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Scientific American Supplement, No. 508, September 26, 1885 by Various
page 26 of 137 (18%)
This basin is 1,400 feet from the mouth of the cave, and about 450
feet below the earth's surface. Several hundred people during five
months in every year depend entirely on that source for all the water
they use. With their frail pitchers and flaring torches they wend
their way, gasping for breath, through the intricate passages, and
reaching the water, are so profusely perspiring that they must wait
before quenching their thirst. The way back is even harder, and they
are tired and loaded; yet these people are such lovers of cleanliness
that on their arrival at their poor huts, before tasting food, they
will use some of the water that has cost them so much, to bathe their
smoke-begrimed skin. As several women once fainted in the cave, men
generally fetch the water now.

Yucatan is, and has been for ages past, quite free from earthquakes,
while all surrounding countries are from time to time convulsed. This
immunity may be due to the vast caverns and numerous great wells
existing throughout the land. Pliny the Elder was of opinion that if
numerous deep wells were made in the earth to serve as outlets for the
gases that disturb its upper strata, the strength of the earthquakes
would be diminished, and if we may judge by Yucatan, Pliny was right
in his conjectures. After him, other scientists who have carefully
studied the subject have expressed the same opinion with regard to the
efficacy of large wells.

ALICE D. LE PLONGEON.

Brooklyn, July 15, 1885.

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