Himalayan Journals, vol 1 by J. D. Hooker (best ebook for manga .TXT) 📖

of the fissures and that of the strike, it is in the Sikkim Himalaya now wholly masked by shiftings, which accompanied subequent elevations and depressions.

 

Mr. Hopkins has mathematically demonstrated that the continued exertion of a force in raising superimposed strata would tend to produce two classes of fractures in those strata; those of the first order at right angles to the direction of the wave or ridge (or line of strike); those of the second order parallel to the strike.

Supposing the force to be withdrawn after the formation of the two fractures, the result would be a ridge, or mountain chain, with diverging fissures from the summit, crossed by concentric fissures; and the courses which the rivers would take in flowing down the ridge, would successively be at right angles and parallel to the strike of the strata. Now, in the Himalaya, a prevalent strike to the northwest has been recognised in all parts of the chain, but it is everywhere interfered with by mountains presenting every other direction of strike, and by their dip never remaining constant either in amount or direction. Consequently, as might be expected, the directions of the river channels bear no apparent relation to the general strike of the rocks.

 

We crossed the Ratong (twenty yards broad) by a cane bridge, suspended between two rocks of green chlorite, full of veins of granite. Ascending, we passed the village of Kameti on a spur, on the face of which were strewed some enormous detached blocks of white and pink stratified quartz: the rocks in situ were all chlorite schist.

 

Looking across the valley to the flank of Mainom, the disposition of the ridges and ravines on its sides was very evident; many of the latter, throughout their westerly course, from their commencement at 10,000 feet, to their debouchure in the Great Rungeet at 2000, had a bluff, cliffy, northern flank, and a sloping southern one. The dip of the surfaces is, therefore, northwest, the exposure consequently of the villages which occupy terraces on the south flanks of the lateral valleys. The Tassiding spur presented exactly the same arrangement of its ravines, and the dip of the rocks being northwest, it follows that the planes of the sloping surfaces coincide in direction (though not in amount of inclination) with that of the dip of the subjacent strata, which is anything but a usual phenomenon in Sikkim.

 

The ascent to Pemiongchi continued very steep, through woods of oaks, chesnuts, and magnolias, but no tree-fern, palms, Pothos, or plantain, which abound at this elevation on the moister outer ranges of Sikkim. The temple (elev. 7,083 feet) is large, eighty feet long, and in excellent order, built upon the lofty terminal point of the great east and west spur that divides the Kulhait from the Ratong and Rungbee rivers; and the great Changachelling temple and monastery stand on another eminence of the same ridge, two miles further west.

 

The view of the snowy range from this temple is one of the finest in Sikkim; the eye surveying at one glance the vegetation of the Tropics and the Poles. Deep in the valleys the riverbeds are but 3000 feet above the sea, and are choked with fig-trees, plantains, and palms; to these succeed laurels and magnolias, and higher up still, oaks, chesnuts, birches, etc.; there is, however, no marked line between the limits of these two last forests, which form the prevailing arboreous vegetation between 4000 and 10,000 feet, and give a lurid line to the mountains. Pine forests succeed for 2000 feet higher, when they give place to a skirting of rhododendron and berberry.

Among these appear black naked rocks, rising up in cliffs, between which are gulleys, down which the snow now (on the 1st January) descended to 12,000 feet. The mountain flanks are much more steep and rocky than those at similar heights on the outer ranges, and cataracts are very numerous, and of considerable height, though small in volume.

 

Pemiongchi is at the same elevation as Dorjiling, and the contrast between the shoulders of 8000 to 10,000 feet on Kinchinjunga, and those of equal height on Tendong and Tonglo, is very remarkable: looking at the latter mountains from Dorjiling, the observer sees no rock, waterfall, or pine, throughout their whole height; whereas the equally wooded flanks of these inner ranges are rocky, streaked with thread-like waterfalls, and bristling with silver firs.

 

This temple, the most ancient in Sikkim, is said to be 400 years old; it stands on a paved platform, and is of the same form and general character as those of Tassiding. Inside, it is most beautifully decorated, especially the beams, columns, capitals and architraves, but the designs are coarser than those of Tassiding.* [Mr. Hodgson informed me that many of the figures and emblems in this temple are those of Tantrica Boodhism, including Shiva, Devi, and other deities usually called Brahminical; Kakotak, or the snake king, a figure terminating below in a snake, is also seen; with the tiger, elephant, and curly-maned lion.] The square end of every beam in the roof is ornamented either with a lotus flower or with a Tibetan character, in endless diversity of colour and form, and the walls are completely covered with allegorical paintings of Lamas and saints expounding or in contemplation, with glories round their heads, mitred, and holding the dole and jewel.

 

Illustration—INTERIOR OF THE TEMPLE AT PEMIONGCHI.

 

The principal image is a large and hideous figure of Sakya-thoba, in a recess under a blue silk canopy, contrasting with a calm figure of the late Rajah, wearing a cap and coronet.

 

Pemiongchi was once the capital of Sikkim, and called the Sikkim Durbar: the Rajah’s residence was on a curious flat to the south of the temple, and a few hundred feet below it, where are the remains of (for this country) extensive walls and buildings. During the Nepal war, the Rajah was driven west across the Teesta, whilst the Ghorkas plundered Tassiding, Pemiongchi, Changachelling, and all the temples and convents to the east of that river. It was then that the famous history of Sikkim,* [This remarkable and beautiful manuscript was written on thick oblong sheets of Tibet paper, painted black to resist decay, and the letters were yellow and gold. The Nepalese soldiers wantonly employed the sheets to roof the sheds they erected, as a protection from the weather.] compiled by the Lamas of Pemiongchi, and kept at this temple, was destroyed, with the exception of a few sheets, with one of which Dr. Campbell and myself were each presented. We were told that the monks of Changachelling and those of this establishmont had copied what remained, and were busy compiling from oral information, etc.: whatever value the original may have possessed, however, is irretrievably lost.

A magnificent copy of the Boodhist Scriptures was destroyed at the same time; it consisted of 400 volumes, each containing several hundred sheets of Daphne paper.

 

The ground about the temple was snowed; and we descended a few hundred feet, to encamp in a most picturesque grove, among chaits and inscribed stones, with a peep of the temples above. Nightingales warbled deliciously night and morning, which rather surprised us, as the minimum thermometer fell to 27.8 degrees, and the ground next day was covered with hoar-frost; the elevation being 6,580 feet.

These birds migrate hither in October and November, lingering in the Himalayan valleys till the cold of early spring drives them further south, to the plains of India, whence they return north in March and April.

 

On the 2nd of January I parted from my friend, who was obliged to hurry to the great annual fair at Titalya. I regretted much being unable to accompany Dr. Campbell to this scene of his disinterested labours, especially as the Nawab of Moorshedabad was to be present, one of the few wealthy native princes of Bengal who still keep a court worth seeing; but I was more anxious to continue my explorations northward till the latest moment: I however accompanied him for a short distance on his way towards Dorjiling. We passed the old Durbar, called Phieungoong (“Bamboo-hill,” so named from the abundance of a small bamboo, “Phieung.”) The buildings, now in ruins, occupy a little marshy flat, hemmed in by slate rocks, and covered with brambles and Andromeda bushes. A wall, a bastion, and an arched gateway, are the only traces of fortifications; they are clothed with mosses, lichens, and ferns.

 

A steep zigzag path, descending amongst long grass and scarlet rhododendrons, leads to the Kaysing Mendong.* [Described at Chapter XII.] Here I bade adieu to Dr. Campbell, and toiled up the hill, feeling very lonely. The zest with which he had entered into all my pursuits, and the aid he had afforded me, together with the charm that always attends companionship with one who enjoys every incident of travel, had so attracted me to him that I found it difficult to recover my spirits. It is quite impossible for anyone who cannot from experience realise the solitary wandering life I had been leading for months, to appreciate the desolate feeling that follows the parting from one who has heightened every enjoyment, and taken far more than his share of every annoyance and discomfort: the few days we had spent together appeared then, and still, as months.

 

On my return to Pemiongchi I spent the remainder of the day sketching in the great temple, gossiping with the Lamas, and drinking salted and buttered tea-soup, which I had begun to like, when the butter was not rancid.

 

My route hence was to be along the south flank of Kinchinjunga, north to Jongri, which lay about four or five marches off, on the road to the long deserted pass of Kanglanamo, by which I had intended entering Sikkim from Nepal, when I found the route up the Yalloong valley impracticable. The village and ruined convents of Yoksun lay near the route, and the temples of Doobdi, Catsuperri and Molli, on the Ratong river.

 

I descended to the village of Tchonpong (alt. 4,980 feet), where I was detained a day to obtain rice, of which I required ten days’

supply for twenty-five people. On the way I passed groves of the paper-yielding Edgeworthia Gardneri: it bears round heads of fragrant, beautiful, yellow flowers, and would be a valuable acquisition to an English conservatory.

 

From Tchonpong we descended to the bed of the Rungbee (alt. 3,160

feet), an affluent of the Ratong, flowing in a deep galley with precipitous sides of mica schist full of garnets, dipping west and northwest 45 degrees: it was spanned by a bridge of two loose bamboo culms, about fifteen yards long, laid across without handrails; after wet sand had been thrown on it the barefooted coolies crossed easily enough, but I, having shoes on, required a hand to steady me.

From this point we crossed a lofty spur to the Ratong (alt. 3000

feet), where we encamped, the coolies being unable to proceed further on such very bad roads. This river descends from the snows of Kinchin, and consequently retains the low temperature 42 degrees, being fully 7 degrees colder than the Rungbee, which at an elevation of but 3000 feet appears very remarkable: it must however be observed that scarcely anywhere does the sun penetrate to the bottom of its valley.

 

We encamped on a gravelly flat, fifty feet above the river, strewn with water-worn boulders, and so densely covered with tall Artemisiae, gigantic grasses, bamboo, plantain, fern, and acacia, that we had to clear a space in the jungle, which exhaled a rank heavy smell.

 

Hoar-frost formed copiously in the night, and though above the sun’s rays were very powerful, they did not reach this spot till 7.30 a.m., the frost remaining in the shade till nearly 9 a.m.;