Page:Aspects of nature in different lands and different climates; with scientific elucidations (IA b29329668 0002).pdf/78

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  • [Footnote: del Rey y de la Reyna). It was Columbus himself who, on

his second voyage, in May 1494, gave that name to this little group of islands, because the agreeable mixture of the silver-leaved arborescent Tournefortia gnapholoides, flowering species of Dolichos, Avicennia nitida, and mangrove hedges, gave to the coral islands the appearance of a group of floating gardens. "Son Cayos verdes y graciosos llenos de arboledas," says the Admiral. On the passage from Batabano to Trinidad de Cuba, I remained several days in these gardens, situated to the east of the larger island, called the Isla de Pinos, which is rich in mahogany trees: my stay was for the purpose of determining the longitude of the different keys (Cayos). The Cayo Flamenco, Cayo Bonito, Cayo de Diego Perez, and Cayo de piedras, are coral islands rising only from eight to fourteen inches above the level of the sea. The upper edge of the reef does not consist simply of blocks of dead coral; it is rather a true conglomerate, in which angular pieces of coral, cemented together with grains of quartz, are embedded. In the Cayo de piedras I saw such embedded pieces of coral measuring as much as three cubic feet. Several of the small West Indian coral islands have fresh water, a phenomenon which, wherever it presents itself, (for example, at Radak in the Pacific; see Chamisso in Kotzebue's Entdeckungs-Reise, Bd. iii. S. 108), is deserving of examination, as it has sometimes been ascribed to hydrostatic pressure operating from a distant coast, (as at Venice, and in the Bay of Xagua east of Batabano), and sometimes to the filtration of rain water. (See my Essai politique sur l'Ile de Cuba, T. ii. p. 137.)]*