Our Arctic province : $b Alaska and the Seal IslandsElliott, Henry Wood
History
Our Arctic province : $b Alaska and the Seal Islands
Elliott, Henry Wood
Alaska -- Description and travel
or keeping slight headway, you return their gaze with interest, and
the next turn of the ship’s rudder most likely throws into full
view a “rancherie,” in which these Indians permanently reside; your
kindly guide then eloquently describes the village and descants with
much vehemence upon the frailties and shortcomings of “Siwashes” in
general—at least all old-stagers in this country agree in despising
the aboriginal man. On the steamer forges through the still,
unruffled waters of intricate passages, now almost scraping her
yard-arms on the face of a precipitous headland—then rapidly shooting
out into the heart of a lovely bay, broad and deep enough to float in
room and safety a naval flotilla of the first class, until a long,
unusually low, timbered point seems to run out ahead directly in the
track, when your guide, giving a quick look of recognition, declares
that Wrangel[7] town lies just around it, and you speedily make your
inspection of an Alaskan hamlet.
Owing to the dense forest-covering of the country, sections of those
clays and sands which rest in most of the hollows are seldom seen,
only here and there where the banks of a brook are cut out, or
where an avalanche has stripped a clear track through the jungle,
do you get a chance to see the soil in southeastern Alaska. There
are frequent low points to the islands, composed, where beaten upon
by the sea, of fine rocky shingle, which form a flat of greater or
less width under the bluffs or steep mountain or hill slopes, about
three to six feet above present high-water mark; they become, in most
cases, covered with a certain amount of good soil, upon which a rank
growth of grass and shrubbery exists, and upon which the Indians love
to build their houses, camp out, etc. These small flats, so welcome
and so rare in this pelagic wilderness, have evidently been produced
by the waves acting at different times in opposing directions.
[Illustration: GRAND GLACIER: ICY BAY
View looking across a profile of its sea-wall face, two and a half
miles: ice cliffs from one hundred and fifty to three hundred feet
high above the water; depth of sea from sixty to eighty fathoms where
it is sounded under the steamer’s keel. An October picture, when all
its surface cavities and pinnacles are concealed by snow and smoothed
by frozen sleet]
Public-domain text, read in full here on John Shaqi.
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