Personal Narrative Of Travels To The Equinoctial Regions Of America During The Years 1799-1804 - Volume 1 - By Alexander Von Humboldt And Aime Bonpland.
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The Valleys Of Caracas And Of The Tuy Run Parallel For A
Considerable Length.
They are separated by a mountainous tract,
which is crossed in going from Caracas to the high savannahs of
Ocumare, passing by La Valle and Salamanca.
These savannahs
themselves are beyond the Tuy; and the valley of the Tuy being a
great deal lower than that of Caracas, the descent is almost
constantly from north to south. As Cape Codera, the Silla, the
Cerro de Avila between Caracas and La Guayra, and the mountains of
Mariara, constitute the most northern and elevated range of the
coast chain; so the mountains of Panaquire, Ocumare, Guiripa, and
of the Villa de Cura, form the most southern range. The general
direction of the strata composing this vast chain of the coast is
from south-east to north-west; and the dip is generally towards
north-west: hence it follows, that the direction of the primitive
strata is independent of that of the whole chain. It is extremely
remarkable, tracing this chain* from Porto Cabello as far as
Maniquarez and Macanao, in the island of Margareta (* I have
spoken, in the preceding chapter, of the interruption in the chain
of the coast to the east of Cape Codera.), to find, from west to
east, first granite, then gneiss, mica-slate, and primitive schist;
and finally, compact limestone, gypsum, and conglomerates
containing sea-shells.
It is to be regretted that the town of Caracas was not built
farther to the east, below the entrance of the Anauco into the
Guayra; on that spot near Chacao, where the valley widens into an
extensive plain, which seems to have been levelled by the waters.
Diego de Losada, when he founded* the town, followed no doubt the
traces of the first establishment made by Faxardo.
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