It Rained Fast; Thunder Rolled At A Distance, And The Gusts Of Wind From The North-North-East Became More And More Violent.

We were during some part of the night in a critical position; we heard before us the noise of the breakers over which we had to pass, and we could ascertain their direction by the phosphoric gleam reflected from the foam of the sea.

The scene resembled the Raudal of Garzita and other rapids which we had seen in the bed of the Orinoco. We succeeded in changing our course and in less than a quarter of an hour were out of danger. While we traversed the bank of the Vibora from south-south-east to north-north-west I repeatedly tried to ascertain the temperature of the water on the surface of the sea. The cooling was less sensible on the middle of the bank than on its edge, a circumstance which we attributed to the currents that there mingle waters from different latitudes. On the south of Pedro Keys the surface of the sea, at twenty-five fathoms deep, was 26.4 and at fifteen fathoms deep 26.2 degrees. The temperature of the sea on the east of the bank had been 26.8 degrees. Some American pilots affirm that among the Bahama Islands they often know, when seated in the cabin, that they are passing over sand-banks; they allege that the lights are surrounded with small coloured halos and that the air exhaled from the lungs is visibly condensed. The latter circumstance appears very doubtful; below 30 degrees of latitude the cooling produced by the waters of the bank is not sufficiently considerable to cause this phenomenon. During the time we passed on the bank of the Vibora the constitution of the air was quite different from what it had been when we quitted it. The rain was circumscribed by the limits of the bank of which we could distinguish the form from afar by the mass of vapour with which it was covered.

On the 9th of December, as we advanced towards the Cayman Islands,* the north-east wind again blew with violence. (* Christopher Columbus in 1503 named the Cayman Islands Penascales de las Tortugas on account of the sea-tortoises which he saw swimming in those latitudes.) I nevertheless obtained some altitudes of the sun at the moment when we believed ourselves, though twelve miles distant, in the meridian of the centre of the Great Cayman, which is covered with cocoa-trees.

The weather continued bad and the sea extremely rough. The wind at length fell as we neared Cape St. Antonio. I found the northern extremity of the cape 87 degrees 17 minutes 22 seconds, or 2 degrees 34 minutes 14 seconds eastward of the Morro of the Havannah: this is the longitude now marked on the best charts. We were at the distance of three miles from land but we were made aware of the proximity of the island of Cuba by a delicious aromatic odour. The sailors affirm that this odour is not perceived when they approach from Cape Catoche on the barren coast of Mexico. As the weather grew clearer the thermometer rose gradually in the shade to 27 degrees: we advanced rapidly northward, carried on by a current from south-south-east, the temperature of which rose at the surface of the water to 26.7 degrees; while out of the current it was 24.6 degrees. We anchored in the port of the Havannah on the 19th December after a passage of twenty-five days in continuous bad weather.

CHAPTER 3.29.

POLITICAL ESSAY ON THE ISLAND OF CUBA. THE HAVANNAH. HILLS OF GUANAVACOA, CONSIDERED IN THEIR GEOLOGICAL RELATIONS. VALLEY OF LOS GUINES, BATABANO, AND PORT OF TRINIDAD. THE KING AND QUEEN'S GARDENS.

Cuba owes its political importance to a variety of circumstances, among which may be enumerated the extent of its surface, the fertility of its soil, its naval establishments, and the nature of its population, of which three-fifths are free men. All these advantages are heightened by the admirable position of the Havannah. The northern part of the Caribbean Sea, known by the name of the Gulf of Mexico, forms a circular basin more than two hundred and fifty leagues in diameter: it is a Mediterranean with two outlets. The island of Cuba, or rather its coast between Cape St. Antonio and the town of Matanzas, situated at the opening of the old channel, closes the Gulf of Mexico on the south-east, leaving the ocean current known by the name of the Gulf Stream, no other outlet on the south than a strait between Cape St. Antonio and Cape Catoche; and no other on the north than the channel of Bahama, between Bahia-Honda and the shoals of Florida. Near the northern outlet, where the highways of so many nations may be said to cross each other, lies the fine port of the Havannah, fortified at once by nature and by art. The fleets which sail from this port and which are partly constructed of the cedrela and the mahogany of the island of Cuba, might, at the entrance of the Mexican Mediterranean, menace the opposite coast, as the fleets that sail from Cadiz command the Atlantic near the Pillars of Hercules. In the meridian of the Havannah the Gulf of Mexico, the old channel, and the channel of Bahama unite. The opposite direction of the currents and the violent agitations of the atmosphere at the setting-in of winter impart a peculiar character to these latitudes at the extreme limit of the equinoctial zone.

The island of Cuba is the largest of the Antilles.* (* Its area is little less in extent than that of England not including Wales.) Its long and narrow form gives it a vast development of coast and places it in proximity with Hayti and Jamaica, with the most southern province of the United States (Florida) and the most easterly province of the Mexican Confederation (Yucatan).* (* These places are brought into communication one with another by a voyage of ten or twelve days.) This circumstance claims serious attention when it is considered that Jamaica, St. Domingo, Cuba and the southern parts of the United States (from Louisiana to Virginia) contain nearly two million eight hundred thousand Africans.

Enter page number Go  Previous Next
Page 61 of 170
Words from 61688 to 62748 of 174507