The Breaking of the Storm, Vol. I.Spielhagen, Friedrich
General
The Breaking of the Storm, Vol. I.
Spielhagen, Friedrich
Fiction
"The animal and vegetable kingdoms," said he, courteously turning to
her--"of the Gulf of Finland have almost a fresh-water character. But
none the less do we find, besides the visible connection, a constant
mutual influence between the ocean and the inner sea--a perpetual
influx and reflux, resulting from a most complicated connection and
combination of the most varied causes, one of which I must more
particularly mention, as it is precisely that to which I am now
referring. This is the regularity of the winds blowing from west to
east, and from east to west, which, moving on the surface of the water,
accompany and cause the ebb and flow of the under-currents. Seamen
reckoned upon these winds almost with the certainty with which they
might count upon a constantly recurring natural phenomenon; and rightly
so, for within the memory of man no essential change had occurred,
until a few years ago the east wind, which used always to appear in the
latter half of August and continue till the middle of October, suddenly
failed, and has not since returned."
"Well? and the consequence?" asked the President, who was listening
with the most rapt attention.
"The consequence is, sir, that enormous masses of water have
accumulated in the Baltic in the course of these years, which have been
the less remarked that they have of course attempted to spread
themselves equally on all sides, but the greatest pressure has always
been in ever-increasing proportion towards the east, so that in the
spring of last year at Nystad, in South Finland, four feet above the
usual water-mark were registered; at Wasa, two degrees farther north,
six feet; and at Tomeo, in the northernmost arm of the Gulf of Bothnia,
there were even eight. The gradual nature of the rise and the almost
universally high shores have to a great degree protected the
inhabitants of those parts from any serious calamity. But for us, whose
shores are almost without exception flat, a sudden reversal of this
stream, which for years has tended uninterruptedly to the east, would
be fearful. This reversal must however happen in case of a gale from
the north-east or east, especially if it lasted for many days. The
water driven westward by the power of the wind will vainly seek an
outlet to the ocean through the narrow straits of the Belt and the
Sound in the Cattegat and Skagerrack, and like some furious wild beast
in the toils, will throw itself upon our shores, pouring for miles
inland, tearing down everything that opposes its blind fury, covering
fields and meadows with sand and rubbish, and causing a devastation of
which our grandchildren and great-grandchildren shall speak with awe."
Public-domain text, read in full here on John Shaqi.
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