Anxious to avoid sleeping at the bottom of the valley, we crawled, very much fatigued, through burnt dry forest, up a very sharp ridge, so narrow that the tent sat astride on it, the ropes being fastened to the tops of small trees on either slope. The ground swarmed with black ants, which got into our tea, sugar, etc., while it was so covered with charcoal, that we were soon begrimed. Our Lepchas preferred remaining on the river-bank, whence they had to bring up water to us, in great bamboo "chungis," as they are called. The great dryness of this face is owing to its southern exposure: the opposite mountains, equally high and steep, being clothed in a rich green forest. At nine the next morning, the temperature was 78 degrees, but a fine cool easterly wind blew. Descending to the bed of the river, the temperature was 84 degrees. The difference in humidity of the two stations (with about 300 feet difference in height) was more remarkable; at the upper, the wet bulb thermometer was 67.5 degrees, and consequently the saturation point, 0.713; at the lower, the wet bulb was 68 degrees, and saturation, 0.599. The temperature of the river was, at all hours of the preceding day, and this morning, 67.5 degrees.* [At this hour, the probable temperature at Dorjiling (6000 feet above this) would be 56 degrees, with a temperature of wet bulb 55 degrees, and the atmosphere loaded with vapour. At Calcutta, again, the temperature was at the observatory 98.3 degrees, wet bulb, 81.8 degrees, and saturation=0.137. The dryness of the air, in the damper-looking and luxuriant river-bed, was owing to the heated rocks of its channel; while the humidity of the atmosphere over the drier-looking hill where we encamped, was due to the moisture of the wind then blowing.] Our course down the river was by so rugged a path, that, giddy and footsore with leaping from rock to rock, we at last attempted the jungle, but it proved utterly impervious. On turning a bend of the stream, the mountains of Bhotan suddenly presented themselves, with the Teesta flowing at their base; and we emerged at the angle formed by the junction of the Rungeet, which we had followed from the west, of the Teesta, coming from the north, and of their united streams flowing south.