Personal Narrative of Travels to the Equinoctial Regions of America, During the Year 1799-1804 — Volume 3Humboldt, Alexander von
History
Personal Narrative of Travels to the Equinoctial Regions of America, During the Year 1799-1804 — Volume 3
Humboldt, Alexander von
Natural history -- South America; Scientific expeditions; South America -- Description and travel
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.
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