The South American Republics, Part 2 of 2Dawson, Thomas Cleland
History
The South American Republics, Part 2 of 2
Dawson, Thomas Cleland
South America -- History
Internally the condition of Bolivia has in the main been quiet since the
Chilean war, and the contest between clericalism and radicalism has lost
much of its bitterness. General Camacho led an unsuccessful insurrection
in 1890 and afterwards fled to Valparaiso. Three years later he planned
another insurrection and the government had great difficulty in
obtaining arms and money for operations against him. Chileans finally
furnished rifles and a loan, and shortly afterwards a treaty was
negotiated by which Bolivia abandoned its alliance with Peru and came
under Chilean influence. Peru resented this and the following year her
restrictions on Bolivian commerce nearly brought the two countries to
blows. The crisis, however, passed, and Bolivia has returned to the
policy of avoiding entangling alliances, while pressing Brazil, Chile,
or Peru to give her outlets to the ocean. In 1896, Alonso, leader of the
conservatives, and that energetic general and explorer, Jose Manuel
Pando, chief of the liberals, contested the presidential election. In
this contest the geographical jealousies which exist between northern
and southern Bolivia played a considerable role. Alonso was successful
and served as president during three years, but early in 1899 Pando
began warlike operations and in April overthrew Alonso in a decisive
battle. Under his vigorous administration the country has been quiet.
The plain of the Madeira has been opened up to settlement, and the
international position of the government is now vastly improved.
ECUADOR
CHAPTER I
THE CARAS
The irrigated valleys of Chile lie open to the ocean or are easily
accessible over the low coast range. The sea-board of Peru is likewise
defenceless, and though the Andean passes are high they are dry and
practicable and offer a way of approach to the table-land behind. The
want of rain from Valparaiso to Paita is explained by the Antarctic
current whose waters cool the breezes so that the warmer land condenses
no moisture. But at the northern boundary of Peru the coast bends
abruptly to the east; the cold current follows its original north-east
direction and lets the warm tropical waters wash the land. From the Gulf
of Guayaquil to Panama the coast and mountainsides are covered with
luxuriant vegetation and the ascent of the passes becomes well-nigh
impracticable. Therefore the Andean plateau in Ecuador is accessible
from the Pacific only on the south and the Colombian plateaux are
virtually cut off from communication with the western ocean.
Public-domain text, read in full here on John Shaqi.
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