Spanish America, Vol. 2 (of 2)Bonnycastle, Richard Henry, Sir
History
Spanish America, Vol. 2 (of 2)
Bonnycastle, Richard Henry, Sir
Latin America -- Description and travel; Latin America -- History
The European inhabitants, and the descendants of Europeans, are noted
for their great politeness and hospitality to strangers; they are
chiefly occupied in commercial enterprize, this and Barcelona being
ports where much trade is carried on. The manner and customs of these
people is nearly allied to those of their brethren in the other great
cities of Spanish America. One of the most singular of their customs is
that of passing most of their evenings sitting on chairs placed in the
river.
In this city, the first question in a morning is, "Is the water cool?"
Their conversaziones are carried on in the rivers where the evening
parties are mostly spent in talking about the weather, the news, and
in smoking. All the inhabitants of the town it is said can swim, and
the children pass the greater part of their time in the water. The
alligator is not dangerous at Cumana, as they are seldom seen, and are
only of the smallest kind; the chief fear that the women have whilst
bathing is from the dolphin, which sometimes comes up the river and
spouts like the whale.
The port of Cumana is formed by the gulf of Cariaco, and its harbour
by the river Manzanares. The gulf of Cariaco is thirty-eight miles in
length and sixty-eight in breadth, with excellent anchoring ground;
and the ocean is always smooth and unruffled from Porto Cabello to the
point of Paria; so much so, that the coasting vessels are not decked;
the only danger in the port of Cumana being a shoal, called Morro Roxo,
half a mile in breadth and very steep on all sides.
This city has been repeatedly shook by subterrene convulsions; and
the natives have a tradition that the gulf of Cariaco was formed by
an earthquake, just before the third voyage of Columbus. In 1530, the
whole coast was shaken, and the city, then called New Toledo, suffered
by having its fort at the mouth of the river destroyed; an immense rent
was made in the coast, from which asphaltum and water issued.
These shocks were very frequent towards the end of the 16th century,
the sea often rising fifteen or twenty fathoms. On the twenty-first
of October, 1766, the city was overthrown, and numbers of persons
perished; the tremblings of the earth continued hourly for fourteen
months; but in 1767, the inhabitants incamped in the streets, when the
shocks only took place once a month; a great drought had happened in
1766, but during 1767, the rains were so continual, that the harvest
was very abundant. In this memorable earthquake the ground opened and
threw out hot water.
Public-domain text, read in full here on John Shaqi.
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