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The universal geography : earth and its inhabitants

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LAKES AND ETTEBS OF PATAGONIA. 388<br />

far more extensive than that of the Colorado. All the running waters of the<br />

eastern slopes of the Andes between 36^ <strong>and</strong> 41"' south latitude are collected by<br />

the Xeuquen <strong>and</strong> the Limay, <strong>its</strong> two main headstreams which enclose a vast<br />

triangular space about the foothills <strong>and</strong> the pampas.<br />

<strong>The</strong> Xeuquen, which rises near the Chilian volcano in the little lake Malbarco,<br />

7,000 feet above sea level, is joined by numerous torrents before plunging into a<br />

wild soTse in the range of foothills below Piedra Lisa. It follows the eastern<br />

base of this range as far as <strong>its</strong> confluence with <strong>its</strong> largest tributary, the Rio<br />

Agrio, which issues from a longitudinal valley between two parallel Cordilleras.<br />

A short distance below the confluence nearly all the mountain tracks from the<br />

passes between Mounts Antuco <strong>and</strong> Quetrupillan, converge at the Paso de los<br />

Indios, that is, the chief ford, now guarded by a fort. Below this point the<br />

Xeuquen sweeps roimd the plateau to <strong>its</strong> junction with the Limay ; but in this<br />

part of <strong>its</strong> course it is joined by no other affluents.<br />

<strong>The</strong> Eio Limay.—Lake Xahtel-Hcapi.<br />

<strong>The</strong> Limay, second main headstream of the Rio Xegro, is formed by the<br />

confluence of numerous torrents which descend from the Argentino-ChUian<br />

water-parting in a space of about 185 miles north <strong>and</strong> south. Several lakes<br />

flooding old glacial valleys send their overflow to the impetuous Limay, which<br />

<strong>its</strong>elf escapes from the famous Lake Xahuel-Huapi, " Tiger Isl<strong>and</strong>," so named<br />

from a long sedgy isl<strong>and</strong> occupying the centre of the basin.<br />

Xahuel-Huapi, which occupies a depression of great importance on the line of<br />

a future trans-continental highway between Bahia Blanca <strong>and</strong> Valdivia, has been<br />

known for over two centuries. Here the Jesuit missionaries had already estab-<br />

L'shed themselves in the midst of the Araucanian Indians so early as 1670, <strong>and</strong> at<br />

the beginning of the eighteenth century they founded a settlement near the head<br />

of the Rio Limay. But this station was destroyed by an incursion of hostile<br />

natives, <strong>and</strong> although it was again visited by other missionaries, Xahuel-Huapi<br />

was not systematically explored till the year 185o.<br />

Since that time numerous travellers have found their way to the shores of this<br />

lovely lake, <strong>and</strong> about 1878 it was formally occupied by the Argentine Govern-<br />

ment. Xevertheless, <strong>its</strong> contour lines are not yet accurately determined, <strong>and</strong> <strong>its</strong><br />

form is differently represented by diSerent observers. According to Siemiradzki<br />

this Alpine sea is much smaller than is usually supposed, being only 28 instead of<br />

50 miles long, as stated by previous travellers, with an extreme breadth of not<br />

more than 9 or 10 miles.<br />

But whatever be <strong>its</strong> size, all are unanimous in praise of this beautiful lake, in<br />

whose crystal waters are mirrored the surrounding heights, in one place bare<br />

trachyte cliffs, in another steep granite escarpments clothed with beech <strong>and</strong> pine<br />

groves, <strong>and</strong> dominated in the background by snowy pyramids. Its altitude above<br />

the sea is variously estimated at from 1,700 to over 2,000 feet.<br />

Immediately after issuing from Nahuel-Huapi, the Limay trends round

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