The geographical distribution of these republics should be indicated. Three of them are island states of the Caribbean Sea. Cuba is the largest of the Antilles; Santo Domingo and Haiti divide between them the next largest. The rich tropical fertility of these West Indian isles has been a proverb for centuries and need not here be emphasised. Upon the mainland, the vast territory of Mexico and the five Central-American republics may be grouped together, forming as they do a kind of sub-continent, a narrowed continuation of North America. Through this region a broad mountain-mass curves from north-west to south-east. This configuration provides the characteristics and the varied products of every zone upon the same parallel of latitude: the torrid coastal strips, bordering both oceans; the beautiful, wholesome and productive region of the central plateau and long upland valleys; and finally the chilly inhospitable regions of the mountain heights. The long sweep of the country south-eastwards through the tropics also provides a wide range of character, from the cattle-rearing plains of Northern Mexico to the coffee and banana plantations of Costa Rica. Nowhere are lands of richer possibilities to be found. The small newly-created Republic of Panamá completes this northern system of Latin-American countries. Thus, before coming to South America at all, we count ten Latin-American states, three in the Antilles, seven upon the mainland. The other ten republics lie within the continent of South America. That continent is shaped by nature in lines of a vast and imposing simplicity, so that it is possible to sketch its main features in a few words. It is divided broadly into mountain, forest and plain--the immense chain of the Andes, the vast Amazonian forests, the wide-stretching plains of the Pampa, and the colossal water system of the three rivers, Orinoco, Amazon, La Plata. The dominating element is the great backbone, the cordillera of the Andes. From the southern islands of Tierra del Fuego this cordillera stretches for 4000 miles along the Pacific coast to the northern peninsulas of the Spanish Main, and thence throws out a great eastward curve along the southern shore of the Caribbean Sea. This continuous mountain-wall, clinging closely to the Pacific coast, determines the whole character of the continent. In the tropical zone, the trade winds, blowing continually from the Atlantic, sweep across South America until they strike this towering mountain barrier. Then they shed their moisture on its eastern slopes, which give birth to the multitudinous upper waters of the Orinoco, the Amazon and the western affluents of the River Plate. The Amazon rather resembles a slowly moving inland sea, its twelve principal tributaries all surpassing the measure of European rivers. The River Plate pours into the ocean more water than all the rivers of Europe put together. The Orinoco, shorter but not less voluminous, drains a vast area with