of the Island ofTrinidad. 75 



nate of lime. From the foot of these mountains for many leagues 

 to the southward there is little else than a thick, fertile, argillaceous 

 soil, without a stone or a single pebble. This tract of land, which is 

 low and perfectly level, is evidently formed by the detritus of the 

 mountains, and by the copious tribute of the waters of the Orinoco, 

 which being deposited by the influence of currents, gradually ac- 

 cumulates, and in a climate where vegetation is astonishingly rapid, 

 is speedily covered with the mangrove and other woods. It is 

 accordingly observed, that the leeward side of the island constantly 

 encroaches on the gulph, and marine shells are frequently found 

 on the land at a considerable distance from the sea. This is the 

 character of Naparima and the greater part of the country I saw along 

 the coast to la Braye. It is not only in forming and extending 

 the coast of Trinidad, that the Orinoco exerts its powerful agency ; 

 co-operating with its mighty sister flood, the Amazons, it has ma- 

 nifestly formed all that line of coast and vast extent of country, in- 

 cluded between the extreme branches of each river. To use the lan- 

 guage of a writer in the Philosophical Transactions of Edinburgh," If 

 " you cast your eye upon the map you will observe from Cayenne 

 " to the bottom of the Gulph of Paria, this immense tract of swamp, 

 *' formed by the sediment of these rivers, and a similar tract of shallow 

 " muddy coast, which their continued operation will one day elevate. 

 " The sediment of the Amazons is carried down thus to leeward (the 

 " westward) by the constant currents which set along from the 

 " southward and the coast of Brazil. That of the Oroonoko is de- 

 " tained and allowed to settle near its mouths by the opposite island 

 " of Trinidad, and still more by the mountains on the main, which 

 " are only separated from that island by the Bocos del Drago. The 

 " coast of Guiana has remained, as it were, the great eddy or resting 

 " place for the washings of great part of South America for ages ; 



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