I stood, with here and there a patch of snow. The valley below me was partly occupied by a ma.s.s of loose alluvial conglomerate, through which the stream had excavated a deep ravine; its direction was south-south-west, and there could be no doubt that the stream which I had crossed the day before, about half-way, was that which drained the valley upon which I now looked down. On the top of the alluvial platform, on the opposite side, there was a narrow strip of green, indicating a small patch of cultivation, without, however, any habitation, the crop being apparently left to its fate till ready for the reaper. In every other direction, stones and snow were alone visible.

[Sidenote: BARREN VALLEY.

_August, 1848._]

I descended obliquely into the valley, so as to reach it about a mile and a half higher up than the spot from which it was first visible.

The descent was very laborious, a great part of it being covered with loose gravel or coa.r.s.e sand, produced by the disintegration of the granite rocks. There was rather more vegetation than on the opposite face, and I collected a number of plants which I had not recently met with; a _Nepeta_, _Scrophularia_, _Cicer_, and _Heracleum_, and two shrubby _Potentillae_, were the commonest species. One of the species of _Potentilla_ (_P. discolor_ of Jacquemont) was remarkable for exciting violent sneezing when touched or shaken; this curious property seemed to be owing to a very fine dust which covered the under surface of the leaves.

After reaching the surface of the alluvial platform overhanging the stream, about half a mile of gentle ascent among large stones brought me, after a journey of ten miles, to my encamping ground. This was a level spot, close to a lateral torrent, which had its source in a snow-bed in the mountains on the left, and was rushing in a most impetuous milk-white torrent over immense boulders, to unite itself to the main stream. The elevation of my camp was about 14,000 feet.

On the morning of the 11th, at starting, I crossed the torrent close to camp. Although much less considerable than it had been the previous afternoon, still, from its great rapidity and the number of boulders in its bed, the crossing was not accomplished without difficulty by the laden animals, who carried the greater part of my baggage. I crossed it myself by leaping from boulder to boulder, which would have been quite impossible in the afternoon of the previous day, when it was swollen by the action of the sun upon the snow. The road lay up the valley parallel to the river, among a most extraordinary acc.u.mulation of granite boulders of all sizes, from one to ten feet in diameter, piled upon one another in vast heaps, and evidently transported by a former glacier. After about half a mile, I crossed the river by a wooden bridge of two or three beams, which must have been brought from Nubra for the purpose, as no timber of any sort grows in the valley. The stream was very rapid and muddy. A mile further, a torrent descending from the mountains on the right was crossed, and soon after I got upon the bank of the main stream, now more tranquil and fordable. The road for the remainder of the march lay along its left bank, over boulders and gravel, ascending now and then a little way on steep sloping banks, entirely composed of transported materials. I encamped on a level, somewhat gra.s.sy spot of ground, which was evidently commonly used as a halting-place, having travelled only four and a half miles, an unnecessarily short day's work. I had throughout my journey had considerable difficulty in fixing the marches at proper lengths, the inhabitants having no measure of distance but the day's journey. In the present instance, my tent was pitched, and most of the party had commenced to cook, or were dispersed to collect fuel, long before my arrival, so that I was obliged to rest content for the day.

[Sidenote: GLACIER.

_August, 1848._]

The course travelled during the day had been north-north-east, but I had evidently arrived nearly as far as was practicable in that direction, for about half a mile in front was the bluff end of a very large glacier, filling up the continuation of the valley. This glacier, which was nearly half a mile wide, was covered almost entirely with stones and earth, very little of its surface being visible, and the dirty black colour of its terminating cliff showing how much soil had been mixed up with it in its progress. The elevation of my tent was about 14,500 feet, and the termination of the glacier may have been 250 feet higher. All around the mountains were very lofty, their tops covered with snow, which nowhere came within 2000 feet at least of the valley, even on northern exposures. Granite was everywhere the prevailing rock, but on the higher mountain slopes, which were often precipitous, it was much intermixed with a dark rock, probably clay-slate.

[Sidenote: ALPINE NETTLE.

_August, 1848._]

During the day I had scarcely seen any vegetation, except when close to the edge of the stream. Among the boulders and on the bare stony ground there was frequently not a vestige of herbage. Near one of the ravines I found the white shrubby _Potentilla_, along with an exceedingly pretty prostrate plant, with bright rose-coloured flowers, belonging to the order of _Compositae_: it was a species of the genus _Allardia_, described by M. Decaisne from the collections of Jacquemont, by whom it was found in Piti. One of the very few alpine plants which I saw during the day was a little gentian, common among the turf close to my tent. Round camp a species of nettle was plentiful, seemingly, like others of the genus, attracted by the nitrogenous nature of the soil of an encamping ground much frequented by shepherds with their flocks. The sting of this nettle, though rather faint, was quite perceptible. It was decidedly an alpine plant, which is rather uncommon, not only in the genus, but the order to which it belongs.

The journey of the 12th of August commenced by a steep ascent into a lateral valley descending from the eastward. The hill-side up which I climbed (apparently the bluff termination of an ancient moraine) was very stony and dry. When a sufficient elevation above my encampment had been gained, I obtained a commanding view of the glacier which occupied the continuation of the main valley. It was nearly straight, and, as I believe, at least five or six miles long; distances, however, are so difficult to estimate on snow, that this must be regarded as a mere guess. The inclination of its surface was considerable; but, while the distance remained doubtful, no just estimate of the height of the ridge from which it descended could be made. On each side, two or three lateral glaciers, descending from the mountains by which it was enclosed, contributed to increase its size, all loaded with heaps of stones, which had at the lower end of the central glacier so acc.u.mulated as completely to cover its whole surface.

[Sidenote: MORAINES.

_August, 1848._]

After 800 or 1000 feet of ascent I found that I had attained the level of the lateral valley, along which the road ran, and that the remainder of the way was much more gentle, but exceedingly fatiguing, from its excessive roughness, and from the great elevation, which made the slightest exertion difficult. On both sides were high ranges of mountains, which had much snow on their summits, and in one or two ravines there was a small snow-bed or incipient glacier, but the distance from the crest of the ridge not being great, no glacier of any length was formed. On the left hand, the mountains were steeper and higher than those on the right, and several bulky glaciers on very steep slopes occupied their ravines. None of these entered the valley along which my road lay, but their moraines often projected to its very centre, forming immense piles of angular fragments of rocks, which attained, in more than one place, a height of several hundred feet, and indicated that the glaciers had at some former period advanced much further than they now do. The main valley was itself everywhere covered with boulders; in some places large blocks, ten to twenty feet in diameter, were arranged at moderate distances from one another, but more frequently the fragments were all small.

[Sidenote: Sa.s.sAR Pa.s.s.

_August, 1848._]

After the first steep ascent, the slope of the valley was uniformly gentle, except when a steep-sided moraine had to be pa.s.sed. Latterly a few small patches of snow occurred in the valley. I encamped at 16,600 feet, on a level gra.s.sy spot of ground close to a small circular plain resembling the bed of a lake, and still partially covered with snow.

The snow level on the mountains to the south had approached within less than one hundred feet of the level of the plain. Though the distance travelled during the day was only six miles, I felt a good deal fatigued, and suffered much from headache, caused by the rarefaction of the air.

From the great quant.i.ty of snow on the mountains all around, there had been throughout the day an abundance of moisture, and vegetation was in consequence much more plentiful than usual. The plants were all alpine, and being mostly diminutive, had to be sought in the crevices of rocks, and among the stones which everywhere abounded. The banks of the stream were frequently gra.s.sy, and there was a great deal of marshy ground. Most of the plants obtained were in full flower, and the colours were in general very bright, and sufficiently varied. By far the greater part belonged to the same genera which prevail on European mountains, such as _Draba_, _Saxifraga_, _Sibbaldia_, _Potentilla_, _Ranunculus_, _Papaver_, _Pedicularis_, _Cerastium_, _Leontopodium_, and _Saussurea_. The most remarkable forms were three species of _Allardia_, several _Astragali_, a one-flowered _Lychnis_, _Delphinium Brunonianum_, and a _Ligularia_. The alpine nettle was common on many parts of the road, chiefly near places frequented by the shepherds as halting-places.

Next day at starting I proceeded along the edge of the small plain close to which I had been encamped. On the right hand was an ancient moraine, which prevented me from seeing the road in advance. At the upper end of the plain I found a small streamlet running parallel to the moraine; and about a mile from camp I reached the end of a small glacier, from which the streamlet had its origin. Crossing the latter, which was still partially frozen, I ascended in a deep hollow between the left side of the glacier and the moraine. The icy ma.s.s had not yet begun to thaw, the temperature being still below freezing. After half a mile I ascended on the surface of the ice, and as soon as I did so, was enabled to see that the glacier had its origin in a ravine on the south, and entered the main valley almost opposite to me. The great body of the ice took a westerly direction, forming the glacier along which I had been travelling; but a portion formed a cliff to the eastward, which dipped abruptly into a small, apparently deep lake. At the distance of perhaps five hundred yards there was another glacier, which descended from a valley in the northern range of mountains, and, like the one on which I stood, presented a perpendicular wall to the little lake. Right and left of the lake were enormous piles of boulders, occupying the interval between its margin and the mountains, or rather filling up a portion of the s.p.a.ce which it would otherwise have occupied. Into this very singular hollow I descended, on a steep icy slope, and pa.s.sing along the northern margin of the lake, ascended on the glacier beyond; as before, between the ice and moraine.

On reaching the surface of the second glacier, I found that a similar but smaller depression lay beyond it to the east, in which also there was a small lake, with another ma.s.s of ice beyond it. This third glacier also came from the north, and was a much more formidable ma.s.s than those which had already been crossed. It was very steep, and was covered with snow, which was beginning to thaw more than was convenient. When at the highest part, I found that though apparently nearly level, it sloped downwards sensibly, though very slightly for nearly half a mile, in an easterly direction. It was evident that I had now reached the highest part of the ascent, and that the crest of the pa.s.s was covered by this glacier. I did not make any observation to determine its alt.i.tude, but the ascent from camp was very moderate, not, I think, exceeding a thousand feet. a.s.suming this estimate to be correct, the height of the pa.s.s would be about 17,600 feet, which I believe will prove not far from the truth.

On so icy an ascent vegetation could not be expected to be plentiful; still, even in the depressions between the glaciers, the crevices among the boulders produced a few plants, mostly the same as those observed the day before, but three species of _Saussurea_ were the most common of all. Before arriving at the first glacier, the beautiful _Primula_ collected on the pa.s.s above Le was met with in great abundance.

[Sidenote: Sa.s.sAR.

_August, 1848._]

For about half a mile, as I have said, the slope of the glacier was just perceptible; beyond that distance the descent was abrupt. On reaching the end of the level portion, I obtained an excellent view to the eastward, in which direction a wide valley was seen at a distance of several miles. Through this valley, from left to right, ran a considerable river, which proved to be the Shayuk. Beyond the river, rocky mountains were seen, apparently nearly as high as those near at hand, and perfectly barren. In descending from the pa.s.s, I soon left the surface of the ice, which, as soon as the slope became abrupt, was too rugged to be walked over. I then got upon the moraine; about half-way down, the glacier, which had latterly been almost entirely covered with debris, came to an end, but a moraine continued a long way down, and the remainder of the descent was very stony. I encamped at about 15,400 feet on a dry gravelly plain, close to the broad valley of the Shayuk, but at least 500 feet above it. To the right, in a very deep ravine, was a small stream, on the banks of which were patches of snow. The name of the ground on which I encamped, which is a usual halting-place, was Sa.s.sar, and the Turki merchants call the pa.s.s also by the same name.

[Sidenote: PLAIN OF SHAYUK RIVER.

_August, 1848._]

From Sa.s.sar not more than three or four miles of the upward course of the river were visible, but within that distance three glaciers were in sight. Two of these stopped short of the valley, while the third, which was at the most distant point visible, appeared to descend to the river. An enormous precipice, which must have been at least 3000 feet in height, rose on the opposite side of the valley beyond the glaciers. Downward the valley of the Shayuk was seen for nearly ten miles, as a wide gravelly plain, with high rugged mountains on both sides.

On the morning after my arrival at Sa.s.sar, it was snowing slightly at daybreak, and continued to do so till near noon. The snow melted almost immediately on the level ground, but on the mountain-sides it lay all day, down as low as the level of my tent. The afternoon was dull and stormy, but no more snow fell. This unfavourable weather was of less consequence, because I had determined to halt in order to make fresh arrangements for my baggage, being advised not to take any cattle beyond Sa.s.sar, the roads in advance being very bad. I afterwards found that they were gravelly, which is more injurious than even rock to the unprotected feet of the Tibetan bullock.

The gravelly sloping hills round my encampment were covered with abundance of vegetation, but few of the species were alpine, and almost all were familiar to me. A species of _Allium_, with purple flowers and broad strap-shaped leaves, was the most plentiful of all.

_Thermopsis_ was frequent, in fruit; other common plants were species of _Artemisia_, _Cynoglossum_, _Cicer_, and _Dracocephalum_. The only new species were a very handsome dark purple _Nepeta_, which grew in large tufts among loose shingle, and a tall _Saussurea_, by far the largest species of the genus which I had found in Tibet, but I believe one of those described from Jacquemont's collections. A species of _Rheum_ occurred occasionally on dry stony places, but it was the same which I had found several times before.

On the 15th of August I resumed my journey. The morning was misty, with a few flakes of snow at intervals, and the sky remained overcast all day, with high squalls of wind. My road lay across the Shayuk, but I found it necessary to ascend about half a mile on the high bank before I reached a place where it was possible to descend to its gravelly plain, which was more than half a mile wide, and quite dest.i.tute of any kind of vegetation. The river was running in several channels, with an average depth of about a foot and a half; in one place only it was as much as two feet. The current ran with considerable rapidity.

On the opposite side of the plain of the Shayuk, I entered an extremely narrow ravine, bounded by precipices of black slate, down which ran a small stream, which crossed at every turn of the ravine from one side to the other, generally close to the rocky wall, and had to be forded a great number of times. After a mile and a half, the road, suddenly quitting the ravine, turned to the right, and ascended by a steep pathway to a wide, very gently rising plain, bounded on both sides by snowy mountains. This plain was partly gra.s.sy, but mostly composed of hard dry clay. In a few spots where snow appeared recently to have lain, the clay was soft and treacherous, sinking under the feet. About a mile's walk over this plain brought me to the highest part of it, beyond which it began to slope to the eastward, at first very gently but afterwards more rapidly. Many large isolated boulders were observed on its surface. It was curious to observe that the gravel produced by the disintegration of the mountains (chiefly, I suppose, by snow-slips in winter) differed in colour on the two sides of the valley, and that the line of demarcation followed very closely the centre of the valley. The northern mountains, being granitic, produced a hard quartzy gravel, while those to the south, which were schistose, contributed a dark-coloured gravel of sharp slaty fragments. On the lower part of the descent, a small rivulet made its appearance in the centre of the plain, and I encamped, after nine and a half miles, close to an open valley of considerable size, whose course seemed to be south-east.

[Sidenote: MURGAI.

_August, 1848._]

This encamping-ground is called by the Turki merchants Murgai, by the Tibetans, Murgo-Chumik; the former name being probably a corruption of the latter. It was the last place at which I was to expect a sufficiency of fuel, or even, with rare exceptions, of gra.s.s for my horse, which, though not often used, I was unwilling to leave behind, lest I should by any accident be disabled from walking. The temperature of boiling water here indicated an elevation of about 15,100 feet, but as the weather was stormy and threatening, this was probably several hundred feet more than the truth. A number of springs appeared to break out of the ground close to my tent, where there was a considerable extent of boggy pasture, much greener than is usual at so great an elevation. A few bushes of _Myricaria elegans_ were the only shrubs, but tufts of _Artemisia_ and _Eurotia_ were sufficiently plentiful to produce an abundance of fuel. In the boggy meadow, a pretty little species of _Primula_ was very abundant; the other plants observed were a white _Pedicularis_, two species of _Triglochin_, and some _Carices_ and gra.s.ses.

The morning of the 16th of August was bright and beautiful, the clouds having been entirely dissipated during the night. The wide valley near which I was encamped descended, as I was informed, to the Shayuk, which it was said to join through a rocky gorge eight or ten miles lower down than Sa.s.sar. Along its course the merchants are in the habit of ascending at the season when the valley of the Shayuk is followed all the way from Nubra, which is only practicable in early spring and late in the autumn, at which times that river is fordable throughout. It is a fortunate circ.u.mstance for the trade that there is thus a choice of routes, for at these seasons the Sa.s.sar pa.s.s must be in a great measure blocked up with snow.

[Sidenote: ASCENT OF MURGAI VALLEY.

_August, 1848._]

On my arrival at Murgai, I had observed that the mountains to the north were very precipitous, and had been puzzled to decide what direction the road might take. On starting, however, I found that it lay along the upward course of the stream which watered the valley before me, and which here issued from the mountains through a very narrow ravine with high precipices on both sides. At first I ascended to the top of a platform of conglomerate which lay at the base of the mountains. The ground was strewed with fragments of limestone, evidently derived from the mountains above; and about half a mile from camp I pa.s.sed a calcareous spring which had deposited large quant.i.ties of tufa throughout the whole of the s.p.a.ce between its source and the face of the precipice which overhung the river: the thickness of the incrustation was, in front of the cliff, from six to eight feet. A little further on, the road descended abruptly to the stream, and, after crossing it several times within a few hundred yards, ascended equally abruptly the steep stony slopes on its left bank, at a point where its course, which had previously been nearly north, turned rather suddenly to the eastward. On emerging from the ravine, two small glaciers came in sight almost directly opposite, in branches of a narrow and very deep gorge, which descended from the mountains to the north nearly in the original direction of the ravine. The road ascended to the height of at least 1000 feet, and then proceeded along the steep slopes, alternately ascending and descending over very stony ground, occasionally covered with loose limestone shingle. The stream was visible below, running through a narrow rocky fissure.

After about a mile and a half, the road again descended to the river, now a little wider, with a gravelly channel. Here I found that there were two roads. One of these, for loaded animals, ascended steeply on the north side, to the height of nearly 1000 feet, and again descended very abruptly. The other was in the bed of the stream, which was partially filled up with huge blocks of rock. The stream being almost dry, I took the lower road, which for pedestrians was only objectionable from its great roughness, and because it was necessary to cross the rivulet occasionally. After about a quarter of a mile, the ravine suddenly opened out into a gravelly plain nearly half a mile in width, traversed by numerous branches of the little stream: these were now almost dry, owing to the cloudy weather of the last few days having in a great measure stopped the melting of the glaciers by which they were supplied. Along this open plain I continued for nearly five miles. In one place only it contracted again for a few hundred yards into a gorge full of huge rocky ma.s.ses heaped one on another, by which it was apparently quite blocked up; this however was avoided by a slight ascent among angular limestone fragments. On descending into the plain again, I observed a very small patch of gra.s.sy ground on a bank a few feet above the level of the stream, the only herbage seen during the day. About a mile further on I encamped, after a march of nine miles, on the south side of the plain, on a dry bank elevated four or five feet above its gravelly bed. There was a sudden change in the direction of the valley just at my encamping-ground, its further course being in a direction west of north. The elevation of my tent was very nearly 16,000 feet.

High, rugged, precipitous mountains, with snowy tops, rose on both sides of the road during the whole of this day's journey. The rock throughout the day was limestone, a few thin layers of slate excepted.

It varied much in colour, but was generally very dark and highly crystalline, and often contained large ma.s.ses of white calcareous spar. It was distinctly stratified, and occasionally exhibited obscure traces of what might be fossils, but which were too indistinct to be relied upon. The princ.i.p.al ma.s.s of snow seen was nearly due south of my encampment, but this was probably owing to the northerly exposure of the mountains on that side. The vegetation observed during the day was scanty in the extreme; _Eurotia_, a _Saussurea_ with very viscid leaves, _Oxytropis chiliophylla_, and _Biebersteinia odora_ being almost the only plants on the stony slopes and shingle during the first half of the way. On the gravelly plain there was no vegetation at all, but on its margins a few scattered plants were occasionally to be found, a _Pyrethrum_ and two or three _Cruciferae_ being the species noted. The most remarkable plant observed during the day was a species of _Alsine_ in dense hemispherical tufts, a foot or more in diameter. This plant (the moss of Moorcroft's visit to Garu, and of other travellers in and on the borders of Tibet) is a common Tibetan plant at very great elevations, 16,000 feet being perhaps not far from its lowest level[25].

On the 17th my road lay entirely along the gravelly plain in a direction always considerably to the west of north. The plain gradually narrowed as I advanced, and came to an end by contracting into a rocky ravine, just as I halted for the day. The mountains on the left were still very lofty; one glacier was seen on that side. On the right the mountains were lower and quite without snow, but extremely rugged and rocky. The slope of the valley was scarcely perceptible, but I found at the end of my day's journey, which amounted to twelve miles, that I had risen above 700 feet, the height of my encampment being a little more than 16,700 feet. The day was bright and sunny, and the stream, which, in the morning was quite insignificant, not three feet wide and scarcely ankle-deep, had increased much by the afternoon, and had become of a dirty red colour.

It was twenty feet wide, and a foot and a half deep, where I crossed it just before halting. The vegetation was still more scanty than the day before, though most of the plants then noted were again seen occasionally. Small tufts of a little _Stipa_ were not uncommon, const.i.tuting almost the only food for cattle, as patches of green gra.s.s, a few feet in diameter, were only seen twice during the day.

Two very small _Saussureae_ formed dense tufted ma.s.ses on the surface of the ground, and a little rose-coloured _Astragalus_ spread itself prostrate over the gravel; indeed, this mode of growth seemed to be characteristic either of the climate or soil, as I found, though rarely, a species of _Myricaria_, with short thick wiry branches lying flat on the ground and spreading into patches a yard in diameter.

[Sidenote: REMARKABLE LIMESTONE.

_August, 1848._]

Not far from the point where the direction of the valley changed so suddenly, the blue or greyish ma.s.sive but brittle limestone of the higher mountains gave place to a rock of a very different appearance.

This was also a limestone, perfectly white, or with a very faint yellowish or greyish tinge, and either quite amorphous, with a saccharine texture, and often honeycombed, or composed of a congeries of very minute crystals. Occasionally, but rarely, rolled pebbles were seen in it. No traces of stratification were anywhere discoverable, in which respect it differed very strikingly from the limestone of the previous day, in which lines of stratification, much contorted, were well seen in many sections exposed at different heights. This remarkable limestone formed the rock on both sides of the gravelly plain during the greater part of the day's journey. In one place only metamorphic slate was seen below it, dipping at a high angle to the north-east. The limestone was extremely brittle, and the cliffs terminated above in sharp pinnacles of the most fantastic shapes, while at the base they were covered with heaps of angular debris[26]. A coa.r.s.e conglomerate replaced the limestone during the last mile previous to my encamping.

[Sidenote: ELEVATED PLAIN OF KARAKORAM.

_August, 1848._]

On the 18th of August, after following for a few hundred yards the course of the stream through a narrow rocky gorge, the road turned abruptly to the right, up a dry stony ravine, ascending rather rapidly. The coa.r.s.e conglomerate of the lower part of this ravine was succeeded by a coa.r.s.e sandstone, and that again by an incoherent alluvial conglomerate with a clayey matrix. After a short distance, the ravine widened out into a narrow, gravelly, moderately steep valley, with low rounded hills on either side. By degrees, as I increased my elevation, superb snowy mountains came in sight to the south-west, and on attaining the top of the ascent an open, gravelly, somewhat undulating plain lay before me, while behind a grand snowy range was seen in perfection, forming apparently a continuous chain, with a direction from south-east to north-west. The snow was to the eye perfectly continuous in both directions as far as the mountains were visible, and appeared everywhere to lie on the mountain-sides to three and four thousand feet below their tops. As I had pa.s.sed through this apparent chain of mountains without rising above 16,000 feet, the continuity of the snowy ma.s.s was of course a deception. Many very lofty peaks rose above the others at intervals. The height of the more distant ones I could not venture to estimate, but I felt at the time fully convinced that a very high peak, just opposite to me, and distant, according to bearings taken afterwards, about ten miles (in a direct line) from the edge of the plain, was 6000 or 7000 feet higher than the ground on which I stood, or at least 24,000 feet above the level of the sea. I do not wish that any great degree of confidence should be placed on this estimate, but I think it right that I should state my impression at the time, formed without any wish to exaggerate.

The stream along which I had ascended during the two last days lay in a deep ravine far below the level of the plain. Its source was evidently not far distant, and it issued no doubt from a large glacier at the head of the gorge, though the slight upward slope of the plain to the west prevented me from seeing its precise origin. In a northerly direction the plain appeared to extend for six or seven miles, and beyond it lay several ranges of mountains running from east to west, but only very moderately patched with snow. Eastward the plain diminished slightly in elevation for four or five miles, at which distance there was a low range of hills, and immediately at their foot a small stream apparently running to the northward. Beyond these low hills were a number of lofty black peaks to the northward of the great ma.s.s of snow, on the further side of which the country probably dips to the eastward in the direction of Khoten. Every one of my guides positively denied the existence of any road in that direction; afraid, perhaps, that I might attempt to proceed by it; for I learned afterwards, on my return to Le, from a merchant of Yarkand, that there was an unfrequented path by which Khoten might be reached, if the Chinese authorities were willing to permit it to be used.