Something about sugar

by George M. Rolph

GUADELOUPE AND MARTINIQUE

GUADELOUPE

The French West Indian colony of Guadeloupe consists of two islands that lie in the middle of the Leeward group between 15 degrees 57 minutes and 16 degrees 31 minutes north latitude and 61 degrees 10 minutes and 61 degrees 49 minutes west longitude. They are separated by a channel from one hundred feet to four hundred feet wide, called Rivière Salée.

Basse-Terre, the western island, is twenty-eight miles long, from twelve to fifteen miles wide and its area is 364 square miles. It presents a rugged surface, broken by hills and highlands, and a backbone of mountains runs through it from north to south. It is of volcanic origin, having been thrown up by four volcanic centers, Grosse Montagne (2590 feet), Les Mamelles (2536 feet and 2368 feet), Morne sans Toucher (4855 feet), and La Soufrière (4868 feet). The last-named volcano was in eruption in 1797, and in 1843 its disturbances wrecked several towns; today, however, the only evidences of life are a few hot springs and the emission of sulphurous vapors at certain points.

Basse-Terre is watered by a number of streams that become swollen and turbulent during the rainy season.

Grande-Terre, the eastern island, is low and level, the greatest elevation being only 450 feet. It consists of a plain of limestone formation with a conglomerate of sand and broken shells. It is about twenty-two miles long from north to south and its area is 255 square miles. The population is 190,273, chiefly negroes and mulattoes. For water supply it is dependent upon ponds and cisterns, as, owing to the porosity of the soil, no rivers or streams exist.

The climate is warm and humid. The mean yearly temperature is 78 degrees Fahrenheit, the minimum 61 degrees and the maximum 101 degrees. The wet season is from July to November, and on the coast the annual rainfall is about eighty-six inches, with a great deal more in the interior. Terrific storms visit the island and hurricanes have wrought much destruction.

The soil is fertile and rich and the principal crop is sugar cane, which is grown on over half the total cultivated area. The principal sugar centers are Point-à-Pitre, St. Anne and Le Moule in Grande-Terre, all of which have well-appointed usines. There is also a large usine in Basse-Terre.

Guadeloupe was discovered by Columbus in 1493. One hundred and forty-two years afterward l’Olive and Duplessis took possession in the name of a French company called the Compagnie des Iles d’Amérique. The native Caribs did not long survive the cruel treatment accorded them by l’Olive, and efforts at colonization were the reverse of successful, in fact four chartered companies were ruined in the attempt. In 1674 the islands passed into the possession of the French crown and they were governed from Martinique for a long time. In 1759 they were captured by the British, in whose hands they remained for four years. The British again occupied them in 1794, but were driven out the following summer by Victor Hugues with the help of liberated slaves. The last British occupation took place during the Hundred Days of 1815, and they finally withdrew in 1816. Slavery in Guadeloupe was abolished in 1848.

MARTINIQUE

The French colony of Martinique is the most northerly of the Windward islands. It is situated between 14 degrees 55 minutes and 14 degrees 23 minutes north latitude and 60 degrees 48 minutes and 61 degrees 16 minutes west longitude. Its area is 381 square miles, its greatest length from northwest to southeast 36 miles, and its extreme width 18 miles. The population, negroes and half-castes for the most part, numbered 190,000 in 1913.

The surface is mountainous, the highest peak being Mt. Pelée, which rises 4428 feet above sea-level. The appalling eruption of this volcano in May, 1902, was one of the greatest disasters of modern times and cost the lives of 40,000 people. About one-third of the island’s surface consists of extensive plains, most of them occurring in the south. The soil of the northern part is of volcanic formation, while in the south it is composed of clay. There are a number of streams, some of them of considerable size.

Near the coast the average temperature for June is 83 degrees, and for January 77 degrees, the mean for the year being about 80 degrees Fahrenheit. The wet season extends from June to October and the total yearly rainfall approximates 87 inches. August is the wettest month and March the driest. In the low region of the sea coast the climate is not healthful for Europeans during the hot period, but a more salubrious atmosphere and a temperature 10 degrees lower is found in the wooded uplands, 1500 feet above the sea. Fresh, dry northerly winds prevail from November to February, easterly winds from March to June, and damp, warm southerly winds from July to October. Earthquakes are frequent, but hurricanes seldom visit the island.

Martinique was discovered by Columbus on June 15, 1492, and the French Compagnie des Iles d’Amérique took possession of it in 1635. It was settled in the same year by Pierre Belain, captain-general of the island of St. Christopher, and in 1674 it became the property of the crown.

Sugar culture was begun in 1650, and a few years later the aboriginal Caribs were exterminated, their place being filled by negro slaves, of whom there were 60,000 in the island by 1736. Slavery was abolished in 1848.[71]

During the seventeenth century Martinique was attacked several times by the British and the Dutch. It was captured in 1762 by the British under Admiral Rodney, but restored to the French in the following year. It was held by the British from 1793 to 1801 and also between 1809 and 1814.

The capital of the island is Fort de France, on the west coast. It is situated upon a fine harbor and has 18,000 inhabitants. Besides the chief product, sugar, the colony raises coffee, cocoa, tobacco and cotton.