The travellers had spent one whole year in reaching Quito, and the first
few days after their arrival were necessarily devoted to rest and an
exchange of civilities with the inhabitants. They then commenced their
operations with measuring a piece of ground, which was to be the base of
the whole work, and in this the remainder of the year 1736 was consumed.
The plain of Yaruqui, selected for this purpose, is situated one
thousand four hundred and ninety-four feet lower than Quito, and is four
leagues to the north-east of that city. “The quality, disposition, and
lower situation, all contribute to render it less cold than Quito.
Eastward it is defended by the lofty cordillera of Guamani and
Pambamarca, and westward by that of Pichincha. The soil is entirely
sand; so that besides the heat naturally resulting from the direct rays
of the sun, it is increased by the rays being reverberated by the two
cordilleras: hence it is also exposed to violent tempests of thunder,
lightning, and rain. But being quite open towards the north and south,
such dreadful whirlwinds form here that the whole interval is filled
with columns of sand, carried up by the rapidity and gyrations of
violent eddy winds, which sometimes produce fatal consequences; one
melancholy instance happened while we were there—an Indian, being caught
in one of these blasts, died on the spot. It is not indeed at all
strange that the quantity of sand in one of these columns should totally
stop all respiration in any living creature who has the misfortune of
being involved in it.”
Public-domain text, read in full here on John Shaqi.
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