Personal Narrative of Travels to the Equinoctial Regions of America, During the Year 1799-1804 — Volume 3Humboldt, Alexander von
History
Personal Narrative of Travels to the Equinoctial Regions of America, During the Year 1799-1804 — Volume 3
Humboldt, Alexander von
Natural history -- South America; Scientific expeditions; South America -- Description and travel
We distinguish in the mountainous part of South America a chain and
three groups of mountains, namely, the Cordillera of the Andes, which
the geologist may trace without interruption from Cape Pilares, in the
western part of the Straits of Magellan, to the promontory of Paria
opposite the island of Trinidad; the insulated group of the Sierra
Nevada de Santa Marta; the group of the mountains of the Orinoco, or
of La Parime; and that of the mountains of Brazil. The Sierra de Santa
Marta being nearly in the meridian of the Cordilleras of Peru and New
Grenada, the snowy summits descried by navigators in passing the mouth
of the Rio Magdalena are commonly mistaken for the northern extremity
of the Andes. I shall soon prove that the colossal group of the Sierra
de Santa Marta is almost entirely separate from the mountains of Ocana
and Pamplona which belong to the eastern Cordillera of New Grenada.
The hot plains through which runs the Rio Cesar, and which extend
towards the valley of Upar, separate the Sierra Nevada from the Paramo
de Cacota, south of Pamplona. The ridge which divides the waters
between the gulf of Maracaibo and the Rio Magdalena is in the plain on
the east of the Laguna Zapatoza. If, on the one hand, the Sierra de
Santa Marta has been erroneously considered (on account of its eternal
snow, and its longitude) to be a continuation of the Cordillera of the
Andes, on the other hand, the connexion of that same Cordillera with
the coast mountains of the provinces of Cumana and Caracas has not
been recognized. The littoral chain of Venezuela, of which the
different ranges form the Montana de Paria, the isthmus of Araya, the
Silla of Caracas and the gneiss-granite mountains north and south of
the lake of Valencia, is joined between Porto Cabello, San Felipe and
Tocuyo to the Paramos de las Rosas and Niquitao, which form the
north-east extremity of the Sierra de Merida, and the eastern
Cordillera of the Andes of New Grenada. It is sufficient here to
mention this connexion, so important in a geological point of view;
for the denominations of Andes and Cordilleras being altogether in
disuse as applied to the chains of mountains extending from the
eastern gulf of Maracaibo to the promontory of Paria, we shall
continue to designate those chains (stretching from west to east) by
the names of littoral chain, or coast-chain of Venezuela.
Public-domain text, read in full here on John Shaqi.
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