Personal Narrative Of Travels To The Equinoctial Regions Of America During The Years 1799-1804 - Volume 3 - By Alexander Von Humboldt And Aime Bonpland.
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The Partition Ridge Of This Basin Is Formed By Small
Table-Lands, Known By The Names Of Mesas De Amana,
Guanipa and Jonoro.
In the eastern part, between the meridians 63 and 66 degrees, the
plains or savannahs run southward
Beyond the bed of the Orinoco and
the Imataca, and form (as they approach the Cujuni and the Essequibo)
a kind of gulf along the Sierra Pacaraina.
(3b.) PART OF THE BASIN OF VENEZUELA RUNNING FROM SOUTH TO NORTH.
The great breadth of this zone of savannahs (from 100 to 120 leagues)
renders the denomination of land-strait somewhat improper, at least if
it be not geognostically applied to every communication of basins
bounded by high Cordilleras. Perhaps this denomination more properly
belongs to that part in which is situated the group of almost unknown
mountains that surround the sources of the Rio Negro. In the basin
comprehended between the eastern declivity of the Andes of New Grenada
and the western part of the Sierra Parime, the savannahs, as we have
observed above, stretch far beyond the equator; but their extent does
not determine the southern limits of the basin here under
consideration. These limits are marked by a ridge which divides the
waters between the Orinoco and the Rio Negro, a tributary stream of
the Amazon. The rising of a counter-slope almost imperceptible to the
eye, forms a ridge that seems to join the eastern Cordillera of the
Andes to the group of the Parime. This ridge runs from Ceja (latitude
1 degree 45 minutes), or the eastern slope of the Andes of Timana,
between the sources of the Guayavero and the Rio Caguan, towards the
isthmus that separates the Tuamini from Pimichin.
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