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)
area of country. This position for the dam was first suggested by a
French engineer, Godin de Lepinay, who, in a paper read before the
congress of engineers in Paris in 1879, advocated a lock canal with a
dam controlling the Chagres River at Gatun. This, then, was the biggest
problem peculiar to the high-level scheme, for the cutting through the
"continental divide," though an even more titanic labour, would have had
to be accomplished whatever type of canal had been adopted.
No feature of the construction has been subject to so much criticism and
anxious solicitude as this Gatun dyke. On it depends the maintenance of
Gatun Lake and the supply of water for the canal. If the dam fails,
everything fails. The real cause of the difficulty was the foundation
upon which this big artificial hill had to be laid. The great dam at
Assouan in Egypt is based upon the eternal granite, upon which masonry
of natural stone is built. It is, therefore, part and parcel of the
solid framework of our planet, and will probably last as long. The Gatun
dam is, however, founded upon the alluvial deposits of the Chagres
River. This alluvium consists of gravel firmly cemented with mud and
clay, and is unquestionably water-tight. These deposits go down in
places to a depth of 280 feet before the solid rock is reached. The dam
had, therefore, to be laid down on the top of them.
Now this foundation, though water-tight, is soft. It would have been
impossible to place upon it a massive structure of rock or concrete. The
deposits would have given way under its weight. The only plan was to
dump down in the valley an earthen dam, making it very broad so as to
distribute the weight over as large a space as possible of the alluvium
underneath. A steep slope would have been impossible, for the weight of
the central portion would have pushed the clay and gravel outwards, and
the whole mass would have subsided. The earth-dam was to block the
valley through which the Chagres had hitherto flowed uninterruptedly to
the sea. This valley is a mile and a half wide, and this is, therefore,
the length of the dam. Its base is 2,100 feet wide. It is 398 feet
through at the surface of the water, 100 feet wide at the top, and was
to be 115 feet above sea-level. The last figure has, it seems, been
brought down to 104 feet, which will be an advantage, as the weight upon
the foundations will be proportionately less.
Public-domain text, read in full here on John Shaqi.
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