Personal Narrative Of Travels To The Equinoctial Regions Of America During The Years 1799-1804 - Volume 3 - By Alexander Von Humboldt And Aime Bonpland.
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(* At The Foot Of The Two Forts San Jose
And San Fernando, Constructed For The Defence Of The Boca Chica, It
May Be Seen How Much The Land Has Gained Upon The Sea.
Necks of land
are formed on both sides, and also before the Castillo del Angel
which, northward, commands the fort of San Fernando.) It is this small
entrance which should have been closed; its opening is only 250
toises, and the passage or navigable channel is 110 toises.
If it
should one day be determined to abandon the Boca Chica, and
re-establish the Boca Grande in the state which nature seems to
prescribe, new fortifications must be constructed on the
south-south-west of the town. This fortress has always required great
pecuniary outlays to keep it up.
The insalubrity of Carthagena varies with the state of the great
marshes that surround the town on the east and north. The Cienega de
Tesca is more than fifteen miles long; it communicates with the ocean
where it approaches the village of Guayeper. When, in years of
drought, the heaped-up earth prevents the salt water from covering the
whole plain, the emanations that rise during the heat of the day when
the thermometer stands between 28 and 32 degrees are very pernicious
to the health of the inhabitants. A small portion of hilly land
separates the town of Carthagena and the islet of Manga from the
Cienega de Tesca. Those hills, some of which are more than 500 feet
high, command the town. The Castillo de San Lazaro is seen from afar
rising like a great rocky pyramid; when examined nearer its
fortifications are not very formidable. Layers of clay and sand,
belonging to the tertiary formation of nagelfluhe, are covered with
bricks and furnish a kind of construction which has little stability.
The Cerro de Santa Maria de la Popa, crowned by a convent and some
batteries, rises above the fort of San Lazaro and is worthy of more
solid and extensive works. The image of the Virgin, preserved in the
church of the convent, has been long revered by mariners. The hill
itself forms a prolonged ridge from west to east. The calcareous rock,
with cardites, meandrites and petrified corals, somewhat resembles the
tertiary limestone of the peninsula of Araya near Cumana. It is split
and decomposed in the steep parts of the rock, and the preservation of
the convent on so unsolid a foundation is considered by the people as
one of the miracles of the patron of the place. Near the Cerro de la
Popa there appears, on several points, breccia with a limestone cement
containing angular fragments of Lydian stone. Whether this formation
of nagelfluhe is superposed on tertiary limestone of coral, and
whether the fragments of the Lydian stone come from secondary
limestone analogous to that of Zacatecas and the Moro de Nueva
Barcelona, are questions which I have not had leisure to investigate.
The view from the Popa is extensive and varied, and the windings and
rents of the coast give it a peculiar character. I was assured that
sometimes from the windows of the convent and even in the open sea,
before the fort of Boca Chica, the snowy tops of the Sierra Nevada de
Santa Marta are discernible. The distance of the Horqueta to the Popa
is seventy-eight nautical miles. This group of colossal mountains is
most frequently wrapped in thick clouds: and it is most veiled at the
season when the gales blow with violence. Although only forty-five
miles distant from the coast, it is of little service as a signal to
mariners who seek the port of Saint Marta. Hidalgo during the whole
time of his operations near the shore could take only one observation
of the Nevados.
A gloomy vegetation of cactus, Jatropha gossypifolia, croton and
mimosa covers the barren declivity of Cerro de la Popa. In herbalizing
in those wild spots, our guides showed us a thick bush of Acacia
cornigera, which had become celebrated by a deplorable event. Of all
the species of mimosa the acacia is that which is armed with the
sharpest thorns; they are sometimes two inches long; and being hollow,
serve for the habitation of ants of an extraordinary size. A woman,
annoyed by the jealousy and well founded reproaches of her husband,
conceived a project of the most barbarous vengeance. With the
assistance of her lover she bound her husband with cords, and threw
him, at night, into a bush of Mimosa cornigera. The more violently he
struggled, the more the sharp woody thorns of the tree tore his skin.
His cries were heard by persons who were passing, and he was found
after several hours of suffering, covered with blood, and dreadfully
stung by the ants. This crime is perhaps without example in the
history of human turpitude: it indicates a violence of passion less
assignable to the climate than to the barbarism of manners prevailing
among the lower class of the people.
My most important occupation at Carthagena was the comparison of my
observations with the astronomical positions fixed by the officers of
the expedition of Fidalgo. In the year 1783 (under the ministry of M.
Valdes) Don Josef Espinosa, Don Dionisio Galiano and Don Josef de Lanz
proposed to the Spanish government a plan for taking a survey of the
coast of America, in order to extend the atlas of Tofino to the
western colonies. The plan was approved; but it was not till 1792 that
an expedition was fitted out at Cadiz, and they were enabled to
commence their scientific operations at the island of Trinidad.
CHAPTER 3.31. CUBA AND THE SLAVE TRADE.
I might enumerate among the causes of the lowering of the temperature
at Cuba during the winter months, the great number of shoals with
which the island is surrounded, and on which the heat is diminished
several degrees of centesimal temperature. This diminished heat may be
assigned to the molecules of water locally cooled, which go to the
bottom; to the polar currents, which are borne toward the abyss of the
tropical ocean, or to the mixture of the deep waters with those of the
surface at the declivities of the banks.
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