“Captain Webb of the Bengal establishment, was at one time employed on a survey of a province of Kumaoon. On the twenty-first day of June, his camp was eleven thousand, six hundred and eighty feet above Calcutta. The surface was covered with very rich vegetation as high as the knee; there were very extensive beds of strawberries in full flower; and plenty of currant-bushes in blossom all around, in a clear spot of rich black mold soil, surrounded by a noble forest of pine, oak and rhododendron. On the twenty-second of June he reached the top of Pilgoenta-Churhaee, (or ascent,) twelve thousand, six hundred and forty-two feet above Calcutta. He was prevented from distinguishing very distant objects by a dense fog; but there was not the smallest patch of snow near him; and the surface, a fat black mold through which the rock peeped, was covered with strawberry plants, (not yet in flower,) butter-cups, dandelions, and a profusion of other flowers. The shoulders of the hill above him, about four hundred and fifty feet more elevated, were covered with the same to the top; and above five hundred feet below was a forest of pine, rhododendron and birch. There was some snow seen below in deep hollows, but it dissolves in the course of the season. These facts led Captain Webb to infer, that the inferior limit of perpetual congelation on the Himalaya mountains is beyond thirteen thousand, five hundred feet, at least, above the level of Calcutta: and that the level of the table-land of Tartary, immediately bordering on their range, is very far elevated beyond eight thousand feet, the hight at which it has been estimated.

“On the night of the sixteenth of July, we slept at Bheemkeudar, near the source of the Coonoo and Bheem streams. There is no wood near this place, even in the very bottom of the valley, and we had left even the stunted birch at a considerable distance below; but there was a profusion of flowers, ferns, thistles, &c., and luxuriant pasturage. Captain Webb’s limit of wood is at least as high as twelve thousand to twelve thousand, three hundred feet. I would, therefore, presume the site of Bheemkeudar to be considerably above that level; say thirteen thousand to thirteen thousand, three hundred feet, above the level of Calcutta. From thence we ascended at first rather gradually, and then very rapidly, till we left all luxuriant vegetation, and entered the region of stripped and scattered and partially melting snow. From calculating the distance passed, and adverting to the elevation we had attained, I would presume that this was at least fifteen hundred feet above Bheemkeudar, or from fourteen thousand, five hundred, to fifteen thousand feet above Calcutta.

“We proceeded onward, ascending very rapidly, while vegetation decreased gradually to a mere green moss, with here and there a few snow-flowers starting through it; snow fast increasing, till at length we entered on what I presume was the perennial and unmelting snow, entirely beyond the line of vegetation, where the rock was bare even of lichens: and in this we ascended, as I think, about eight hundred feet; for, though Bamsooroo Ghat may not be so far above this line, we continued ascending, even after crossing that point, and I would incline to estimate this utmost extent of ascent at two thousand feet more, or nearly seventeen thousand feet above the level of Calcutta.

“Whilst proposing to consider the point of sixteen thousand to sixteen thousand, five hundred feet, as that of inferior congelation, I must observe that there was no feeling of frost in the air, and the snow was moist, though hard, chiefly through the influence of a thick mist, which, in fact, amounted to a very small drizzling rain, which fell around: all which would seem to indicate, that the true line of congelation had not there been attained; but we were surrounded by snow which evidently never melted. To a great depth below it extended all over the hills, very little broken, while on the valleys from whence the Coonoo and Bheem streams issue, at full two thousand feet below, it lay covering them and the surrounding mountains in an unbroken mass, many hundred feet thick. Thus, though it may seem contradictory, the line of perpetual congelation, in fact seems fixable at even below the point I have ventured to indicate, and, I presume, might, on these grounds, be placed somewhere between fifteen and sixteen thousand feet above the level of Calcutta.

“The result of all the considerations that arise out of the foregoing remarks is a belief, that the loftiest peaks of the Himalaya range will be found to fall considerably short of the hight attributed to them by Mr. Colebrooke; and that their loftiest peaks do not more than range from eighteen thousand to twenty-two or twenty-three thousand feet above the level of the sea.

“Having reached the top of an ascent, we looked down upon a very deep and dark glen, called Palia Gadh, which is the outlet to the waters of one of the most terrific and gloomy valleys I have ever seen. But it would not be easy to convey by any description a just idea of the peculiarly rugged and gloomy wildness of this glen: it looks like the ruins of nature, and appears, as it is said to be, completely impracticable and impenetrable. Little is to be seen except dark rock: wood only fringes the lower parts and the waters’ edge: perhaps the spots and streaks of snow, contrasting with the general blackness of the scene, highten the appearance of desolation. No living thing is seen; no motion is visible but that of the waters; no sound is heard but their roar. Such a spot is suited to engender superstition, and here it is accordingly found in full growth. Many wild traditions are preserved, and many extravagant stories related of it.

“The glen above described, is by far the most gloomy, savage scene we have yet met with. I regret that the weather did not permit a sketch of it to be attempted. Beyond this we could see nothing in the course of the river but rocky banks. The opposite side is particularly precipitous; yet along its face a road is carried, which is frequented as much as this, and leads to villages still farther up. By the time we had reached the village, the clouds which had lowered around and sunk down on the hills, began to burst with loud thunder and heavy rain. The noise was fearfully reverberated among the hills; and during the night more than once the sound was heard of fragments from the brows of the mountains, crashing down to the depths below with a terrific din. Our quarters were good. I slept in a temple, neat, clean and secure from the weather.”

SOURCE OF THE JUMNA.

GUNGOTREE, THE SOURCE OF THE JUMNA, A BRANCH OF THE
GANGES, IN THE HIMALAYA MOUNTAINS.