Porto Rico, the most easterly and the fourth in size of the Greater Antilles, lies at the entrance to the Caribbean sea, between 17 degrees 50 minutes and 18 degrees 30 minutes north latitude and between 65 degrees 30 minutes and 67 degrees 15 minutes west longitude. It is about 100 miles long by 36 miles wide and has an area of 3606 square miles.
A range of mountains from 2000 feet to 3700 feet in height runs from east to west. The south slope of the island rises abruptly from the foothills, while on the north the ascent is more gradual and broken to a great extent by rugged spurs and deep ravines. There is but little coastal plain on the north, except at the river mouths, but on the south a considerable stretch of lowlands is found. Although many indentations occur in the coast line, few of them afford safe shelter for ships. There are thirty-nine rivers and a great number of smaller streams, but none of the rivers is navigable for more than a mile or two from the sea.
The climate is healthful and is tempered by the northeast trade winds that, with certain modifications due to local conditions, blow steadily the year round. The mean annual temperature is about 80 degrees Fahrenheit. The rainy season begins in May and ends in November and the average yearly precipitation at the foot of Mount El Yunque on the northeast coast is 120 inches. At San Juan it is 55 inches, while other sections of the island are semi-arid or subject to severe droughts. Porto Rico is particularly free from epidemics. The last case of yellow fever was reported in 1897. Cholera and bubonic plague are unknown, and dysentery diseases, formerly common, are steadily decreasing. Like other West Indian islands, it is subject to hurricanes, that of 1899 having been unusually disastrous. The census of 1910 gave the population as 1,118,012.
A. Moscioni, Photo.
SUGAR PLANTATION SCENE IN PORTO RICO
A. Moscioni, Photo.
SUGAR-SHIPPING PORT, PORTO RICO
The soil is fertile and may be divided into three classes. First, the red soil, generally found in the mountains; second, the black soil, containing much humus, and third, the coral sand soil of the coast plains. The black has proved to be the best for sugar cane, although excellent yields have been obtained from the coast lands. Notwithstanding the fact that both soil and climate are well suited to cane cultivation, the extension of the industry is checked by the formation of the country. The hilly character of the island and the comparatively limited transportation facilities do not admit of cane being grown in the interior. All of the modern plantations are near the coast, where sugar can be easily transported to steamers. In the north cane may be raised without irrigation, but in the south, where the greater part of the crop is produced, irrigation is necessary. About 400,000 acres of the surface of Porto Rico are under cultivation and half of this area is devoted to sugar. The cane grows chiefly on the rich alluvial lowlands along the coast. On the southern seaboard there is plenty of good land that has never been planted, but to make this available for agriculture means the construction of costly irrigation works with extensive aqueducts and much tunneling.