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The universal geography : earth and its inhabitants

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EIVEBS OP PARAGUAY. 301<br />

becomes more decided, <strong>and</strong> the water flows, not in a rocky bed, but over layers<br />

of tosca, an extremely tenacious white clay, probably saline, for the Pilcomayo<br />

discharges brackish waters into the Paraguay.<br />

It was long supposed that <strong>its</strong> mouths had frequently shifted ; but lateral<br />

channels, false rivers <strong>and</strong> creeks may possibly have wrongly been taken for<br />

branches of the Pilcomayo. <strong>The</strong> present mouth joins the Paraguay three miles<br />

below Asuncion, opposite the Lambare bluff. But in 1721 the chief branch was<br />

Fig. 128 —View taken on the Pilcomayo.<br />

stated to be "nine leagues," or about 26 miles away. <strong>The</strong> Kio Oonfuso, which<br />

reaches the Paraguay 22 miles above Asuncion, is a different river, <strong>and</strong> not an arm<br />

of the Pilcomayo, as shown by <strong>its</strong> much more saline water. But when in flood<br />

the two streams may perhaps communicate through the intervening bafiados. On<br />

the other h<strong>and</strong> the Araguay-Guazu, explored in 1886 by Fern<strong>and</strong>ez for 440 miles<br />

from <strong>its</strong> confluence with the Paraguay, probably branches off from the Pilcomayo<br />

about the middle part of <strong>its</strong> course. Both streams resemble each other in their

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