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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The Plain, Then Thinly Inhabited, Was Filled With
Brushwood, Interspersed With Trunks Of Scattered Trees And Parasite
Plants, Enveloped With A Thick Sward, Less Capable Of Emitting Radiant
Caloric Than The Soil That Is Cultivated And Consequently Not
Sheltered From The Rays Of The Sun.
With the destruction of the trees,
and the increase of the cultivation of sugar, indigo, and cotton, the
springs, and all the natural supplies of the lake of Valencia, have
diminished from year to year.
It is difficult to form a just idea of
the enormous quantity of evaporation which takes place under the
torrid zone, in a valley surrounded with steep declivities, where a
regular breeze and descending currents of air are felt towards
evening, and the bottom of which is flat, and looks as if levelled by
the waters. It has been remarked, that the heat which prevails
throughout the year at Cura, Guacara, Nueva Valencia, and on the
borders of the lake, is the same as that felt at midsummer in Naples
and Sicily. The mean annual temperature of the valleys of Aragua is
nearly 25.5 degrees; my hygrometrical observations of the month of
February, taking the mean of day and night, gave 71.4 degrees of the
hair hygrometer. As the words great drought and great humidity have no
determinate signification, and air that would be called very dry in
the lower regions of the tropics would be regarded as humid in Europe,
we can judge of these relations between climates only by comparing
spots situated in the same zone.
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