The Panama Canal: A history and description of the enterpriseMills, J. Saxon (John Saxon)
Philosophy
The Panama Canal: A history and description of the enterprise
Mills, J. Saxon (John Saxon)
Panama Canal (Panama)
The isthmus rapidly degenerated into a moral as well as a climatic
pest-house. Froude described the condition of things at Panama in one
terrible sentence: "In all the world there is perhaps not now
concentrated in any single spot so much swindling and villainy, so much
foul disease, such a hideous dung-heap of moral and physical
abomination." In fairness, however, it must be said that Lesseps himself
cannot be held directly responsible for this state of affairs. He lived
in Paris, and had probably little notion of what was happening at
Panama. He furnished an example of the proverbial effects of too much
success and prosperity. He seems to have become a superstitious believer
in his own star, and to have thought that nothing could fail with which
he was associated. Still less can the French nation be blamed for the
wild doings of their representatives at the isthmus. And there is at
least one redeeming feature in the conduct of this enterprise. In the
midst of the moral and physical abominations that infested the isthmus
during the French occupation, the engineering work went on steadily and
conscientiously. Much of the French work was available for the Americans
when they took over the task, and the engineers of the United States
have always testified generously to the excellence of the French
excavation and construction along the Canal route.
It must be carefully noted that the French canal was to be sea-level
like the Suez, Corinth, and Kiel Canals. The construction of such a
waterway differed in many important ways from that of the high-level
lock canal which the United States have completed. To understand this we
must consider briefly the character of the country which lies between
Panama and Colon. The dominant and decisive features of the isthmus at
this point are the Chagres River and the Culebra Mountains. The Chagres
enters the Caribbean a little west of Colon. Its valley runs right
across the isthmus south-south-eastwardly towards Panama for about
twenty-six miles, then, at a place called Bas Opisbo, suddenly swerves
away to the north-east into the trackless and jungle-clad hill country.
This valley is the only transverse trench which the isthmus affords at
this stretch, and it has always fixed the attention of surveyors looking
out for a canal site. If the isthmus had been a rainless desert like
that of Suez, a canal could have been constructed by a further
preparation of this river valley and some heavy excavations along the
nine-mile reach from Obispo to the Pacific. The sea would then have been
admitted, the ebb and flow of the Pacific (the Atlantic shore is almost
tideless) being regulated by a tidal lock. But the problem is not nearly
so simple. The isthmus is one of the rainiest places in the world,
enjoying on the Atlantic side 140 inches of rain a year. At Panama the
rate is much smaller, not more than 60 inches. In the central hills the
rainfall averages 90 to 95 inches. The average number of rainy days in
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