By way of Cape Horn : $b four months in a Yankee clipperStevenson, Paul Eve
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By way of Cape Horn : $b four months in a Yankee clipper
Stevenson, Paul Eve
Hosea Higgins (Ship); Seafaring life; Voyages to the Pacific coast
“Beyond the shadow of the ship
I watched the water-snakes;
They moved in tracks of shining white,
And when they reared, the elfish light
Fell off in hoary flakes.
“Within the shadow of the ship
I watched their rich attire;
Blue, glossy green, and velvet black,
They coiled and swam; and every track
Was a flash of golden fire.”
How singularly devoid some men are of decent feelings! I talked last
evening at the pumps with Murphy (he whose nose was pulled) and Rumps.
The latter was boasting as to how long he could stay drunk without
seeing startling visions, and rejoiced in saying that he had been
in the lock-up of more than one city in the United States. Murphy,
however, bowled him completely over by remarking quite calmly, “I been
in the jail of every large seaport in the world.”
Though the temperature is just as high, 84° at noon on deck, the
humidity has almost disappeared and the weather seems clear and
settled. Latitude, 2° 49′ north; longitude, 27° west.
+June 6+
Indications seem to point with certainty to our having taken the
southeast Trades, for a strong breeze sprang up at six this morning,
descending upon us in a squall. We trembled lest it should prove naught
but a puff; but we had the satisfaction of seeing it steadily increase,
so that four hours later we had logged thirty-four miles, close-hauled,
laying our course, the wind being strong and true at southeast. It
might not be thought amiss if I state here what the origin of the
trade-winds is. They are due to the inrush of cold air from the poles
towards the equator to take the place of the warm current which rises
from the latter. Owing to the easterly rotation of the earth on its own
axis the air from the north becomes a northeast wind, and that from
the south a southeast wind. The hot air flows to the poles as an upper
current, and, having been cooled there, it descends to the surface of
the earth to form the westerly or anti-trade-winds.
Public-domain text, read in full here on John Shaqi.
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