Western Himalaya and Tibet

hells and fragments of pottery-Ancient temple imbedded in clay-Lakes caused by subsidence-Islamabad-Shahabad-Vegetation-Vernag-Banahal Pass-Valley of Banahal-Tro

rs of a mile in length, shaded on both sides by very fine poplar-trees, runs from the eastern end of the town, parallel to this canal, as far as the hill called the Takht, at the foot of which is situated the passage by which the lake discharges its waters into the canal. The weather was very favourable, the sprin

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s of tall reeds, among which a very narrow-leaved Typha and an Arundo were the commonest plants. Three or four species of Potamogeton were abundant in the lake, just coming into flower, but most of the water-plants were only beginning to vegetate. I saw three or four flowers of a water-lily (Nymph?a alba), and

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branching from a long canal which passes down the centre, through a succession of ponds well built in masonry, and provided with artificial fountains, which are made to play on festivals and holidays. Pavilions of fine marble occupy the intersections of

s of the surrounding country, and the absolute ugliness of the swamps in the centre of the valley. Nor should it be forgotten, when we compare the accounts given by early travellers with the impressions made upon us by the present appearance of the valley, that Kashmir is no longer in the same state as it was in

nd and on foot, in order to see the country. My first halting-place was Pampur, seven miles from the town of Kashmir. After traversing the magnificent avenue of poplars, which runs north-west from the town, the road winds round the base of the Takht, the eastern face of which is only separated from the Jelam by a low swampy tract, a few hundred yards in breadth.

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es an elevated plain, quite bare of trees, and only partially cultivated, while the remainder was covered with grass. The surface of this plain was eroded by wide transverse valleys, formed by little streams which ran towards the Jelam: these were flat, and well cultiva

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eous, and partly amygdaloidal. Several gigantic Umbellifer?, already in full flower, were abundant in the lower parts of the open valley by which I ascended. One of these was Prangos pabularia, which formed dense thickets four or five feet high. From this open valley I got upon a sharp ridge, grassy below but very rocky above, along which I proceeded almost to the top; but being stopped by a precipice, I was obliged to enter a narrow rocky ravine, by asc

etation was not generally alpine, most of the plants of the middle zone extending to the very top, there were many pretty little spring flowers, which did not extend far down. A Primula, Pedicularis, Gentiana, Leontopodium, Corydalis, and Callianthemum, were all in flower. On the northern slope of the mountain, a wood of deciduous trees,

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lace of deposits much more recent than those which extend over the whole plain, and which were therefore formed when the valley was occupied by a large lake. Avantipura was formerly the site of a very large tow

d the deep recess in the mountains, and terminate below quite abruptly, without any apparent cause, in a perfectly horizontal line along the mountain-side. The mountain behind is an isolated peak, furrowed by numerous ravines, which are dry except immediately after rain. The

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ated on the banks of the Jelam, there occur beds of fine brown-coloured clay, containing in great quantity fragments of pottery, with here and there small pieces of charcoal and bone. In one place on the bank of a small ravine, which then probably carried a streamlet into the lake, I found th

. This lake contains abundance of shells, and in the neighbourhood of the town it is made the receptacle of refuse of every kind, broken pottery being particularly plentiful. In shallow places in t

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far from the river, but perhaps twenty feet above its level, and certainly far below the level to which the clay containing pottery rises on the hill-sides. One of the temples is quite in ruins, the immense blocks of which it is built being piled confusedly on one another. The beautiful colonnade (exactly like that at Martand) by which it is surrounded, is evidently

in the neighbourhood of a very dense population. Their present appearance, I think, helps to explain the nature and origin of the many lakes or marshy depressions which occur in all parts of the valley. It appears evident that at Avantipura, at some period subsequent to the building of the temples, a subsidence of the ground must have taken place during one of the many earthquakes which are well known to have convulsed the Kashmir valley. This subsidence, w

ent platforms are seemingly much too extensive to have been formed by the trifling streamlets which now run along them, without the assistance of volcanic action. The lakes, too, are deeper than the present level of the river, a circumsta

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banks like canals, while others were almost as large as the main stream, and broad and shallow, with a sandy bed and gently flowing current. Near Bijbehara, a considerable village, with many timber-built houses and a substantial bridge of deodar, the banks are beautifully wooded with shady trees. Above this village the Jelam is much smaller, often shallow, and the banks lower, though still eight or ten feet above the water, and not swampy, but either fringed with willow and mulberry trees, or bare and covered with fields of green corn, or of rape now in full flower. The bridge of Islamabad, which is the limit of navigation, is nearly a mile from the town, whi

hells, chiefly Lymn??, were seen. Further on, the appearance of the country began to change: there were still plenty of rice-fields, but they rose in steps one above another, and the water in the irrigation canals flowed rapidly over pebbly beds. Crossing another branch of the Jelam, which had a broad channel full of large boulders, but shallow and easily fordable, the road began gradually to ascend a low range of hills covered with grass and bushes where it was dry, but still laid out in rice-fields wherever water was procurable. These hills, which a

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olia and a shrubby Indigofera. I also observed Viola serpens, Thymus Serpyllum, Lactuca dissecta, and Fragaria Indica. Among the rice-fields several plains plants occurred, such as Potentilla supina, Convolvulus arvensis, Mazus rugosus, S

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ilt of marble, is large, contains many fish, and supplies a considerable stream. It is the reputed source of the Behat or Jelam, but the main branch of that river descends from the mountains a good way further to the south-west. The hills on both sides of the Shahabad valley are of limestone, the strike of which seemed to be west-south-west, or nearly in the direction of the valley. It is very

e hills were bare and grassy. In the forests of Kashmir (as was first pointed out by Dr. Falconer) we do not find the oak, Andromeda, and Rhododendron, which are so abundant at similar elevations in the outer Himalaya.

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cended below 7000 feet. Ascending rapidly on a ridge, the brushwood gave place to a fine wood of maple, horse-chesnut, cherry, hazel, and elm, all just bursting into leaf. The dip of the limestone rocks was exceedingly variable, at one time southerly, at another northerly, but the strike was, I believe, the same as the day before. The ascent continuing rapid, the shady side of the ridge was soon covered with snow; but the road kept on the sou

est did not cease on account of elevation, because on the opposite hill, which had a northern exposure, a shady wood, chiefly consisting of pines, rose to a level considerably higher than that of the pass, which was a depression in the ridge, considerably overtopped by

erfectly level plain, covered with rice-fields and scattered villages, marked by groves of trees. On the descent I followed a very steep rocky ridge. About half-way down, the amygdaloid was replaced by metamorphic slate, and for the remainder of the descent the rocks were alternations of slate, very hard conglomerate, and quartz rock. The dip of these strata was very variable, and on the face of several spurs

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cur, nor are any vines cultivated in the valley. The winter is said to be quite as severe as in Kashmir; and the elevation, so far as I could determine it by the boiling-point of water, is a little greater, the lower villages (in one of which I encamped) being about 5500 feet, while the highest fields are about 6000 feet. In the woods, Fothergilla, cherry, sycamore, and horse-chesnut were common, just as in Kashmir. The season was much further advanced than on the north side of the pass, all these trees being fully in leaf, and the horse-chesnut in flower. The greater

s about 8000 feet above the sea, which overhangs the valley of the Chenab. The bounding spurs which hem in the Banahal valley descend almost perpendicularly upon the Chenab, and dip at last very abruptly to that river. At first, large masses of snow were visible at the sources of all the lateral valleys, but lower down the elevation was not sufficient, and the hills were bare. After leaving the last village of Banahal, the bottom of the valley was for some time level and covered with fine forest, consisting chiefly of magnificent trees of Celtis, elm, and alder; the others were two s

eared, and the general appearance of the vegetation was very different from what it would have been at the same elevation further east, the plants of a hot climate being chiefly such as delight in a dry heat, and are capable of enduring a considerable amount of winter cold, provided the summer temperature be sufficiently elevated. It was evident that the te

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of the ridge by which I ascended, there was a grove of fine deodar-trees, and in the bottom of the dell a shady wood of horse-chesnut and sycamore. I had now entered a zone in which the flora was quite similar to that of Simla; Fothergilla being the only tree I observed, which is not common in that district. And it wa

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s being those of the middle zone, except the silver fir, which descended to a lower level than it usually does in the Simla hills. There was some cultivation of wheat and barley within a very short distance of the summit, which overlooked the valley of the Chenab; and as the day was fortunately clear, there was a very fine view. The ravine through which the river flowed appeared everywhere rugge

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lage of Nasmon, on which tropical vegetation made its appearance very abruptly. Pinus longifolia grew scattered along the sides of this hill, and Daphne, pomegranate, the olive of the Sutlej valley, Vitex Negundo, Colebrookea, Rottlera, Sissoo, Adhatoda Vasica, a thorny Celastrus, Acacia modesta and Lebbek, and Bauhinia variegata, made their appearance in succession, in the order in which I have named them. Most of these are the same as the shrubby forms common in the Sutlej valley at Rampur; but the Celastrus and Acacia modesta are plants of th

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ed of the river. Plane, orange, apricot, and pear trees grew in the gardens, with Melia Azedarach, and a few trees of the European cy

orned with a profusion of bushes of Nerium odorum, in full flower, and highly ornamental. The vegetation along the river exhibited the same curious contrast of tropical and temperate forms, which I have already described as characteristic of the dry valleys of the interior of the Himalaya, at elevations between two and four thousand feet; and the tropical plants were so similar to those which I observed on the Sutlej, that I need not particularize them. There was no forest in any part of the valley near the river, but a few trees of Pinus longifolia grew scatt

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mixed with Zizyphus and wild pomegranate. The young shoots and panicles of the olive were abundantly covered with a white floccose glutinous matter, the source of which I could not exactly determine; but I could see no trace of any insects by which it could have been formed, so that it was perhaps a natural exudation from the tree. Small woods of Pinus longifolia occurred at intervals, almost alone, for few plants seem to thrive under its shade. At 4000 fe

sides were richly cultivated, as far up as 6000 feet, above which elevation fine forest commenced; and the snowy top of the mountain behind, which I had seen from the pass of the 12th, was visible rising behind the f

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ere were a few trees of Pinus excelsa and Picea, but the forest was not dense. About 7000 feet, on the north-western face of a spur, there was much cultivation of wheat and barley, hardly yet in ear. Here there was a fine view in the direction of the upper valley of the Chenab, of rugged mountains, scarcely wooded on the slope exposed to view, rising behind one another, the more distant still heavily snowed. Higher up, the forest was chiefly formed of the holly-leaved oak, but the latter part of the ascent was through a dark forest of silver fir, intermixed with a few fine yews. The underwood here was chiefly Viburnum nervosum, still in flower, though its leaves were almost fully developed.

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aved oak, forming open woods, in the glades of which patches of cultivation soon occurred; I encamped at about 7000 feet, at the village of Katti. During the day the sandstone rock occurred uninterruptedly, partly, as the day before, of a reddish-brown colour, partly grey, or nearly white. On the descent large angular

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henab, the elevation of whose bed was about 3000 feet. The descent, which was almost precipitous, led down the face of a mass of clay, in some respects like the alluvial deposits so common in Tibet. Similar masses of alluvium, all table-topped, and very steep, and much worn by ravines, had occurred throughout the whole of the descent from Katti. A few pines grew on this steep bank, and

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or I had not expected to find this Kashmir tree so close to the plains, and in a district the flora of which was so completely that of the Simla hills. On the summit of the pass, which was not more than 6000 feet, I found a beautiful gentian (G. Kurroo of Royle) and a yellow spinous Astragalus, seemingly the same species whi

s became frequent, and were surrounded by extensive cultivation, and all temperate vegetation disappeared. I encamped at the village of Kirmichi, where the valley which I was following appeared to expan

stant about twenty miles. In crossing this open plain, or dhun, I nearly followed the course of a little stream which had excavated for itself a deep channel in the soft sandstone of which the plain was composed. This rock was very different in appearance from the red or grey sandstone which had accompanied us from Balota; it was pure white, and almost horizontally stratified, while that was always highly inclined. During the latter part of my journey of the 10th I no

lm occupied drier spots; and I saw a few trees of Cassia fistula. Crossing a broad shallow river which flowed to the eastward at the southern boundary of this dhun, in a depression faced by cliffs of sandstone, I entered among low hills covered with scattered trees of Pinus longifolia. Th

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d, being in the steeper parts paved with large flat stones, while in the more rocky parts the sandstone was cut into steps. A flat and well cultivated valley lay to the south of this range, in the centre of which flowed a river, in a wide channel several hundred feet below the level of the plain: it was very shallow, and was crossed by stepping-stones. Another hilly t

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plane, densely covered with a jungle of low thorny trees. The same sort of jungle usually skirts their base to a distance of two or three miles, or as far as the alluvial soil of the level country which lies beyond is covered with stones and shingle. It is principally composed of Acacia modesta and Catechu, and of two species of Zizyphus. The northern or inner face of this range of hills is very steep, often quite precipitous; and where they overhang the Tawi, they terminate abruptly in a line of cliffs facing the river. A similar range, but a good deal lower, descends from the eastw

eds dipping very gently towards the plains. The boulders of which it is composed are waterworn, and very various in composition, but all ref

ope of the different tributaries which join the Tawi from the right and left, tends to keep out of sight the longitudinal ranges parallel to that river, from which the lateral ramifications proceed. When we obtain a detailed survey of the district, it will be found that the lateral valleys on each side of the Tawi do not