Part 4 (2/2)
[Sidenote: DESCENT TOWARDS THE SUTLEJ.
_August, 1847._]
For this reason the main road or highway through Kunawar crosses to the right bank of the Sutlej, a short way above Nachar. At starting, therefore, on the morning of the 14th of August, we began to descend towards the river. For about a mile and a half the descent was very gentle, through a good deal of cultivation. There were many fruit-trees, but very little natural wood; a few horse-chesnut trees were observed, and occasionally a scattered deodar, spruce, or pine.
On the earlier part of the road the pines were _P. excelsa_, but lower down that tree gave place to _P. longifolia_. After a mile and a half, the descent became more rapid, over a rocky and bad road, which continued to the bridge, distant three miles from Nachar. On the bare, arid, and rocky hills between Nachar and the river, several very striking novelties were observed in the vegetation; but as the road had for several days been at a higher level, and generally among dense forest, it is not improbable that many of these new plants may occur on the lower parts of the hills, in the immediate vicinity of the river, further to the westward. The new species were in all about six in number, of which three--two species of _Daphne_ and an olive--were very abundant, and therefore prominent features in the appearance of the country.
[Sidenote: w.a.n.gTU BRIDGE.
_August, 1847._]
At the point where the bridge has been thrown across, the river Sutlej has an elevation, by the determination of Captain Gerard, of 5200 feet above the level of the sea. Its bed and the banks on both sides are very rocky and bare, and the width of the stream not more than seventy feet. The bridge is of that kind called by the mountaineers _sanga_, which means a wooden bridge or bridge of planks, contrasted with _jhula_, a rope-bridge. On the left bank the pier of the bridge is formed by an isolated rock, separated from the rocky banks by an ancient bed of the river, now quite dry, but worn smooth by the action of the current. This former channel is stated by Gerard to have been blocked up by a fall of rocks from above; previous to which occurrence, the isolated rock must have stood as an island in the centre of the stream. The construction of the bridge is singular, but simple, and only adapted for very little traffic. Six stout trunks of trees are laid alongside of one another on the pier, so that the end towards the river is a little higher than the other; above these are placed in succession two similar layers of trunks, each projecting several feet beyond the one below it, and the whole of these are kept in position by a substantial stone building, through which the roadway runs. A similar structure on the opposite bank narrows the distance to be spanned, at the same time that it affords support to the central portion of the bridge, which consists of two strong pine-trees fifty feet in length, placed about two feet apart, and supporting stout cross planking. The whole forms a bridge quite strong enough to support foot-pa.s.sengers or lightly laden horses, the only purpose for which it is required.
[Sidenote: WATERFALL.
_August, 1847._]
In spite of the considerable elevation which the Sutlej valley had now acquired, a number of plants of tropical character occurred in the neighbourhood of the w.a.n.gtu bridge. These were mostly common gra.s.ses and _Cyperaceae_, _Polycarpaea corymbosa_, _Achyranthes aspera_, and a few other species, all common mountain-plants at low elevations, which here, from the great heat caused by the lessened rain and the concentration of the sun's rays, at the bottom of a deep bare valley, surmounted on both sides by mountains 10,000 feet above its level, enjoy a congenial climate. They are, however, confined to the most exposed places, and to the lower levels only. A few rugged pine-trees are scattered on the steep rocks, both _Pinus excelsa_, which does not descend quite to the base of the hills, and _Pinus longifolia_, which has here reached nearly its eastern limits, the elevation of the river-bed soon becoming greater than that at which it will grow. Close to the w.a.n.gtu bridge, on the right bank, a considerable stream joins the Sutlej from the north, and is crossed by the road not far from its junction with the great river. The lower part of this tributary exhibits a succession of fine rapids and a waterfall, now much swollen by the melting of the snow; and which, notwithstanding the want of trees and consequent bareness of the accessories, formed a picture such as often greets the eye of the traveller in the alpine districts of Himalaya, but which no amount of repet.i.tion renders less grand and magnificent. Captain Gerard has, in his little 'Tour in Kunawar,'
described this torrent in strong language, which showed that he felt the beauty of the scene. For this he has been condemned by Jacquemont, who sneeringly says that he describes it ”comme si c'etait le Niagara,” an expression which induced me to turn on the spot to Gerard's book, so that I can testify to the accuracy and absence of exaggeration of his description.
After crossing this stream, the road ascends the spur which runs parallel to it, to an elevation of about 1000 feet above the Sutlej, but only to descend again to its banks, the ascent being caused by the impracticable nature of the rocky banks of the river. The spur was bare of trees, but with scattered brushwood, in which the olive and white _Daphne_, observed on the descent from Nachar, still abounded, with several other novelties, among which a _Clematis_, _Silene_, _Stellaria_, and _Selaginella_, all previously-described Kunawar species, were the most remarkable. Several of the gra.s.ses of the plains of India, such as a _Panic.u.m_ (perhaps _P. paludosum_), _Eleusine Indica_, and _Heteropogon contortus_, occurred on the hot dry pastures among the rocks, up to above 6000 feet. The rock was everywhere gneiss, but varied much in appearance and texture, and contained many granite veins.
[Sidenote: CHEGAON.
_August, 1847._]
After regaining the river, the road ran along its bank, or on low spurs not more than a few hundred feet above it, through a dry treeless tract, till about two miles from the end of the day's journey, when a long steep ascent led to Chegaon, a large village situated on a stream with steep rocky banks, the houses as usual being surrounded with fruit-trees. Here we encamped after a march of at least fourteen miles, at an elevation of 7000 feet above the level of the sea, or nearly 1800 feet above the valley of the Sutlej.
[Sidenote: GERARD'S PINE.
_August, 1847._]
Next day our journey was a short one, not more than five and a half miles, to the village of Miru. It began by a rapid ascent for two miles to the crest of the ridge, advancing all the time towards the Sutlej, which wound round the base of the steep spur 2000 feet below.
The ascent was bare (as the slopes facing the west generally are), and the hill-side almost precipitous; but as soon as the crest of the ridge, at an elevation of about 8000 feet, had been gained, scattered trees appeared of a species not previously seen. This was _P.
Gerardiana_, the pine of Kunawar and the other dry regions of the Western Himalaya, from the back parts of Garhwal (where it has been seen by Dr. Jameson) to the valleys of the Upper Chenab. The first trees met with were small, and in appearance quite distinct from _P.
longifolia_ and _excelsa_, being more compact, with much shorter leaves and a very peculiar bark, falling off in large patches, so as to leave the trunk nearly smooth.
[Sidenote: MIRU.
_August, 1847._]
Beyond the crest of the ridge, from which the view into the Sutlej valley, and towards the mountains across the river, was superb, the road on the east slope again receded from the river, entering an oak-wood, through which it continued nearly level for more than a mile, but soon began to descend slightly towards the stream, which ran at the bottom of a deep ravine, down to which the road plunged abruptly, to ascend again as steeply on the other side; after which a steep ascent of upwards of a mile led to Miru, a large village in which we encamped, at an elevation of 8500 feet.
At this delightful elevation, in a climate where the periodical rains of the Himalaya are scarcely felt, embosomed in extensive orchards of luxuriant fruit-trees, and facing the south, so that it has the full benefit of the sun's rays to mature its grain-crops, Miru is one of the most delightful villages of Kunawar, being rivalled only by Rogi and Chini, beyond which the climate becomes too arid for beauty. The crops at Miru, both of grain and fruit, were most luxuriant, and the vine thrives to perfection. The princ.i.p.al vineyards, however, are lower down, at elevations of between 6000 and 7000 feet, at which level the sun has more power in autumn to ripen the grape.
The scenery around Miru is indescribably beautiful, as it almost overhangs the Sutlej 3000 feet below, while beyond the river the mountain-slopes are densely wooded, yet often rocky and with every variation of form. A single peak, still streaked with snow, but too steep for much to lie, rises almost due opposite; behind which the summits of the chain south of the Sutlej rise to an elevation of upwards of 18,000 feet.
At Miru we found that we had completely left the rainy region of the mountains, and henceforward the weather continued beautiful. The change had been very gradual. At Serahan we had heavy rain; a rainy night at Tranda was succeeded by a brilliant day, till the afternoon, when it rained smartly for an hour. The next day was again fine, and at Miru, though the afternoon was cloudy, and a heavy storm was visible among the mountains across the Sutlej, only a few drops of rain fell. The transition from a rainy to a dry climate had thus been apparently very sudden, four days having brought us from Serahan, where the periodical rains were falling heavily, to a place at which there were only light showers. This was in part, of course, accident.
Fine weather may, perhaps, have set-in in the interval in all parts of the mountains. In very rainy seasons, when the rain-fall in the outer Himalaya is considerably above the mean, heavy showers extend into Kunawar, at least as far as Chini; and careful meteorological observations would probably show that the transition of climate is a very gradual one, the snowy mountains and the great spurs which run towards the Sutlej collecting and condensing, as they increase in elevation, more and more of the moisture which is brought by the south-east winds from the Bay of Bengal.
[Sidenote: VEGETATION OF KUNAWAR.
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