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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I Believed
At First, According To The Analogy Of The Phenomena Furnished By
The Mountains Of Franconia, That The Presence
Of these hornblende
masses with crystals of common (uncompact) feldspar indicated the
proximity of transition rocks; but in the high
Valley of Caracas,
near Antimano, balls of the same diabase fill a vein crossing the
mica-slate. On the western declivity of the hill of Cabo Blanco,
the gneiss is covered with a formation of sandstone, or
conglomerate, extremely recent. This sandstone combines angular
fragments of gneiss, quartz, and chlorite, magnetical sand,
madrepores, and petrified bivalve shells. Is this formation of the
same date as that of Punta Araya and Cumana?
Scarcely any part of the coast has so burning a climate as the
environs of Cabo Blanco. We suffered much from the heat, augmented
by the reverberation of a barren and dusty soil; but without
feeling any bad consequences from the effects of insolation. The
powerful action of the sun on the cerebral functions is extremely
dreaded at La Guayra, especially at the period when the yellow
fever begins to be felt. Being one day on the terrace of the house,
observing at noon the difference of the thermometer in the sun and
in the shade, a man approached me holding in his hand a potion,
which he conjured me to swallow. He was a physician, who from his
window, had observed me bareheaded, and exposed to the rays of the
sun. He assured me, that, being a native of a very northern
climate, I should infallibly, after the imprudence I had committed,
be attacked with the yellow fever that very evening, if I refused
to take the remedy against it.
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