The South American Republics, Part 1 of 2Dawson, Thomas Cleland
History
The South American Republics, Part 1 of 2
Dawson, Thomas Cleland
South America -- History
Skirting the ridge on the east and draining the vast slopes of the
Brazilian mountains of their tropical rainfall, is the great river
Parana. In latitude 27 deg. it turns abruptly to the west, as if about to
cross the pampa, but a hundred miles farther on it resumes its southward
course. At this last turn the Parana flows into a river which comes
straight down from the north, draining the bed of the old inland sea
that used to divide South America. This junction of the Parana and the
Paraguay forms the second largest river in the world--a river without
obstructions to navigation, but which is so immense that it cannot be
bridged. In latitude 32 deg. it turns back to the south-east, soon receives
the Uruguay,--a swifter stream, that drains the southern part of the
Atlantic highlands,--and then opens out into the great shallow estuary
known as the River Plate. Between the Uruguay and the Parana is the
Argentine Mesopotamia,--a flat region where the low-lying plains,
covered with luscious grasses, intersected with streams, and
interspersed with timber, gradually rise up-stream into the highlands of
the Missions.
[Illustration: ARGENTINA, PARAGUAY, URUGUAY, BOLIVIA AND CHILE]
[Illustration: FOREST SCENE IN ARGENTINA.
[From steel print.]]
To the west the pampa is bounded by the foothills of the Andes and the
parallel chains with which that great mountain system reinforces its
flanks. At the Bolivian frontier, the great outward-jutting shoulder of
the Andes looms up among a series of subordinate chains. South of them,
for a thousand miles, is a belt of broken country averaging two hundred
miles in width. The pampa creeps up to the very foot of the mountain
ranges and where it is watered blossoms like a garden. A quarter of the
population of the Republic lives in the irrigated valleys of these
Andean provinces.
A comparatively narrow, arid, belt stretches diagonally across the South
American continent from the Pacific, in Northern Chile, to the Atlantic
in Northern Patagonia. Consequently, from north to south, and from the
Atlantic back toward the north-east border of this arid belt, the
rainfall of Argentina decreases. On the north-eastern frontier it is
about 80 inches a year; at Rosario, 40; at Cordoba, 30; at Buenos Aires,
35. In the Andean provinces it decreases from over forty, near the
Bolivian frontier, to five or six at San Juan in the latitude of Santa
Fe and Cordoba. In the eastern part of the great pampa the rainfall is
ample for cereal crops; in the western half the rains are periodical and
the region is better adapted to grazing than to agriculture, and there
the grass lands are intersected with tracts of desert which grow larger
towards the south. In the Andes the eastern ranges, catching the
rain-laden upper currents, send down ample water to irrigate the valleys
and adjacent plains.
Public-domain text, read in full here on John Shaqi.
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