Personal Narrative Of Travels To The Equinoctial Regions Of America During The Years 1799-1804 - Volume 2 - By Alexander Von Humboldt And Aime Bonpland.
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In A River, The
Colour Of The Reflected Light Comes To Us Always From The Interior
Strata Of The Fluid, And Not From The Upper Stratum.
Some celebrated naturalists, who have examined the purest waters of
the glaciers, and those which flow from mountains covered with
perpetual snow, where the earth is destitute of the relics of
vegetation, have thought that the proper colour of water might be
blue, or green.
Nothing, in fact, proves, that water is by nature
white; and we must always admit the presence of a colouring principle,
when water viewed by reflection is coloured. In the rivers that
contain a colouring principle, that principle is generally so little
in quantity, that it eludes all chemical research. The tints of the
ocean seem often to depend neither on the nature of the bottom, nor on
the reflection of the sky on the clouds. Sir Humphrey Davy was of
opinion that the tints of different seas may very likely be owing to
different proportions of iodine.
On consulting the geographers of antiquity, we find that the Greeks
had noticed the blue waters of Thermopylae, the red waters of Joppa,
and the black waters of the hot-baths of Astyra, opposite Lesbos. Some
rivers, the Rhone for instance, near Geneva, have a decidedly blue
colour. It is said, that the snow-waters of the Alps are sometimes of
a dark emerald green. Several lakes of Savoy and of Peru have a brown
colour approaching black. Most of these phenomena of coloration are
observed in waters that are believed to be the purest; and it is
rather from reasonings founded on analogy, than from any direct
analysis, that we may throw any light on so uncertain a matter. In the
vast system of rivers near the mouth of the Rio Zama, a fact which
appears to me remarkable is, that the black waters are principally
restricted to the equatorial regions. They begin about five degrees of
north latitude; and abound thence to beyond the equator as far as
about two degrees of south latitude. The mouth of the Rio Negro is
indeed in the latitude of 3 degrees 9 minutes; but in this interval
the black and white waters are so singularly mingled in the forests
and the savannahs, that we know not to what cause the coloration must
be attributed. The waters of the Cassiquiare, which fall into the Rio
Negro, are as white as those of the Orinoco, from which it issues. Of
two tributary streams of the Cassiquiare very near each other, the
Siapa and the Pacimony, one is white, the other black.
When the Indians are interrogated respecting the causes of these
strange colorations, they answer, as questions in natural philosophy
or physiology are sometimes answered in Europe, by repeating the fact
in other terms. If you address yourself to the missionaries, they
reply, as if they had the most convincing proofs of the fact, that the
waters are coloured by washing the roots of the sarsaparilla. The
Smilaceae no doubt abound on the banks of the Rio Negro, the Pacimony,
and the Cababury; their roots, macerated in the water, yield an
extractive matter, that is brown, bitter, and mucilaginous; but how
many tufts of smilax have we seen in places, where the waters were
entirely white. In the marshy forest which we traversed, to convey our
canoe from the Rio Tuamini to the Cano Pimichin and the Rio Negro,
why, in the same soil, did we ford alternately rivulets of black and
white water? Why did we find no river white near its springs, and
black in the lower part of its course? I know not whether the Rio
Negro preserves its yellowish brown colour as far as its mouth,
notwithstanding the great quantity of white water it receives from the
Cassiquiare and the Rio Blanco.
Although, on account of the abundance of rain, vegetation is more
vigorous close to the equator than eight or ten degrees north or
south, it cannot be affirmed, that the rivers with black waters rise
principally in the most shady and thickest forests. On the contrary, a
great number of the aguas negras come from the open savannahs that
extend from the Meta beyond the Guaviare towards the Caqueta. In a
journey which I made with Senor Montufar from the port of Guayaquil to
the Bodegas de Babaojo, at the period of the great inundations, I was
struck by the analogy of colour displayed by the vast savannahs of the
Invernadero del Garzal and of the Lagartero, as well as by the Rio
Negro and the Atabapo. These savannahs, partly inundated during three
months, are composed of paspalum, eriochloa, and several species of
cyperaceae. We sailed on waters that were from four to five feet deep;
their temperature was by day from 33 to 34 degrees of the centigrade
thermometer; they exhaled a strong smell of sulphuretted hydrogen, to
which no doubt some rotten plants of arum and heliconia, that swam on
the surface of the pools, contributed. The waters of the Lagartero
were of a golden yellow by transmitted, and coffee-brown by reflected
light. They are no doubt coloured by a carburet of hydrogen. An
analogous phenomenon is observed in the dunghill-waters prepared by
our gardeners, and in the waters that issue from bogs. May we not also
admit, that it is a mixture of carbon and hydrogen, an extractive
vegetable matter, that colours the black rivers, the Atabapo, the
Zama, the Mataveni, and the Guainia? The frequency of the equatorial
rains contributes no doubt to this coloration by filtration through a
thick mass of grasses. I suggest these ideas only in the form of a
doubt. The colouring principle seems to be in little abundance; for I
observed that the waters of the Guainia or Rio Negro, when subjected
to ebullition, do not become brown like other fluids charged with
carburets of hydrogen.
It is also very remarkable, that this phenomenon of black waters,
which might be supposed to belong only to the low regions of the
torrid zone, is found also, though rarely, on the table-lands of the
Andes.
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