The Spell of the Rockies — John Stuart Mill — John Shaqi
The Spell of the Rockies
John Stuart Mill · en
There was no snow about, and three weeks before at the same place I
had found only one small drift which was shielded and half-covered
with shelving rock. The dry Western air is insatiable and absorbs
enormous quantities of water, and, as the Indians say, "eats snow."
The snowless area about me was on a similar slope and at about the
same altitude as the snow-filled woods, so the forest is evidently an
effective check upon the ravenous winds.
Now the rain almost ceased, and I began to descend. The upper gentle
slopes were completely covered with a filmy sheet of clear water which
separated into tattered torrents and took on color. These united and
grew in size as they progressed from the top, and each was separated
from its companions by ridges that widened and gulches that deepened
as down the sides they went. The waters carried most of the eroded
material away, but here and there, where they crossed a comparatively
level stretch, small deposits of gravel were made or sandbars and
deltas formed.
Occasionally I saw miniature landslides, and, hoping for a larger one
to move, I hurried downward. Knowing that the soil is often deep at
the foot of crags on account of contributions from above, together
with the protection from erosion which the cliffs gave, I endeavored
to find such a place. While searching, I had occasion to jump from a
lower ledge on a cliff to the deposit below. The distance to the slope
and its real pitch were minimized by the mists. After shooting through
the air for at least thrice the supposed distance to the slope, I
struck heavily and loosened several rods of a landslide. I tumbled off
the back of it, but not before its rock points had made some
impressions.
I sought safety and a place of lookout on a crag, and picked bits of
granite gravel from my anatomy. Presently I heard a muffled creaking,
and looked up to see a gigantic landslide starting. At first it moved
slowly, seemed to hesitate, then slid faster, with its stone-filled
front edge here and there doubling and rolling under; finally the
entire mass broke into yawning, ragged fissures as it shot forward and
plunged over a cliff. Waiting until most of the straggling, detached
riffraff had followed, I hastened to examine the place just evacuated.
In getting down I disturbed a ground-hog from his rock point, and
found that he was in the same attitude and position I had seen him
holding just before the slide started, so that the exhibition had
merely caused him to move his eyes a little.
In the cracks and crevices of the glaciated rock-slope from which this
mass had slid, there were broken, half-decayed roots and numerous
marks which showed where other roots had held. It seems probable that
if the grove which sustained them had not been destroyed by fire, they
in turn would have anchored and held securely the portion of land
which had just slipped away.