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The universal geography : earth and its inhabitants

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AMAZONIA. 05<br />

the foot of the " Cucuhy Rock," a superb granite bluff 1,000 feet high, visible for<br />

a great distance on the surrounding plains. After <strong>its</strong> junction with the TJaupcs<br />

the mainstream trends eastwards between two chains of granite hills, which con-<br />

stitute the true water-parting between the Orinoco <strong>and</strong> Amazons systems. <strong>The</strong><br />

rocky divide, which is con-<br />

tinued north-eastwards to ^'5- 32.—Lowee Couese of the Eio Beanco.<br />

the Parima range, has<br />

been pierced at this point<br />

by the waters descending<br />

from the gently sloping<br />

northern plains. Geolo-<br />

gically speaking, the part-<br />

ing line occurs, not at the<br />

bifurcation of the Cassi-<br />

quiare, but at the breach<br />

effected by the running<br />

waters along the continu-<br />

ous series of cataracts, 50<br />

on the Uaupes <strong>and</strong> 25 on<br />

the Rio Negro, cataracts<br />

which, despite their slight<br />

faU, present a picturesque<br />

eflfect with their project-<br />

ing reefs, eddies, <strong>and</strong><br />

swirling waters. <strong>The</strong> Rio<br />

Negro series has a total<br />

incline of not more than<br />

50 feet in a distance of<br />

about 40 miles.<br />

<strong>The</strong> Rio Branco<br />

("White River"), which<br />

promises to acquire great<br />

importance as the most<br />

direct future highway<br />

between British Guiana<br />

<strong>and</strong> Central Amazonia, has<br />

been frequently ascended<br />

by the Portuguese. Re-<br />

cently a Yenezuelo-Brazi-<br />

Scale i : 3,600,000.<br />

lian Frontier Commission has studied <strong>its</strong> upper valleys, but the surveys have<br />

been suspended owing to the hostility of the natives.<br />

nest of Greenwich 60°<br />

60 Miles.<br />

Like the Rio Negro, the Parima, as the Rio Branco was formerly called, has<br />

for <strong>its</strong> true upper course an affluent much longer <strong>and</strong> more copious than the branch<br />

commonly regarded as the chief headstream. This affluent, the Uraricoera, rises

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