The Panama Canal: A history and description of the enterprise
John Stuart Mill · en
On the other plan, the Chagres and its tributaries would be made the
feeders of the upper reaches of the canal. So far from being politely
shown off the premises, the question rather was whether they would be
able to supply sufficient water all the year round for the needs of the
canal. Then this harnessing of the Chagres meant the taming of its
waters in a huge artificial lake, in which the impetuous current would
be quenched and through which the dredged channel of the waterway would
run. The New Panama Company had recommended the construction of a huge
dam for this purpose at Bohio towards the Atlantic end of the canal, and
this plan had been adopted by the first American Isthmian Commission,
which issued its report in 1901. I may add that the Spooner Act, which
authorized the construction of a canal, also contemplated a lock or
high-level waterway. As we shall see, Bohio was not in the end adopted
as the site of the big dam, but Gatun, where it is now constructed, with
its concrete spillway carrying away the overflow waters of the lake down
the old Chagres channel to the near Atlantic. I need not say that these
were two very different ways of "caring for" the Chagres and its
affluents. The tide-level canal would also, of course, be supplied with
sea-water, while the high-level will be a fresh-water canal. Colonel
Goethals, the chief engineer of the canal, anticipates rather a curious
result from this latter circumstance. He thinks the bed of the upper
reaches of the canal will in course of time be quite paved with the
barnacles washed by the fresh-water from the bottoms of the great
ocean-going vessels passing through the canal.
The second physical feature is the hill country or the "Continental
Divide" which the canal enters near the point where the Chagres River
crosses its course. Here runs the famous Culebra Cut, the nine-mile-long
artificial canyon, the biggest excavation in the world. Now the highest
elevation of these hills along the centre line of the canal was 312 feet
above sea-level. The bottom of the canal at the cutting is 40 feet, so
that the vertical depth of the cut on the centre line is 272 feet. The
engineers of the tide-level scheme would have had not only to excavate
85 feet deeper--that is, to 45 feet below sea-level--but to make the
cutting immensely wider in order to avoid the danger of disastrous
landslides. This would have meant an enormous amount of additional work,
as well as expense. Nevertheless, the controversy between the two
principles was very warmly and equally sustained. It may be mentioned
that Mr. Bunau-Varilla was an especially ardent advocate of the
tide-level scheme. In fact, he was not for calling the waterway a canal
at all; he would have christened it "the Straits of Panama."