Crossing another chain, and still ascending, the explorers reached another little lake, the Kara-goll, or “Black Lake,” with its waters shining a deep emerald green. This effect, however, is not produced by any surrounding verdure, for the lake is almost encompassed by high mountains, and crags of red and yellowish granite, that rise up into the region of eternal snow. At the upper end a huge mass of basaltic rocks, of a deep grey colour, forms a fine contrast to the yellow castellated forms at their base. On the opposite side of the lake high precipices of granite are backed by grand mountain summits, white with the snows of uncounted ages. Fording the Kara-sou, or “black water”—a stream issuing from the lake—and crossing a beautiful valley, the riders entered a thickly wooded region which stretches over the lower mountain range down to the Katounaia, and arrived on the bank of the river Bitchuatoo. Thrice had they changed from summer to winter in the course of a day’s ride. Turning to the south, they ascended a steep and lofty summit, from which it was supposed the Bielouka would be visible. It proved to be a rocky height that towered above all the mountains to the west of the Katounaia, even above the loftiest crests of the Chelsoun; and vast and magnificent was the panorama which it commanded. In the foreground, a ridge of huge granite crags, tinted with mosses of almost every hue. In all directions rolled chains of snowy peaks, like the storm-tossed waves of a suddenly frozen sea; and as they rolled, they gradually ebbed, so to speak, down to the far steppes of Chinese Tartary, and were lost in a vapour-shrouded horizon. But the Bielouka was not to be seen, and Mr. Atkinson resumed his ride, keeping along the crest of the mountain for about two versts, and then striking into a little valley, watered by several lakelets. A dreary place! There were neither shrubs nor trees; and the barrenness of desolation was relieved only by a few patches of short mossy grass. Sharp edges of slate, projecting above the surface, showed that the upheaval of the strata had been effected perpendicularly. To the south rose “half a mountain” in a precipice of not less than 2500 feet above the lakes; while a similarly strange combination of cliffs faced it on the north. Between these precipices, at the head of the valley, towered what might be taken for a colossal dome; beyond which a forest of white peaks were sharply defined against the blue serene.