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
As we draw into Oonimak Pass—it is the gateway for all sailing
vessels bound to Bering Sea from American ports, we, in closing up
with the land, almost lose sight of Shishaldin, and come into the
shadow of the rougher and less attractive volcano of Pogromnia.
It shows ample evidence of its origin by the streams of blackened
frost-riven basalt and breccia which are ribbed upon its rugged
sides; great masses of eruptive rock and pumice lie here and there
scattered all over the broad-stubbed head of the mountain; tons and
tons of this material have rolled from thence in lavish profusion
and disorder, clear down for miles to the very waters of the sea
and straits, strewing that entire route with huge débris. Seams
of snow and ice lacquer, in white, thread the bold black crown
of this, the “booming” or “noisy” volcano of the Russians. It has
not been in action since 1820, when it then threw showers of ashes
and pumice; but those fires in its furnace are only banked, as it
has been smoking in inky brown and black clouds at irregular and
frequent intervals ever since; loud mutterings, deep rumblings and
wide-felt tremors of land and sea are aroused by it constantly. This
Island of Oonimak has been always regarded by the Russians as the
roof of a subterranean smelting furnace with many chimneys through
which telluric forces ascended from the molten masses beneath. It has
been, and is still, the theatre of the greatest plutonic activity
in Alaska. Russian eye-witnesses have described violent earthquakes
here where whole ridges of the interior and coast have been rent
asunder, cleft open, from which torrents of lava poured and columns
of flame and clouds of ashes, steam and smoke, have risen so as to be
viewed and noticed for a circuit of hundreds of miles around. These
manifestations were always accompanied by violent earthquakes, and
tidal-waves which often submerged adjacent villages on the sea-level,
and also whole native settlements were swept away in mountain floods
caused by the sudden melting of those big banks of ice and snow on
such volcanic summits and their foothills, upon which the hot breccia
from a vomiting crater fell.[69]
This great island in olden times was the one most densely populated
by the Aleutes. The excesses and terrible outrages of Russian
promishlyniks, followed by the wholesale work of death wrought by
small-pox, have utterly eliminated every human settlement from the
length and breadth of Oonimak, upon which no one has resided since
1847. Ruins on the north shore show the abandoned sites of numerous
large hamlets; one was over four thousand two hundred feet in
its frontage on the beach. The fear and superstition which those
tragedies of early Russian intercourse produced in the simple minds
of the natives, who belonged by birth to this great island, became
at length so potent as to cause the entire and permanent abandonment
of their desolated villages, which were once so populous and well
satisfied.
Public-domain text, read in full here on John Shaqi.
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