the john muir exhibit - writings - travels_in_alaska - chapter 1
Travels in Alaska
by John Muir
Part I
The Trip of 1879
Travels in Alaska
Chapter I
Puget Sound and British Columbia
After eleven years of study and exploration in the Sierra Nevada of California and the
mountain-ranges of the Great Basin, studying in particular their glaciers, forests, and
wild life, above all their ancient glaciers and the influence they exerted in sculpturing
the rocks over which they passed with tremendous pressure, making new landscapes, scenery,
and beauty which so mysteriously influence every human being, and to some extent all life,
I was anxious to gain some knowledge of the regions to the northward, about Puget Sound
and Alaska. With this grand object in view I left San Francisco in May, 1879, on the
steamer Dakota, without any definite plan, as with the exception of a few of the Oregon
peaks and their forests all the wild north was new to me.
To the mountaineer a sea voyage is a grand, inspiring, restful change. For forests and
plains with their flowers and fruits we have new scenery, new life of every sort; water
hills and dales in eternal visible motion for rock waves, types of permanence.
It was curious to note how suddenly the eager countenances of the passengers were
darkened as soon as the good ship passed through the Golden Gate and
began to heave on the waves of the open ocean. The crowded deck was speedily deserted on
account of seasickness. It seemed strange that nearly every one afflicted should be more
or less ashamed.
Next morning a strong wind was blowing, and the sea was gray and white, with long
breaking waves, across which the Dakota was racing half-buried in spray. Very few of the
passengers were on deck to enjoy the wild scenery. Every wave seemed to be making
enthusiastic, eager haste to the shore, with long, irised tresses streaming from its tops,
some of its outer fringes borne away in scud to refresh the wind, all the rolling,
pitching, flying water exulting in the beauty of rainbow light. Gulls and albatrosses,
strong, glad life in the midst of the stormy beauty, skimmed the waves against the wind,
seemingly without effort, oftentimes flying nearly a mile without a single wing-beat,
gracefully swaying from side to side and tracing the curves of the briny water hills with
the finest precision, now and then just grazing the highest.
And yonder, glistening amid the irised spray, is still more striking revelation of warm
life in the socalled howling waste,--a half-dozen whales, their broad backs like glaciated
bosses of granite heaving aloft in near view, spouting lustily, drawing a long breath, and
plunging down home in colossal health and comfort. A merry school of porpoises, a square
mile of them, suddenly appear, tossing themselves into the air in abounding strength and
hilarity, adding foam to the waves and making all the wilderness wilder.
One cannot but feel sympathy with and be proud of these brave neighbors, fellow citizens
in the commonwealth of the world, making a living like the rest of us. Our good ship also
seemed like a thing of life, its great iron heart beating on through calm and storm, a
truly noble spectacle. But think of the hearts of these whales, beating warm against the
sea, day and night, through dark and light, on and on for centuries; how the red blood
must rush and gurgle in and out, bucketfuls, barrelfuls at a beat!
The cloud colors of one of the four sunsets enjoyed on the voyage were remarkably pure
and rich in tone. There was a well-defined range of cumuli a few degrees above the
horizon, and a massive, dark-gray rain-cloud above it, from which depended long, bent
fringes overlapping the lower cumuli and partially veiling them; and from time to time
sunbeams poured through narrow openings and painted the exposed bosses and fringes in ripe
yellow tones, which, with the reflections on the water, made magnificent pictures. The
scenery of the ocean, however sublime in vast expanse, seems far less beautiful to us
dry-shod animals than that of the land seen only in comparatively small patches; but when
we contemplate the whole globe as one great dewdrop, striped and dotted with continents
and islands, flying through space with other stars all singing and shining together as
one, the whole universe appears as an infinite storm of beauty.
The California coast-hills and cliffs look bare and uninviting as seen
from the ship, the magnificent forests keeping well back out of sight beyond the reach of
the sea winds; those of Oregon and Washington are in some places clad with conifers nearly
down to the shore; even the little detached islets, so marked a feature to the northward,
are mostly tree-crowned. Up through the Straits of Juan de Fuca the forests, sheltered
from the ocean gales and favored with abundant rains, flourish in marvelous luxuriance on
the glacier-sculptured mountains of the Olympic Range.
We arrived in Esquimault Harbor, three miles from Victoria, on the evening of the
fourth day, and drove to the town through a magnificent forest of Douglas spruce,--with an
undergrowth in open spots of oak, madrone, hazel, dogwood, alder, spiraea, willow, and
wild rose,--and around many an upswelling moutonné rock, freshly glaciated and
furred with yellow mosses and lichens.
Victoria, the capital of British Columbia, was in 1879 a small old-fashioned English
town on the south end of Vancouver Island. It was said to contain about six thousand
inhabitants. The government buildings and some of the business blocks were noticeable, but
the attention of the traveler was more worthily attracted to the neat cottage homes found
here, embowered in the freshest and floweriest climbing roses and honeysuckles
conceivable. Californians may well be proud of their home roses loading sunny verandas,
climbing to the tops of the roofs and falling over the gables in white and red cascades.
But here, with so much bland fog and dew and gentle laving rain, a still
finer development of some of the commonest garden plants is reached. English honeysuckle
seems to have found here a most congenial home. Still more beautiful were the wild roses,
blooming in wonderful luxuriance along the woodland paths, with corollas two and three
inches wide. This rose and three species of spiraea fairly filled the air with fragrance
after showers; and how brightly then did the red dogwood berries shine amid the green
leaves beneath trees two hundred and fifty feet high.
Strange to say, all of this exuberant forest and flower vegetation was growing upon
fresh moraine material scarcely at all moved or in any way modified by post-glacial
agents. In the town gardens and orchards, peaches and apples fell upon glacier-polished
rocks, and the streets were graded in moraine gravel; and I observed scratched and grooved
rock bosses as unweathered and telling as those of the High Sierra of California eight
thousand feet or more above sea-level. The Victoria Harbor is plainly glacial in origin,
eroded from the solid; and the rock islets that rise here and there in it are unchanged to
any appreciable extent by all the waves that have broken over them since first they came
to light toward the close of the glacial period. The shores also of the harbor are
strikingly grooved and scratched and in every way as glacial in all their characteristics
as those of new-born glacial lakes. That the domain of the sea is being slowly extended
over the land by incessant wave-action is well known; but in this freshly
glaciated region the shores have been so short a time exposed to wave-action that they are
scarcely at all wasted. The extension of the sea affected by its own action in
post-glacial times is probably less than the millionth part of that affected by glacial
action during the last glacier period. The direction of the flow of the ice-sheet to which
all the main features of this wonderful region are due was in general southward.
From this quiet little English town I made many short excursions--up the coast to
Nanaimo, to Burrard Inlet, now the terminus of the Canadian Pacific Railroad, to Puget
Sound, up Fraser River to New Westminster and Yale at the head of navigation, charmed
everywhere with the wild, new-born scenery. The most interesting of these and the most
difficult to leave was the Puget Sound region, famous the world over for the wonderful
forests of gigantic trees about its shores. It is an arm and many-fingered hand of the
sea, reaching southward from the Straits of Juan de Fuca about a hundred miles into the
heart of one of the noblest coniferous forests on the face of the globe. All its scenery
is wonderful--broad river-like reaches sweeping in beautiful curves around bays and capes
and jutting promontories, opening here and there into smooth, blue, lake-like expanses
dotted with islands and feathered with tall, spiry evergreens, their beauty doubled on the
bright mirror-water.
Sailing from Victoria, the Olympic Mountains are seen right ahead, rising in bold
relief against the sky, with jagged crests and peaks from six to eight
thousand feet high,--small residual glaciers and ragged snow-fields beneath them in wide
amphitheatres opening down through the forest-filled valleys. These valleys mark the
courses of the Olympic glaciers at the period of their greatest extension, when they
poured their tribute into that portion of the great northern ice-sheet that overswept
Vancouver Island and filled the strait between it and the mainland.
On the way up to Olympia, then a hopeful little town situated at the end of one of the
longest fingers of the Sound, one is often reminded of Lake Tahoe, the scenery of the
widest expanses is so lake-like in the clearness and stillness of the water and the
luxuriance of the surrounding forests. Doubling cape after cape, passing uncounted
islands, new combinations break on the view in endless variety, sufficient to satisfy the
lover of wild beauty through a whole life. When the clouds come down, blotting out
everything, one feels as if at sea; again lifting a little, some islet may be seen
standing alone with the tops of its trees dipping out of sight in gray misty fringes; then
the ranks of spruce and cedar bounding the water's edge come to view; and when at length
the whole sky is clear the colossal cone of Mt. Rainier may be seen in spotless white,
looking down over the dark woods from a distance of fifty or sixty miles, but so high and
massive and so sharply outlined, it seems to be just back of a strip of woods only a few
miles wide.
Mt. Rainier, or Tahoma (the Indian name), is the noblest of the volcanic cones
extending from Lassen Butte and Mt. Shasta along the Cascade Range to
Mt. Baker. One of the most telling views of it hereabouts is obtained near Tacoma. From a
bluff back of the town it was revealed in all its glory, laden with glaciers and snow down
to the forested foothills around its finely curved base. Up to this time (1879) it had
been ascended but once. From observations made on the summit with a single aneroid
barometer, it was estimated to be about 14,500 feet high. Mt. Baker, to the northward, is
about 10,700 feet high, a noble mountain. So also are Mt. Adams, Mt. St. Helens, and Mt.
Hood. The latter, overlooking the town of Portland, is perhaps the best known. Rainier,
about the same height as Shasta, surpasses them all in massive icy grandeur,--the most
majestic solitary mountain I had ever yet beheld. How eagerly I gazed and longed to climb
it and study its history only the mountaineer may know, but I was compelled to turn away
and bide my time.
The species forming the bulk of the woods here is the Douglas spruce (Pseudotsuga
douglasii), one of the greatest of the western giants. A specimen that I measured near
Olympia was about three hundred feet in height and twelve feet in diameter four feet above
the ground. It is a widely distributed tree, extending northward through British Columbia,
southward through Oregon and California, and eastward to the Rocky Mountains. The timber
is used for shipbuilding, spars, piles, and the framework of houses, bridges, etc. In the
California lumber markets it is known as "Oregon pine." In Utah, where it is
common on the Wahsatch Mountains, it is called "red pine." In
California, on the western slope of the Sierra Nevada, it forms, in company with the
yellow pine, sugar pine, and incense cedar, a pretty well-defined belt at a height of from
three to six thousand feet above the sea; but it is only in Oregon and Washington,
especially in this Puget Sound region, that it reaches its very grandest development,--tall,
straight, and strong, growing down close to tidewater.
All the towns of the Sound had a hopeful, thrifty aspect. Port Townsend, picturesquely
located on a grassy bluff, was the port of clearance for vessels sailing to foreign parts.
Seattle was famed for its coal-mines, and claimed to be the coming town of the North
Pacific Coast. So also did its rival, Tacoma, which had been selected as the terminus of
the much-talked-of Northern Pacific Railway. Several coal-veins of astonishing thickness
were discovered the winter before on the Carbon River, to the east of Tacoma, one of them
said to be no less than twenty-one feet, another twenty feet, another fourteen, with many
smaller ones, the aggregate thickness of all the veins being upwards of a hundred feet.
Large deposits of magnetic iron ore and brown hematite, together with limestone, had been
discovered in advantageous proximity to the coal, making a bright outlook for the Sound
region in general in connection with its railroad hopes, its unrivaled timber resources,
and its far-reaching geographical relations.
After spending a few weeks in the Puget Sound a friend from San
Francisco, we engaged passage on the little mail steamer California, at Portland, Oregon,
for Alaska. The sail down the broad lower reaches of the Columbia and across its foamy
bar, around Cape Flattery, and up the Juan de Fuca Strait, was delightful; and after
calling again at Victoria and Port Townsend we got fairly off for icy Alaska.
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