24th.—We left the cantonment about 11 A.M., and proceeded down the Burrampooter, which is a very uninteresting river, and appears more like a net-work of water and sand banks; opposite Jumalpore, the banks are about a mile apart, but the distance between the extreme banks, leaving the island opposite the cantonment out of the question, is much more. During the dry weather this part of the river is passable, and indeed is in some places nothing but a dry bed of sand, so that people walk across it. During our stay at the above place we met with many interesting and new plants, among which a new species of Villarsia occupied the most prominent place. Cyperaceæ, Gramineæ, and aquatic Scrophularineæ abound. Solanum spirale occurs in abundance, and the trees commence to be clothed with ferns. I observed only one Epiphytica Orchidea, probably an Aerides.
The banks consist hitherto of nothing but sand, covered with Saccharum spontaneum. Andropogon muricatus is scarcely to be met with.
26th.—We left Mymensing this morning, and proceeded down the Burrampooter, the banks of which still present for the most part nothing but a succession of sandy banks covered with Saccharum spontaneum. The stream is not very rapid, and the river, owing to the numerous islands and banks, does not present so imposing an appearance as the Ganges. For the last week strong easterly winds have prevailed.
27th.—We entered the mouth of the Soormah, or, as the natives seem to call it, the Barak. The water of this river or portion of the Megna? is remarkably clear, compared with that of the Ganges; as indeed is that of the Burrampooter.
30th.—Some time after we entered the Soormah we apparently left its channel, and up to this morning we have passed through a tract of jheels with a few clear and very deep channels. The villages are built on small eminences, and are entirely surrounded with water; they have the usual form, and those houses adjoining the water have fences of an Arundo, which they tell us are intended to keep out the grass. We have since entering these jheels passed through and between immense beds of vegetation, formed principally of Oplismenus (Panicum) stagninus, Leersia? aristata, which by-the-bye is a distinct genus. Villarsia cristata, Nymphæalotus, Potamogeton, Azolla Salvinii, etc. etc. The only novel things we have met with are Ischæmum cuspidatum, Roxb. (sui generis,) and a small grass intermediate between Panicum and Chamæraphis. The wild form of Oryza sativa, Panicum interruptum and Leersia? ciliaris, Roxb. also occur; the two former in abundance. On the more dry tracts, that occasionally though very rarely occur, Andropogon muricatus appears. No Saccharum presented itself since the 28th. High ground was visible yesterday evening, apparently at a great distance.
October 1st.—We have continued to pass through immense jheels: about 6 A.M. we arrived at Hubbe-gunge, a large native town, situated on the Barak, which does not deserve the name of a river. The actual distance from this place to Chattuc is about 42 miles, and the high land in that direction was faintly visible for about 2 hours in the morning. The ground to the Eastward is losing the “Jheel” character, and appears densely wooded, and to the S.E. rather high hills are visible. Altogether this land of jheels is very remarkable, particularly on account of the great depth of the water, which except in one point has hitherto always exceeded 6 feet, and yet the water has fallen in all probability two or three more. As the head quarters of tropical aquatic plants, it is well worthy of attention; the profusion of Leersia aristata, Roxb. is immense, but this is almost exceeded by Oplismenus stagninus.
On the 3rd October, we left the tract of jheels, and proceeded by small rivers, overhung with jungle and fine bamboos; on the 5th we re-entered the Soorma and proceeded down it to Chattuc, which is situated on the left bank of the river, and which we reached in the afternoon. During our passage down the river we had beautiful views of the mountains, which do not however strike one with an idea of great height. We could plainly distinguish two or three waterfalls shooting over scarped precipices.
Churra Punjee, October 30th.—After a residence of 20 days here, I wrote to Mr. Solly, stating nothing particular, except that Bucklandia has coniferous tissue, and that Podostemon will probably prove Monocotyledonous and allied to Pistiaceæ. Our stay here has proved a source of great delight, and accumulation of botanical and geological treasures. The cantonments of Churra are at an elevation of 4200 feet above the sea, the native village being situated half way up the ascent which closes in the table-land on which the cantonment is situated towards the N. and W., and it is hence about 300 feet higher. The country immediately adjoining the cantonment is flat, with here and there a rounded hillock, destitute of any covering but grasses and a few low, half shrubby plants. To the Eastward there is a very deep and beautiful valley, the west side of which in particular is densely covered with jungle, but this does not contain any large trees. The opposite side, fronting our bungalow, runs nearly N. and S., presents a succession of ravines, and a most picturesque and varied surface. This valley, along the bottom of which as is usual a torrent runs, opens into the low country at Terrya Ghat, which is situated at the foot of the ascent to Churra. Directly to the south, and at a distance of about two miles from the cantonments, there is another valley likewise occupied below by a torrent fed by the Moosmai falls. The commencement of all these valleys, that I have at least seen, is a sheer precipice, which often, and particularly at Moosmai, assumes the form of a vast amphitheatre, over the brink of which cascades, especially at Moosmai, fall in tolerable plenty. It is in these places that the immense depth of the sandstone is best seen; the depth of the valley of Moosmai is, I am told, 1500 feet, the country above these precipices is generally level, and is in fact table-land. The most beautiful valley is at Maamloo, a village to the Westward of Churra, and about five miles distant. The approach to Churra is pretty enough, and gives the best view of the cantonment. The coal mines are to the Westward, and close to Churra. These I have not yet seen; the coal is of the very best description, it does not splinter, gives remarkably few ashes, affords an admirable fire and the best coke. Water-courses are plenty about Churra, but the body of water is at this season small, although it becomes considerable after a few hours rain; it is then that the great fall at Moosmai becomes really beautiful, the water shooting over the precipice and falling into a bason about 150 feet below. By a succession of these falls, although of more limited height, it at length reaches the bottom of the valley. It is only on the precipices about the fall that the Chamærops appears to grow; at the foot of a precipice a little to the right (going from Churra,) a tree fern grows, which I have Wallich’s authority for stating to be Polypod giganteum, a fern which occurred at Mahadeb, and which I have seen in somewhat similar situations at Mergui. All my excursions have been confined to this valley and to the water-courses immediately around Churra; once only have I quitted the table-land and proceeded to Maamloo, and yet in this very limited space the profusion of objects has been such as to enable me only to embrace a very limited proportion. The above excursion proved very rich. About half way to Maamloo I discovered a solitary tree fern (Alsophila Brunoniana,) and to the left, and up the broken sides of the calcareous cliffs that occur here and between Maamloo and Moosmai, a group of several magnificent specimens, of which on the succeeding day we brought home three. We saw none above 30 feet, although the specimen in the British Museum from these hills measures 45. Their axis is of small diameter, and is nearly cylindrical, the vascular fascicles being disposed in covered bundles, often assuming the form of a UU near the circumference of the very dense cellular tissue of which the axis is chiefly composed. Towards the base it is enveloped in an oblique dense mass of intermottled rigid fibres (roots) which, as they are developed in the greatest extent, the nearer they approach the base, give the trunk a conical form. Their growth is essentially endogenous, and will probably be found when examined aborigine to approximate to that of Cycadeæ, although these last are of a more exogenous than endogenous nature. Nothing however is known of the growth of Palms, Cycadeæ, or tree ferns. I have above alluded to the calcareous rocks or cliffs; these are of the same formation with those that occur so abundantly on the Tenasserim coast, although they are much more rich in vegetation. These I first saw at Terrya Ghat; like those of Burmah they abound in caves, and assume the most varied and picturesque forms; they appear to be the head quarters of Cyrthandraceæ, of which we found a noble species with the flower of a Martynia growing among the tree-ferns. They are very rich in ferns and mosses, of which last near the tree-ferns I gathered four species of four genera without moving a foot. The cliffs in which, or at the foot of which the coal is found, bound the Churra cantonments to the Westward. These are chiefly calcareous. The entrance to Churra lies between this and the precipice at Moosmai. Very few animals of any description are to be seen about Churra. I have seen one small species of deer, about half as large again as the mouse-deer of Mergui, and one young flying squirrel of a greyish black colour, with a very bushy tail. Leopards are, they say, not uncommon. Tigers do not generally come so high. Of birds, I mean about Churra, there are several species of hawks, and their old companions crows and swallows; but I have seen no sparrows, which is singular enough. There is one beautiful species of jay, with crimson-orange beak and legs, and a pretty king-fisher; but, except perhaps in the valleys, birds, I should say, are very scarce. With respect to shooting, scarcely any is to be had; wood-cocks are found in the dells about Churra, but sparingly. I have seen only one snipe and one quail.
Regarding the natives, I have little to say. They are a stout-built, squat, big-legged hill tribe: the women in regard to shape being exactly like their mates; and as these are decidedly ugly—somewhat tartarish-looking people, very dirty, and chew pawn to profusion—they can scarcely be said to form a worthy portion of the gentler sex. They appear to be honest; but that is a quality which, from the example of their European lords, they are said to be losing fast. They have no written character; every thing being transmitted by tradition, and performed by the interchange of tokens. They drink like fish, and manufacture a bad kind of arrack, the pernicious effects of which were experienced by the European invalids when the Sanatarium was in existence. They pay respect to their dead by the erection of a sort of kairns and large erect slabs of sandstone rounded off at the upper end: of these, I believe, they put up three or five to each friend, according to their means and, probably, rank. The Churra people cultivate nothing but a little cotton, and perhaps a species of Eleasine. They depend upon the plains for their support and supplies, and this is good management since rice at Terrya Ghat is sold at 70 or 80 seers a rupee. Their hire is, considering the cheapness of their food, very expensive; a man being rated at four annas a day, a woman at three, and a boy at two. I should add, that they have no caste.
The climate is certainly very cool and cold, the thermometer ranging from about 56° to 66° in-doors at this time of the year. The rains are said to be the coldest part of the year; they are excessive, commencing in April and ceasing in October. It occasionally rains for fifteen or sixteen days in succession, and without intermission; and nine or ten inches have been known to fall in twenty-four hours. Since we have been here, inclusive of this, we have had four days of wet weather, of which three were continued rain. Both were ushered in by the sudden irruption of heavy mists from below, which soon spread over the country, obscuring every thing. These sudden irruptions occur during the partial breaking up of the rain, during which time the valleys are completely choked up with dense mists, the summits of the hills on the opposite side to that on which one stands being alone visible. After the rains were over, in the first instance, the plains, or rather the mass of haze hanging over them, presented a most curious spectacle.