Personal Narrative Of Travels To The Equinoctial Regions Of America During The Years 1799-1804 - Volume 2 - By Alexander Von Humboldt And Aime Bonpland.


































































































































 -  The Nile has no porpoises:*
those of the sea go up the Delta no farther than Biana and Metonbis
towards - Page 522
Personal Narrative Of Travels To The Equinoctial Regions Of America During The Years 1799-1804 - Volume 2 - By Alexander Von Humboldt And Aime Bonpland. - Page 522 of 777 - First - Home

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The Nile Has No Porpoises:* Those Of The Sea Go Up The Delta No Farther Than Biana And Metonbis Towards Selamoun.

(* Those dolphins that enter the mouth of the Nile, did not escape the observation of the ancients.

In a bust in syenite, preserved in the museum at Paris, the sculptor has represented them half concealed in the undulatory beard of the god of the river.)

At five in the evening we regained with some difficulty the bed of the river. Our canoe remained fast for some minutes between two trunks of trees; and it was no sooner disengaged than we reached a spot where several paths, or small channels, crossed each other, so that the pilot was puzzled to distinguish the most open path. We navigated through a forest so thick that we could guide ourselves neither by the sun nor by the stars. We were again struck during this day by the want of arborescent ferns in that country; they diminish visibly from the sixth degree of north latitude, while the palm-trees augment prodigiously towards the equator. Fern-trees belong to a climate less hot, and a soil but little mountainous. It is only where there are mountains that these majestic plants descend towards the plains; they seem to avoid perfectly flat grounds, as those through which run the Cassiquiare, the Temi, Inirida, and the Rio Negro. We passed in the night near a rock, called the Piedra de Astor by the missionaries. The ground from the mouth of the Guaviare constantly displays the same geological formation.

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