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CUBA (the aboriginal name)

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Originally appearing in Volume V07, Page 595 of the 1911 Encyclopedia Britannica.
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See also:

CUBA (the aboriginal name)  , a See also:republic, the largest and most populous of the See also:West See also:India Islands, included between the meridians of 740 7' and 84° 57' W. See also:longitude and (roughly) the See also:parallels of 19° 48' and 230 13' N. See also:latitude . It divides the en-See also:trance to the Gulf of See also:Mexico into two passages of nearly equal width,—the Strait of See also:Florida, about 110 m. wide between Capes Hicacos in See also:Cuba and Arenas in Florida (See also:Key West being a little over See also:loo m. from See also:Havana); and the See also:Yucatan Channel, about 130 M. wide between Capes See also:San See also:Antonio and Catoche . On the N.E., E. and S.E., narrower channels See also:separate it from the See also:Bahamas, See also:Haiti (5o m.) and See also:Jamaica (85 m.) . In 1908, by the opening of a railway along the Florida Keys, the See also:time of passage by See also:water between Cuba and the See also:United States was reduced to a few See also:hours . The See also:island is See also:long and narrow, somewhat in the See also:form of an irregular See also:crescent, See also:convex toward the N . It has a decided See also:pitch. to the S . Its length from Cape Maisf to Cape San Antonio along a medial See also:line is about 730 m.; its breadth, which averages about 50 m., ranges from a maximum of 16o m. to a minimum of about 22 M . The See also:total See also:area is estimated at 41,634 sq. m. without the surrounding keys and the Isle of Pines (area about 118o sq. m.), and including these is approximately 44,164 . The See also:geography of the island is still very imperfectly known, and all figures are approximate only . The See also:coast line, including larger bays, but excluding reefs, islets, keys and all See also:minute sinuosities, is about 2500 M. in length . The N. littoral is characterized by bluffs, which grow higher and higher toward the See also:east, rising to 600 ft. at Cape Maisf . They are marked by distinct terraces .

The See also:

southern coast near Cape Maisf is See also:low and sandy . From See also:Guantanamo to See also:Santiago it rises in high escarpments, and W. of Santiago, where the Sierra Maestra runs See also:close to the See also:sea, there is a very high abrupt See also:shore . To the W. of See also:Manzanillo it sinks again, and throughout most of the remaining distance to Cape San Antonio is low, with a sandy or marshy littoral; at places See also:sand hills fringe the shore; near See also:Trinidad there are hills of considerable height; and the coast becomes high and rugged W. of Point Fisga, in the See also:province of Pinar del Rio . On both the N. and the S. See also:side of the island there are long chains of islets and reefs and See also:coral keys (of which it is estimated there are 1300), which limit See also:access to probably See also:half of the coast, and on the N. render See also:navigation difficult and dangerous . On the S. they are covered with mangroves . A large See also:part of the southern littoral is subject to overflow, and much more of it is permanently marshy . The Zapata Swamp near See also:Cienfuegos is 600 sq. m. in area; other large swamps are the Majaguillar, E. of See also:Cardenas, and the Cienaga del Buey, S. of the See also:Canto See also:river . The Isle of Pines in its See also:northern part is hilly and wooded; in its southern part, very low, level and rather barren; a tidal swamp almost cuts the island in two . A $a° B ° C So° D 78° E 7G° F GULF OF St aif of Florida Oa 4•bs~°moo Ir 0 T.rav[ O.t Canter C e ' ON oR !P la `~_ -~or,~~..~ %, M E X O P 4., c . ^o S¢ 4O e ' • ' ? L G . i ,1 \~ e r .5r t °? a' . ``~t/yju .

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End of Article: CUBA (the aboriginal name)
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