Some Engineering Problems Of The Panama Canal In Their Relation To Geology And Topography
Forfatter: Donald F. MacDonald
År: 1915
Forlag: Washington Government printing Office
Sted: Washington
Sider: 88
UDK: 626.1
Published With The Approval Of The Govenor Of The Panama Canal
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40
ENGINEERING PROBLEMS OF PANAMA CANAL.
evidence could be obtained on this point. At any rate no part of
Gatun Dam and no part of the locks is built across this probable
fault zone, so that the locks would not be harmed in any way should
fresh differential movement or faulting occur along it. A glance
at the map comprising Plate IV will show how the whole drainage
of the Gatun Basin, including the Chagres, the Trinidad, and the
Gatun Rivers, joined forces and emptied out into the Caribbean
through a gap in the Quebrancha Hills little more than a mile wide.
In order to form Gatun Lake, therefore, it was necessary only to
close this gap; but to do this was a huge task; it meant the build-
ing of the Gatun Dam.
THREE GREAT QUESTIONS INVOLVED IN DAM.
With tho project of this great dam, three questions in geologic
engineering presented themselves. They were: (1) As Gatun Lake
would have an area of about 165 square miles and would be 85 feet
above sea level and separated from the Caribbean by only a few
miles, would the seaward rim of this lake be found to be porous, or
composed of limestone and thus result in leakage? (2) Would the
bedrock be adequate in strength and in water-tightness to meet the
foundational requirements of the locks and dams? (3) What
would bo the best typo of dam to build under the engineering and
geologic conditions involved ?
Regarding the first of these questions the following was found
to be true. The oceanward rim of Gatun Basin was found to bo in
general a fine-grained argillaceous rock. It has already been de-
scribed as tho Gatun formation (p. 25). This rock is so fine grainßd
as to be relatively impervious. It contains a few local lenses of
gravel and conglomerate, but these seem to be discontinuous and
therefore relatively harmless in thé matter of allowing leakage.
Fortunately, thc.limestone locally forming the upper part of the
rim is not known to extend below the 85-foot, or lake, level in any
important place. If it did, a troublesome leakage that might rob
the lake of considerable water might develop in it.
I ho second question was also answered in the affirmative, for it
was found that tho Gatun rocks are relatively solid and compact
and suitable for foundations of heavy structures. However, some
writers, even recently, have affirmed that tho Gatun rocks would
sol ton. into mud when Gatun Lake filled, and thus the locks and dam
would sink their foundations and bo damaged or destroyed,. Opinions
of this sort spring from a vivid imagination and not from facts. In
the first place, the Canal Zone rocks for centuries have boon saturated
with all tho water tlioy can. hold; nine months in the your tlio rains
are so heavy that tho percentage of absorption as compared with the