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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These
Notions Are Highly Interesting To Geology And The Geography Of
Plants; Because, In Countries Where No Height Has Been Measured, We
May Form An Exact Idea Of The Lowest Height To Which The
Cordilleras Rise, On Looking Into The Map For The Words Paramo And
Nevado.
As the paramos are almost continually enveloped in a cold
and thick fog, the people say at Santa Fe and at Mexico, cae un
paramito when a thick small rain falls, and the temperature of the
air sinks considerably.
From paramo has been made emparamarse,
which signifies to be as cold as if we were on the ridge of the
Andes.) From these observations it follows, that between the
tropics, in plains where the temperature of the air is in the
day-time almost invariably above twenty-seven degrees, warmer
clothing during the night is requisite, whenever in a damp air the
thermometer sinks four or five degrees.
We landed about eight in the morning at the point of Araya, near
the new salt-works. A solitary house, near a battery of three guns,
the only defence of this coast, since the destruction of the fort
of Santiago, is the abode of the inspector. It is surprising that
these salt-works, which formerly excited the jealousy of the
English, Dutch, and other maritime powers, have not created a
village, or even a farm; a few huts only of poor Indian fishermen
are found at the extremity of the point of Araya.
This spot commands a view of the islet of Cubagua, the lofty hills
of Margareta, the ruins of the castle of Santiago, the Cerro de la
Vela, and the calcareous chain of the Brigantine, which bounds the
horizon towards the south.
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