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The universal geography : earth and its inhabitants

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S. FKANCISCO BASiy. 157<br />

the Rio Verde. But tlie largest affluent is the Rio Gr<strong>and</strong>e, which joins the<br />

main stream at the point where it begins to bend round to the north-east.<br />

Through <strong>its</strong> Rio Preto tributary, <strong>its</strong> Sapuo sub-tributarj% a lake with double<br />

discharge, <strong>and</strong> the Rio Somno, the Rio Gr<strong>and</strong>e oflers a continuous waterway<br />

from the S. Francisco to the Tocantins, <strong>and</strong> consequently to the Amazons. <strong>The</strong><br />

engineer Moraes has proposed to construct a canal to divert the Rio Preto into<br />

one of the upper afflu-<br />

ents of the Parnahyba,<br />

<strong>and</strong> thus contribute to<br />

relieve the distress of<br />

the <strong>inhabitants</strong> of Ceara<br />

during periods of long<br />

drought.<br />

Below the Rio Gr<strong>and</strong>e<br />

the S. Francisco has<br />

still to descend 1,300<br />

feet before reaching the<br />

sea. AVhere it begins<br />

to be deflected abruptly<br />

eastwards, <strong>its</strong> level is<br />

lowered through a series<br />

of dangerous steps,<br />

forming the upper<br />

stages of the great Paulo<br />

Affonso Falls, justly re-<br />

garded as the " wonder<br />

of Brazil." Above the<br />

falls the stream whirls<br />

along amid a labyrinth<br />

of isl<strong>and</strong>s, reefs, <strong>and</strong><br />

isolated rocks, so close<br />

together that at low<br />

water a plucky jumper<br />

might leaj) from step-<br />

ping stone to stepping<br />

stone right across the<br />

current, although even<br />

then it discharges over<br />

Pig. 60.<br />

—<br />

Pattlo Apfonso Falls.<br />

Scale 1 : 37.000.<br />

38° 20- West or breenwicln SS")?'<br />

.1,100 Yards.<br />

^;.,,-..>-^<br />

35,000 cubic feet per second. During the floods <strong>its</strong> volume is increased probably<br />

fivefold, for at this point the S. Francisco, already within 60 miles of the sea,<br />

has received all <strong>its</strong> great affluents.<br />

As it draws near the falls the stream ramifies into several channels between<br />

three elongated isl<strong>and</strong>s <strong>and</strong> some neighbouring islets, all formed of a compact<br />

mass of gneiss. At the lower extremity of the group, the channels, which varying

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