Personal Narrative Of Travels To The Equinoctial Regions Of America During The Years 1799-1804 - Volume 3 - By Alexander Von Humboldt And Aime Bonpland.
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In Egypt, At San Domingo And In The Lakes Of The Valley Of
Mexico, The Method Practised For Catching Ducks Was As Follows:
Men,
whose heads were covered with great calabashes pierced with holes, hid
themselves in the water, and seized the birds by the feet.
The
Chinese, from the remotest antiquity, have employed the cormorant, a
bird of the pelican family, for fishing on the coast: rings are fixed
round the bird's neck to prevent him from swallowing his prey and
fishing for himself. In the lowest degree of civilization, the
sagacity of man is displayed in the stratagems of hunting and fishing:
nations who probably never had any communication with each other
furnish the most striking analogies in the means they employ in
exercising their empire over animals.
Three days elapsed before we could emerge from the labyrinth of
Jardines and Jardinillos. At night we lay at anchor; and in the day we
visited those islands or chains of rocks which were most easily
accessible. As we advanced eastward the sea became less calm and the
position of the shoals was marked by water of a milky colour. On the
boundary of a sort of gulf between Cayo Flamenco and Cayo de Piedras
we found that the temperature of the sea, at its surface, augmented
suddenly from 23.5 to 25.8 degrees centigrade. The geologic
constitution of the rocky islets that rise around the island of Pinos
fixed my attention the more earnestly as I had always rather doubted
of the existence of those huge masses of coral which are said to rise
from the abyss of the Pacific to the surface of the water. It appeared
to me more probable that these enormous masses had some primitive or
volcanic rock for a basis, to which they adhered at small depths. The
formation, partly compact and lithographic, partly bulbous, of the
limestone of Guines, had followed us as far as Batabano. It is
somewhat analogous to Jura limestone; and, judging from their external
aspect, the Cayman Islands are composed of the same rock. If the
mountains of the island of Pinos, which present at the same time (as
it is said by the first historians of the conquest) the pineta and
palmeta, be visible at the distance of twenty sea leagues, they must
attain a height of more than five hundred toises: I have been assured
that they also are formed of a limestone altogether similar to that of
Guines. From these facts I expected to find the same rock (Jura
limestone) in the Jardinillos: but I saw, in the chain of rocks that
rises generally five to six inches above the surface of the water,
only a fragmentary rock, in which angular pieces of madrepores are
cemented by quartzose sand. Sometimes the fragments form a mass of
from one to two cubic feet and the grains of quartz so disappear that
in several layers one might imagine that the polypi have remained on
the spot. The total mass of this chain of rocks appears to me a
limestone agglomerate, somewhat analogous to the earthy limestone of
the peninsula of Araya, near Cumana, but of much more recent
formation.
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