The pioneer West : $b Narratives of the westward march of empire
History
The pioneer West : $b Narratives of the westward march of empire
Frontier and pioneer life -- West (U.S.)
The game, _par excellence_, of the Rocky Mountains, and that which
takes precedence in a comestible point of view, is the carnero cimmaron
of the Mexicans, the Bighorn or Mountain sheep of the Canadian hunters.
This animal, which partakes both of the nature of the deer and
goat, resembles the latter more particularly in its habits, and its
characteristic liking to lofty, inaccessible points of the mountains,
whence it seldom descends to the upland valleys excepting in very
severe weather. In size the mountain-sheep is between the domestic
animal and the common red deer of America, but more strongly made than
the latter. Its colour is a brownish dun (the hair being tipped with
a darker tinge as the animal’s age increases), with a whitish streak
on the hind-quarters, the tail being shorter than a deer’s, and tipped
with black. The horns of the male are enormous, curved backwards, and
often three feet in length with a circumference of twenty inches near
the head. The hunters assert that, in descending the precipitous sides
of the mountains, the sheep frequently leap from a height of twenty or
thirty feet, invariably alighting on their horns, and thereby saving
their bones from certain dislocation.
They are even more acute in the organs of sight and smell than the
deer; and as they love to resort to the highest and most inaccessible
spots, whence a view can readily be had of approaching danger, and
particularly as one of the band is always stationed on the most
commanding pinnacle of rock as sentinel, whilst the others are feeding,
it is no easy matter to get within rifle-shot of the cautious animals.
When alarmed they ascend still higher up the mountain: halting now and
then on some overhanging crag, and looking down at the object which
may have frightened them, they again commence their ascent, leaping
from point to point, and throwing down an avalanche of rocks and stones
as they bound up the steep sides of the mountain. They are generally
very abundant in all parts of the main chain of the Rocky Mountains,
but particularly so in the vicinity of the “Parks” and the Bayou
Salado, as well as in the range between the upper waters of the Del
Norte and Arkansa, called the “Wet Mountain” by the trappers. On the
Sierra Madre, or Cordillera of New Mexico and Chihuahua, they are also
numerous.
Public-domain text, read in full here on John Shaqi.
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