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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This Phenomenon Is The More Worthy Of Attention As The Soil
Of These Countries Is Probably Granitic.
I doubt the secondary
formations of the Llanos being continued southward as far as the
valley of Caura.
On the 11th of June we landed on the right bank of the Orinoco at
Puerto de los Frailes, at the distance of three leagues above the
Ciudad de la Piedra, to take altitudes of the sun. The longitude of
this point is 67 degrees 26 minutes 20 seconds, or 1 degree 41 minutes
east of the mouth of the Apure. Farther on, between the towns of La
Piedra and Muitaco, or Real Corona, are the Torno and Boca del
Infierno, two points formerly dreaded by travellers. The Orinoco
suddenly changes its direction; it flows first east, then
north-north-west, and then again east. A little above the Cano
Marapiche, which opens on the northern bank, a very long island
divides the river into two branches. We passed on the south of this
island without difficulty; northward, a chain of small rocks, half
covered at high water, forms whirlpools and rapids. This is La Boca
del Infierno, and the Raudal de Camiseta. The first expeditions of
Diego Ordaz (1531) and Alonzo de Herrera (1535) have given celebrity
to this bar. The Great Cataracts of the Atures and Maypures were then
unknown; and the clumsy vessels (vergantines), in which travellers
persisted in going up the river, rendered the passage through the
rapids extremely difficult. At present no apprehension is felt in
ascending or descending the Orinoco, at any season, from its mouth as
far as the confluence of the Apure and the Meta. The only falls of
water in this space are those of Torno or Camiseta, Marimara, and
Cariven or Carichana Vieja. Neither of these three obstacles is to be
feared with experienced Indian pilots. I dwell on these hydrographic
details because a great political and commercial interest is now
connected with the communications between Angostura and the banks of
the Meta and the Apure, two rivers that lead to the eastern side of
the Cordilleras of New Grenada. The navigation from the mouth of the
Lower Orinoco to the province of Varinas is difficult only on account
of the current. The bed of the river nowhere presents obstacles more
difficult to be surmounted than those of the Danube between Vienna and
Linz. We meet with no great bars, no real cataracts, until we get
above the Meta. The Upper Orinoco, therefore, with the Cassiquiare and
the Rio Negro, forms a particular system of rivers, where the active
industry of Angostura and the shore of Caracas will remain long
unknown.
I obtained horary angles of the sun in an island in the midst of the
Boca del Infierno, where we had set up our instruments. The longitude
of this point according to the chronometer is 67 degrees 10 minutes 31
seconds. I attempted to determine the magnetic dip and intensity, but
was prevented by a heavy storm of rain.
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