قراءة كتاب James's Account of S. H. Long's Expedition, 1819-1820, part 3

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James's Account of S. H. Long's Expedition, 1819-1820, part 3

James's Account of S. H. Long's Expedition, 1819-1820, part 3

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دار النشر: Project Gutenberg
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these became less frequent, and at length ceased entirely. Few cryptogamous plants are seen about any part of the mountain; and neither these nor any others occur frequently on the top of the peak. There is an area of ten or fifteen acres forming the summit, which is nearly level; and on this part scarce a lichen was to be seen. It is covered to a great depth with large splintery fragments of a rock entirely similar to that found at the base of the peak, except perhaps a little more compact in its structure. By removing a few of these fragments, they were found to rest upon a bed of ice, which is of great thickness, and may, perhaps, be as permanent as the rocks with which it occurs.

It was about 4 o'clock P. M. when the party arrived on the summit. In our way we had attempted to cross a large field of snow, which occupied a deep ravine, extending down about half a mile from the top, on the south-eastern side of the peak. This was, however, found impassable, being covered with a thin ice, not sufficiently strong to bear the weight of a man. We had not been long on the summit when we were rejoined by the man who had separated from us, near the outskirts of the timber. He had turned aside and lain down to rest, and afterwards pursued his journey by a different route.

From the summit of the peak, the view towards the north-west and south-west is diversified with innumerable mountains, all white with snow; and on some of the more distant it appears to extend down to their bases. Immediately under our feet, on the west, lay the narrow valley of the Arkansa, which we could trace running towards the north-west, probably more than sixty miles.

On the north side of the peak was an immense [220] mass of snow and ice. The ravine in which it lay terminated in a woodless and apparently fertile valley, lying west of the first great ridge, and extending far towards the north. This valley must undoubtedly contain a considerable branch of the Platte. In a part of it, distant probably thirty miles, the smoke of a large fire was distinctly seen, supposed to indicate the encampment of a party of Indians.5

To the east lay the great plain, rising as it receded, until in the distant horizon it appeared to mingle with the sky. A little want of transparency in the atmosphere, added to the great elevation from which we saw the plain, prevented our distinguishing the small inequalities of the surface. The Arkansa, with several of its tributaries, and some of the branches of the Platte, could be distinctly traced as on a map, by the line of timber along their courses.

On the south the mountain is continued, having another summit, (supposed to be that ascended by Captain Pike,) at the distance of eight or ten miles. This, however, falls much below the high peak in point of elevation, being wooded quite to its top. Between the two lies a small lake, apparently a mile long, and half a mile wide, discharging eastward into the Boiling-spring creek. A few miles farther towards the south, the range containing these two peaks terminates abruptly.6

The weather was calm and clear while the detachment remained on the peak; but we were surprised to observe the air in every direction filled with such clouds of grasshoppers, as partially to obscure the day. They had been seen in vast numbers about [221] all the higher parts of the mountain, and many had fallen upon the snow and perished. It is, perhaps, difficult to assign the cause which induces these insects to ascend to those highly elevated regions of the atmosphere. Possibly they may have undertaken migrations to some remote district; but there appears not the least uniformity in the direction of their movements.7 They extended upwards from the summit of the mountain to the utmost limit of vision; and as the sun shown brightly, they could be seen by the glittering of their wings, at a very considerable distance.

About all the woodless parts of the mountain, and particularly on the summit, numerous tracks were seen, resembling those of the common deer, but most probably have been those of the animal called the big horn. The skulls and horns of these animals we had repeatedly seen near the licks and saline springs at the foot of the mountain, but they are known to resort principally about the most elevated and inaccessible places.

The party remained on the summit only about half an hour; in this time the mercury fell to 42°, the thermometer hanging against the side of a rock, which in all the early part of the day had been exposed to the direct rays of the sun. At the encampment of the main body in the plains, a corresponding thermometer stood in the middle of the day at 96°, and did not fall below 80° until a late hour in the evening.

Great uniformity was observed in the character of the rock about all the upper part of the mountain. [222] It is a compact, indestructible aggregate of quartz and felspar, with a little hornblende, in very small particles. Its fracture is fine, granular, or even; and the rock exhibits a tendency to divide when broken into long, somewhat splintery fragments. It is of a yellowish brown colour, which does not perceptibly change by long exposure to the air. It is undoubtedly owing to the close texture and the impenetrable firmness of this rock that so few lichens are found upon it. For the same reason it is little subject to disintegration by the action of frost. It is not improbable that the splintery fragments, which occur in such quantities on all the higher parts of the peak, may owe their present form to the agency of lightning. No other cause seems adequate to the production of so great an effect.

Near the summit some large detached crystals of felspar, of a pea-green colour, were collected; also large fragments of transparent, white and smoky quartz, and an aggregate of opaque white quartz, with crystals of hornblende.

At about five in the afternoon the party began to descend, and a little before sunset arrived at the commencement of the timber; but before we reached the small stream at the bottom of the first descent, we perceived we had missed our way. It was now become so dark as to render an attempt to proceed extremely hazardous; and as the only alternative, we kindled a fire, and laid ourselves down upon the first spot of level ground we could find. We had neither provisions nor blankets; and our clothing was by no means suitable for passing the night in so bleak and inhospitable a situation. We could not, however, proceed without imminent danger from precipices; and by the aid of a good fire, and no ordinary degree of fatigue, found ourselves able to sleep during a greater part of the night.

15th. At day break on the following morning, the thermometer stood at 38°. As we had few comforts to leave, we quitted our camp as soon as [223] the light was sufficient to enable us to proceed. We had travelled about three hours when we discovered a dense column of smoke rising from a deep ravine on the left hand. As we concluded this could be no other than the smoke of the encampment where we had left our blankets and provisions, we descended directly towards it. The fire had spread and burnt extensively among the leaves, dry grass, and small timber, and was now raging over an extent of several acres. This created

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