James's Account of S. H. Long's Expedition, 1819-1820, part 2James, Edwin
History
James's Account of S. H. Long's Expedition, 1819-1820, part 2
James, Edwin
Indians of North America; Rocky Mountains; United States -- Discovery and exploration; West (U.S.) -- Description and travel
[129] The party mistook this "highest peak" for Pike's Peak. This
mountain, called by the French trappers _Les deux Oreilles_ (Two Ears),
is the one now known as Long's Peak, being named for Major S. H. Long,
the leader of our party. Frémont found in 1842 that this name had been
adopted by the traders, and had become familiar in the country. The
elevation of Long's Peak is 14,271 feet, exceeding that of Pike's Peak
by one hundred and twenty-four feet.—ED.
July 1st. Although the temperature indicated by the thermometer for
several days had been about 80°, in the middle of the day, the heat,
owing to the cool breezes from the mountain, had been by no means
oppressive. On the night of the 30th of June, the mercury fell to 55°,
and on the following morning the air was chilly, and a strong breeze
was felt before sunrise, from the south-east. We left our camp at a
very early hour, and travelled over a tract differing in no respect but
its greater barrenness from that passed on the preceding day. We halted
to dine at the distance of sixteen and a half miles. Many acres of this
plain had not vegetation enough to communicate {178} to the surface the
least shade of green; a few dwarfish sunflowers and grasses, which had
grown here in the early part of the summer, being now entirely withered
and brown. In stagnant pools near the river, we saw the common arrow
head, (sagittaria sagittifolia,) the alisma plantago, and the small
lemna growing together, as in similar situations in the eastern states.
A striking feature of that part of the plain country, we were now
passing, is formed by innumerable ant-heaps, rising from twelve to
eighteen inches above the common level of the surface. They occur with
some uniformity, at intervals of about twenty feet, and are all similar
in size and dimensions. They consist so entirely of small grains of
flesh-coloured felspar, that they have, all of them, an uniform reddish
aspect, and it is not without careful examination, that any other kind
of gravel can be detected in them. The entrance to the interior of each
of these little mounds is uniformly on the eastward side, and very
rarely occurs beyond the boundaries of N. E. and S. E. It is never at
the top, nor on a level with the surface of the soil, but is a little
elevated above it. It seems highly probable, that the active little
architects thus place the entrance of their edifice on the eastward
side, in order to escape the direct influence of the cold mountain
winds.
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