The Western United States: A Geographical ReaderFairbanks, Harold W. (Harold Wellman)
Science
The Western United States: A Geographical Reader
Fairbanks, Harold W. (Harold Wellman)
Physical geography -- West (U.S.); West (U.S)
By following the Skagit River and a tributary stream, one can go
from the bare and snowy summit of the Cascade Range down through
dense forests, and come out at last upon a magnificent delta, where
a fertile plain is slowly but steadily encroaching upon the waters
of the sound. What contrasting scenes are presented along the few
short miles of the course of the river! A trip from its source
to its mouth will be worth all the trouble it involves, although
the trail is often disagreeably wet and sometimes dangerous.
There is no grander scenery in the United States than that of the
Cascade Range; nor are there more dense forests than those found
upon its western slope. The range is hidden in almost perpetual
clouds and storms, and they are fortunate who can reach its summit
upon a pleasant day.
[Illustration: FIG. 55.--SUMMIT OF THE CASCADE RANGE, NEAR THE HEAD
OF THE SKAGIT RIVER]
The forests of fir and hemlock have gained a foothold nearly to the
summit of the range. Upon the little benches and in the protected
nooks the trees grow thriftily, and dense groves are found up to an
elevation of nearly five thousand feet; but upon the more exposed
and rocky slopes stunted trunks show the effect of a constant struggle
with the rocks and winds. Upon other slopes, too high for the trees
to grow, there are low shrubs and arctic mosses; but above all rise
precipitous crags and peaks, utterly bare except for the glaciers
nestling among them.
Under the shade of the upland forests the moss is damp and the
wood wet, so that it is difficult to make a comfortable camp or to
build a fire. But these discomforts are not worthy of consideration
in view of the inspiration which one gains by the outlook from some
commanding point upon the summit of the mountain range.
All about are jagged, splintered peaks. Upon every gentle slope
there rests, within some alcove, a glistening mass of snow and
ice. A score of these glaciers are in sight. They are supplied
in winter by the drifting snows, and yield in summer, from their
lower extremities, streams of ice-cold water. A multitude of streams
raise a gentle murmur, broken occasionally by a dull roar as some
glacier, in its slow descent, breaks upon the edge of a precipice
and its fragments fall into the canon below.
From a position upon the summit above the point where the Skagit
trail crosses the mountains may be seen a little lake, on the surface
of which remains some of last winter's ice not yet melted by the
August sun. If the climate were a little colder, the basin would
be occupied by a glacier instead of a lake. All about the lake
there are steep, rocky slopes, more or less completely covered
with low arctic plants and stunted, storm-beaten hemlocks. From
among the trees at the foot of the lake rises the roof of a miner's
log cabin, and a few hundred feet beyond a small, dark opening in
the face of a cliff shows where the miner is running a tunnel in
his search for gold.
Public-domain text, read in full here on John Shaqi.
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