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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The Dolphins, Or Toninas, Sported
By The Side Of Our Boat.
According to the relation of Mr. Colebrooke,
the Delphinus gangeticus, which is the fresh-water porpoise of the Old
World, in like manner accompanies the boats that go up towards
Benares; but from Benares to the point where the Ganges receives the
salt waters is only two hundred leagues, while from the Atabapo to the
mouth of the Orinoco is more than three hundred and twenty.
About noon we passed the mouth of the little river Ipurichapano on the
east, and afterwards the granitic rock, known by the name of Piedra
del Tigre. Between the fourth and fifth degrees of latitude, a little
to the south of the mountains of Sipapo, we reach the southern
extremity of that chain of cataracts, which I proposed, in a memoir
published in 1800, to call the Chain of Parima. At 4 degrees 20
minutes it stretches from the right bank of the Orinoco toward the
east and east-south-east. The whole of the land extending from the
mountains of the Parima towards the river Amazon, which is traversed
by the Atabapo, the Cassiquiare, and the Rio Negro, is an immense
plain, covered partly with forests, and partly with grass. Small rocks
rise here and there like castles. We regretted that we had not stopped
to rest near the Piedra del Tigre; for on going up the Atabapo we had
great difficulty to find a spot of dry ground, open and spacious
enough to light a fire, and place our instrument and our hammocks.
On the 28th of April, it rained hard after sunset, and we were afraid
that our collections would be damaged. The poor missionary had his fit
of tertian fever, and besought us to re-embark immediately after
midnight. We passed at day-break the Piedra and the Raudalitos* (* The
rock and little cascades.) of Guarinuma. The rock is on the east bank;
it is a shelf of granite, covered with psora, cladonia, and other
lichens. I could have fancied myself transported to the north of
Europe, to the ridge of the mountains of gneiss and granite between
Freiberg and Marienberg in Saxony. The cladonias appeared to me to be
identical with the Lichen rangiferinus, the L. pixidatus, and the L.
polymorphus of Linnaeus. After having passed the rapids of Guarinuma,
the Indians showed us in the middle of the forest, on our right, the
ruins of the mission of Mendaxari, which has been long abandoned. On
the east bank of the river, near the little rock of Kemarumo, in the
midst of Indian plantations, a gigantic bombax* (* Bombax ceiba.)
attracted our curiosity. We landed to measure it; the height was
nearly one hundred and twenty feet, and the diameter between fourteen
and fifteen. This enormous specimen of vegetation surprised us the
more, as we had till then seen on the banks of the Atabapo only small
trees with slender trunks, which from afar resembled young
cherry-trees. The Indians assured that these small trees do not form a
very extensive group.
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