Junior High School Literature, Book 1Elson, William H. (William Harris)
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Junior High School Literature, Book 1
Elson, William H. (William Harris)
American literature; English literature; Readers
“Between Lofoden and Moskoe,” he says, “the depth of the water is between
thirty-six and forty fathoms; but on the other side, toward Ver (Vurrgh),
this depth decreases so as not to afford a convenient passage for a
vessel, without the risk of splitting on the rocks, which happens even
in the calmest weather. When it is flood, the stream runs up the country
between Lofoden and Moskoe with a boisterous rapidity; but the roar of
its impetuous ebb to the sea is scarce equaled by the loudest and most
dreadful cataracts, the noise being heard several leagues off; and the
vortices or pits are of such an extent and depth, that if a ship comes
within its attraction, it is inevitably absorbed and carried down to the
bottom, and there beat to pieces against the rocks; and when the water
relaxes, the fragments thereof are thrown up again. But these intervals
of tranquillity are only at the turn of the ebb and flood, and in calm
weather, and last but a quarter of an hour, its violence gradually
returning. When the stream is most boisterous, and its fury heightened by
a storm, it is dangerous to come within a Norwegian mile of it. Boats,
yachts, and ships have been carried away by not guarding against it
before they were within its reach. It likewise happens frequently that
whales come too near the stream, and are overpowered by its violence; and
then it is impossible to describe their howlings and bellowings in their
fruitless struggles to disengage themselves. A bear once, attempting to
swim from Lofoden to Moskoe, was caught by the stream and borne down,
while he roared terribly, so as to be heard on shore. Large stocks of
firs and pine trees, after being absorbed by the current, rise again
broken and torn to such a degree as if bristles grew upon them. This
plainly shows the bottom to consist of craggy rocks, among which they are
whirled to and fro. This stream is regulated by the flux and reflux of
the sea—it being constantly high and low water every six hours. In the
year 1645, early in the morning of Sexagesima Sunday, it raged with such
noise and impetuosity that the very stones of the houses on the coast
fell to the ground.”
Public-domain text, read in full here on John Shaqi.
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