Something about sugar : $b Its history, growth, manufacture and distributionRolph, George M. (George Morrison)
History
Something about sugar : $b Its history, growth, manufacture and distribution
Rolph, George M. (George Morrison)
Sugar
1900 41,269 tons
1901 51,077 ”
1902 44,913 ”
1903 46,029 ”
1904 50,744 ”
1905 38,240 ”
1906 62,975 ”
1907 50,564 ”
1908 48,933 ”
1909 52,972 ”
1910 exports 44,139 ”
1911 ” 37,282 ”
1912 ” 32,557 ”
1913 ” 31,665 ”
1914 ” 47,251 ”
1915 ” 49,107 ”
1916 ” 55,000 ”[70]
SANTO DOMINGO
Haiti is divided into two unequal parts, the republic of Haiti
(République d’Haiti), comprising 10,204 square miles, and the republic
of Santo Domingo (República Dominicana), with an area of 19,325 square
miles. It is one of the four large islands of the West Indies and lies
between 17 degrees 37 minutes and 20 degrees north latitude and 68
degrees 20 minutes and 74 degrees 28 minutes west longitude. Its length
from east to west is about 407 miles and its greatest width is 160 miles.
The total population is 2,737,700.
The surface of the island is exceedingly mountainous, three distinct
ranges traversing it from east to west. The loftiest peak, Loma Tina,
near the city of Santo Domingo, reaches a height of 10,300 feet. The
extensive intervening valleys are fertile and watered by numerous rivers,
none of which, however, are deep enough to be navigable.
The climate is hot and humid. An average temperature for the month of
January would be about 75.4 degrees Fahrenheit, for July 84 degrees,
and for the year 79.2 degrees. There are no active volcanoes, but great
damage is done from time to time by earthquakes and hurricanes. The
yearly rainfall is abundant, averaging about 120 inches. In San Pedro de
Macoris, however, where the greater part of the sugar crop of the island
is grown, the annual precipitation is in the neighborhood of 60 inches.
As this is not sufficient for the needs of the growing cane, the planters
have to do a certain amount of irrigating, and the water for this purpose
is obtained from artesian wells.
The soil of the sugar-growing territory is of porous limestone
formation, which shows evidence of disturbances and upheavals due to
volcanic agency. Overlying this is a deposit of decomposed vegetable
matter from three to twelve inches in thickness, and there are areas
where a rich black or red soil, varying from one to two feet in depth, is
found.
Public-domain text, read in full here on John Shaqi.
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