Personal Narrative of Travels to the Equinoctial Regions of America, During the Year 1799-1804 — Volume 3Humboldt, Alexander von
History
Personal Narrative of Travels to the Equinoctial Regions of America, During the Year 1799-1804 — Volume 3
Humboldt, Alexander von
Natural history -- South America; Scientific expeditions; South America -- Description and travel
On the morning of the 11th March we visited Cayo Flamenco. I found the
latitude 21 degrees 59 minutes 39 seconds. The centre of this island
is depressed and only fourteen inches above the surface of the sea.
The water here is brackish while in other cayos it is quite fresh. The
mariners of Cuba attribute this freshness of the water to the action
of the sands in filtering sea-water, the same cause which is assigned
for the freshness of the lagunes of Venice. But this supposition is
not justified by any chemical analogy. The cayos are composed of
rocks, and not of sands, and their smallness renders it extremely
improbable that the pluvial waters should unite in a permanent lake.
Perhaps the fresh water of this chain of rocks comes from the
neighbouring coast, from the mountains of Cuba, by the effect of
hydrostatic pressure. This would prove a prolongation of the strata of
Jura limestone below the sea and a superposition of coral rock on that
limestone.* (* Eruptions of fresh water in the sea, near Baiae,
Syracuse and Aradus (in Phenicia) were known to the ancients. Strabo
lib. 16 page 754. The coral islands that surround Radak, especially
the low island of Otdia, furnish also fresh water. Chamisso in
Kotzebue's Entdekkungs-Reise volume 3 page 108.)
It is too general a prejudice to consider every source of fresh or
salt water to be merely a local phenomenon: currents of water
circulate in the interior of lands between strata of rocks of a
particular density or nature, at immense distances, like the floods
that furrow the surface of the globe. The learned engineer, Don
Francisco Le Maur, informed me that in the bay of Xagua, half a degree
east of the Jardinillos, there issue in the middle of the sea, springs
of fresh water, two leagues and a half from the coast. These springs
gush up with such force that they cause an agitation of the water
often dangerous for small canoes. Vessels that are not going to Xagua
sometimes take in water from these ocean springs and the water is
fresher and colder in proportion to the depth whence it is drawn. The
manatees, guided by instinct, have discovered this region of fresh
waters; and the fishermen who like the flesh of these herbivorous
animals,* find them in abundance in the open sea. (* Possibly they
subsist upon sea-weed in the ocean, as we saw them feed, on the banks
of the Apure and the Orinoco, on several species of Panicum and
Oplismenus (camalote?). It appears common enough, on the coast of
Tabasco and Honduras, at the mouths of rivers, to find the manatees
swimming in the sea, as crocodiles do sometimes. Dampier distinguishes
between the fresh-water and the salt-water manatee. (Voyages and
Descr. volume 2) Among the Cayos de las doce leguas, east of Xagua,
some islands bear the name of Meganos del Manati.)
Public-domain text, read in full here on John Shaqi.
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