The sounds which the ocean makes must be very significant and
interesting to those who live near it. When I was leaving the shore at
this place the next summer, and had got a quarter of a mile distant,
ascending a hill, I was startled by a sudden, loud sound from the sea,
as if a large steamer were letting off steam by the shore, so that I
caught my breath and felt my blood run cold for an instant, and I
turned about, expecting to see one of the Atlantic steamers thus far
out of her course, but there was nothing unusual to be seen. There was
a low bank at the entrance of the Hollow, between me and the ocean, and
suspecting that I might have risen into another stratum of air in
ascending the hill,—which had wafted to me only the ordinary roar of
the sea,—I immediately descended again, to see if I lost _hearing_ of
it; but, without regard to my ascending or descending, it died away in
a minute or two, and yet there was scarcely any wind all the while. The
old man said that this was what they called the “rut,” a peculiar roar
of the sea before the wind changes, which, however, he could not
account for. He thought that he could tell all about the weather from
the sounds which the sea made.
Old Josselyn, who came to New England in 1638, has it among his
weather-signs, that “the resounding of the sea from the shore, and
murmuring of the winds in the woods, without apparent wind, sheweth
wind to follow.”
Being on another part of the coast one night since this, I heard the
roar of the surf a mile distant, and the inhabitants said it was a sign
that the wind would work round east, and we should have rainy weather.
The ocean was heaped up somewhere at the eastward, and this roar was
occasioned by its effort to preserve its equilibrium, the wave reaching
the shore before the wind. Also the captain of a packet between this
country and England told me that he sometimes met with a wave on the
Atlantic coming against the wind, perhaps in a calm sea, which
indicated that at a distance the wind was blowing from an opposite
quarter, but the undulation had travelled faster than it. Sailors tell
of “tide-rips” and “ground-swells,” which they suppose to have been
occasioned by hurricanes and earthquakes, and to have travelled many
hundred, and sometimes even two or three thousand miles.
[Illustration: Hunting for a Leak]
Public-domain text, read in full here on John Shaqi.
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