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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It May Be Supposed That The Danger Is
Imminent Only To Those Who Lose Themselves Far From Any Habitation, Or
Who, Having Been Stripped By Robbers, As Has Happened Of Late Years,
Have Been Fastened By The Body And Hands To The Trunk Of A Palm-Tree.
In order to escape as much as possible from the heat of the day, we
set off at two in the morning, with the hope of reaching Calabozo
before noon, a small but busy trading-town, situated in the midst of
the Llanos.
The aspect of the country was still the same. There was no
moonlight; but the great masses of nebulae that spot the southern sky
enlighten, as they set, a part of the terrestrial horizon. The solemn
spectacle of the starry vault, seen in its immense expanse - the cool
breeze which blows over the plain during the night - the waving motion
of the grass, wherever it has attained any height; everything recalled
to our minds the surface of the ocean. The illusion was augmented when
the disk of the sun appearing on the horizon, repeated its image by
the effects of refraction, and, soon losing its flattened form,
ascended rapidly and straight towards the zenith.
Sunrise in the plains is the coolest moment of the day; but this
change of temperature does not make a very lively impression on the
organs. We did not find the thermometer in general sink below 27.5;
while near Acapulco, at Mexico, and in places equally low, the
temperature at noon is often 32, and at sunrise only 17 or 18 degrees.
The level surface of the ground in the Llanos, which, during the day,
is never in the shade, absorbs so much heat that, notwithstanding the
nocturnal radiation toward a sky without clouds, the earth and air
have not time to cool very sensibly from midnight to sunrise.
In proportion as the sun rose towards the zenith, and the earth and
the strata of superincumbent air took different temperatures, the
phenomenon of the mirage displayed itself in its numerous
modifications. This phenomenon is so common in every zone, that I
mention it only because we stopped to measure with some precision the
breadth of the aerial distance between the horizon and the suspended
object. There was a constant suspension, without inversion. The little
currents of air that swept the surface of the soil had so variable a
temperature that, in a drove of wild oxen, one part appeared with the
legs raised above the surface of the ground, while the other rested on
it. The aerial distance was, according to the distance of the animal,
from 3 to 4 minutes. Where tufts of the moriche palm were found
growing in long ranges, the extremities of these green rows were
suspended like the capes which were, for so long a time, the subject
of my observations at Cumana. A well-informed person assured us, that
he had seen, between Calabozo and Uritucu, the image of an animal
inverted, without there being any direct image.
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