CHAPTEE XIII 



NOKTHBKN STATES OF SOUTH AMERICA 



The great continent of South America (Pig. 18), with its 

 roughly triangular shape, is not much smaller than its 

 northern relative. The basis of the triangle facing northward 

 is hounded by the Caribbean Sea, and the two other sides 

 by the Atlantic and Pacific Oceans respectively. There is 

 a very general impression that the west coast of South 

 America is mountainous, the remainder being a vast plain. 

 This is not quite correct. A northern continuation of 

 the long chain of the Andes skirts also tihe southern shores 

 of the Caribbean Sea, while to the south-east of it lies the 

 highland of Guiana and further south the Brazilian highland. 

 The two eastern highlands — ^that of Guiana and Brazil — are 

 broken into two parts by the Amazon valley. The space 

 between these eastern highlands and the Andes is occupied 

 by the central lowlands. We might say, therefore, that the 

 three great natural regions of South America are the eastern 

 highlands, the central lowlands and the western Cordillera. 

 The Amazon, Orinoco and La Plata — the three great streams 

 ^all drain eastward. 



The main part of the continent has a tropical climate. 

 Sub-tropical and temperate conditions prevail in the south. 

 The climate of the Brazilian region is exceptionally favour- 

 able for a luxuriant development of the fauna and flora, 

 whereas certain parts of what Dr. Wallace called " the Chilean 

 sub -region " are arid, and inimical to expansion and specific 

 differentiation of animals and plants. 



Although our acquaintance with the fauna, flora and 

 geology of this vast continent is naturally much less complete 

 than that of North America or Europe, we possess unmis- 

 takable evidences of the fact that South America has under- 

 gone considerable alterations in the distribution of land and 



