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 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. The town of Cuenca in the kingdom of Quito, is surrounded by
three small rivers, the Machangara, the Rio del Matadero, and the
Yanuncai; of which the two former are white, and the waters of the
last are black (aguas negras). These waters, like those of the
Atabapo, are of a coffee-colour by reflection, and pale yellow by
transmission.
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