Personal Narrative of Travels to the Equinoctial Regions of America, During the Year 1799-1804 — Volume 3 — John Shaqi
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
The cause of the periodical swellings of the Orinoco acts equally on
all the rivers that take rise in the torrid zone. After the vernal
equinox, the cessation of the breezes announces the season of rains.
The increase of the rivers (which may be considered as natural
pluviometers) is in proportion to the quantity of water that falls in
the different regions. This quantity, in the centre of the forests of
the Upper Orinoco and the Rio Negro, appeared to me to exceed 90 or
100 inches annually. Such of the natives, therefore, as have lived
beneath the misty sky of the Esmeralda and the Atabapo, know, without
the smallest notion of natural philosophy, what Eudoxus and
Eratosthenes knew heretofore,* that the inundations of the great
rivers are owing solely to the equatorial rains. (* Strabo lib. 17
page 789. Diod. Sic. lib. l c. 5.) The following is the usual progress
of the oscillations of the Orinoco. Immediately after the vernal
equinox (the people say on the 25th of March) the commencement of the
rising is perceived. It is at first only an inch in twenty-four hours;
sometimes the river again sinks in April; it attains its maximum in
July; remains at the same level from the end of July till the 25th of
August; and then decreases progressively, but more slowly than it
increased. It is at its minimum in January and February. In both
worlds the rivers of the northern torrid zone attain the greatest
height nearly at the same period. The Ganges, the Niger, and the
Gambia reach the maximum, like the Orinoco, in the month of August.*
(* Nearly forty or fifty days after the summer solstice.) The Nile is
two months later, either on account of some local circumstances in the
climate of Abyssinia, or of the length of its course, from the country
of Berber, or 17.5 degrees of latitude, to the bifurcation of the
delta. The Arabian geographers assert that in Sennaar and in Abyssinia
the Nile begins to swell in the month of April (nearly as the
Orinoco); the rise, however, does not become sensible at Cairo till
toward the summer solstice; and the water attains its greatest height
at the end of the month of September.* (* Nearly eighty or ninety days
after the summer solstice.) The river keeps at the same level till the
middle of October; and is at its minimum in April and May, a period
when the rivers of Guiana begin to swell anew. It may be seen from
this rapid statement, that, notwithstanding the retardation caused by
the form of the natural channels, and by local climatic circumstances,
the great phenomenon of the oscillations of the rivers of the torrid
zone is everywhere the same. In the two zodiacs vulgarly called the
Tartar and Chaldean, or Egyptian (in the zodiac which contains the
sign of the Rat, an in that which contains those of the Fishes and
Aquarius), particular constellations are consecrated to the periodical
overflowings of the rivers. Real cycles, divisions of time, have been
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