James's Account of S. H. Long's Expedition, 1819-1820, part 3James, Edwin
History
James's Account of S. H. Long's Expedition, 1819-1820, part 3
James, Edwin
Indians of North America; Rocky Mountains; United States -- Discovery and exploration; West (U.S.) -- Description and travel
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.
Public-domain text, read in full here on John Shaqi.
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