The Arctic World : $b Its plants, animals, and natural phenomena. With a historical sketch of Arctic discovery, down to the British polar expedition: 1875-76.Anonymous
Science
The Arctic World : $b Its plants, animals, and natural phenomena. With a historical sketch of Arctic discovery, down to the British polar expedition: 1875-76.
Anonymous
Arctic regions; Arctic regions -- Discovery and exploration -- British
It is, he says, an unfortunate Geyser, with so little command over its
temper and stomach, that you can get a _rise_ out of it whenever
you like. Nothing more is necessary than to collect a quantity of sods
and throw them down its funnel. As it has no basin to protect it from
these liberties, you can approach to the very edge of the pipe, which
is about five feet in diameter, and look down at the boiling water
perpetually seething at the bottom. In a few minutes the dose of turf
just administered begins to disagree with it; it works itself up into
“an awful passion;” tormented by the qualms of incipient sickness,
it groans and hisses, and boils up, and spits at you with malicious
vehemence, until at last, with a roar of mingled pain and rage, it
throws up into the air a column of water forty feet high, carrying with
it all the sods that have been thrown in, and scattering them, scalded
and half-digested, at your feet. So irritated has the poor thing’s
stomach become by the discipline it has undergone, that even long
after all foreign matter has been thrown off, it continues retching
and sputtering, until at last nature is exhausted, when, sobbing and
sighing to itself, it sinks back into the bottom of its den.
The ground around the Geysers, for about a quarter of a mile, looks
as if it had been “honeycombed by disease into numerous sores and
orifices;” not a blade of grass grew on its hot, inflamed surface,
which consisted of unwholesome-looking red livid clay, or crumpled
shreds and shards of slough-like incrustations.
* * * * *
A region, corresponding in character to the desert mountain-mass we
have been describing, stretches westward from it to the extremity of
the ridge of the Snaefield Syssel, and terminates in the remarkable
cone of Snaefield Jokul.
The island coasts exhibit a singularly broken outline, and the deep
lochs or fiords, like those of Norway, only less romantic, dip into the
interior for many miles, and throw off numerous branches. These fiords
are wild and gloomy; dark, still inlets, with precipices on either
side, a thousand feet in height, and the silence unbroken, save by the
occasional wash of the waters, or the scream of a solitary ocean-bird.
Inland, however, they assume a gentler character: they end in long
narrow valleys, watered by pleasant streams, and bright with pasture.
In these bits of Arcadia the inhabitants have built their towns and
villages.
In the valleys on the north coast, which are adorned by clumps of
willow and juniper, the soil is comparatively fertile; but the most
genial scenery is found on the east, where, in some places, the
birch-trees reach a height of twenty feet, and are of sufficient size
to be used in house-building. The fuel used by the Icelanders is the
drift-wood which the Gulf Stream brings from Mexico, the Carolinas,
Virginia, and the River St. Lawrence.
Public-domain text, read in full here on John Shaqi.
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